Lecture: "How Did They Make Those Maps"
A history of mapmaking explores how observers measured the Earth, recorded coordinates and built maps before satellites and modern surveying.
字幕來源:Vidleaf 自動語音辨識,可能有誤。Vidleaf 加入 AI 標點,保留原字詞與時間戳。下方可查看原始字幕。
AI 生成摘要
This lecture explores how maps were constructed before aerial photography and satellites. It connects observations of the Earth with the methods of Eratosthenes and Ptolemy, then follows practical navigation through portolan charts and instruments used at sea. Later examples examine the mapping of Africa and the Great Lakes, including errors copied from earlier maps and improvements made through land surveys. The speaker challenges the idea that cartographic knowledge simply became more accurate at every step. The linked chapters let readers compare methods of measurement with the ways information was preserved, reused and sometimes misunderstood.
重點
- [8:23] Eratosthenes' example connects observations of sunlight and distance with estimating the Earth's size.
- [28:47] Ptolemy's geographic work survived through descriptions and recorded coordinates.
- [1:06:51] The Great Lakes examples show how borrowing from earlier maps could preserve errors as well as knowledge.
根據字幕生成。請透過連結對照原影片核對。 概覽與重點由 Vidleaf 於 2026-10-21 核對。
完整概覽
This talk, titled "How did they do that?", opens with thanks to Jeff and the McClung Museum staff for hosting and an invitation to the museum's map exhibit, described as a fine collection of important maps of North America, the world, Tennessee and the area. It begins with a basic map-making question—how one would map the spot where you are standing—and uses visibility at increasing altitudes, from a six-foot-tall person seeing about three miles up to the shuttle Columbia in 1993 at 163 miles up seeing about 1,200 miles, to show how altitude expands map-making vision. Historical maps, including a Portuguese atlas map of about 1565, a Forlani map of about 1565, the first map published in America in 1677, and General Smith's map of the Tennessee government from about 1825, are laid next to aerial and satellite photographs and said to overlay fairly well, though some features such as Nantucket and Martha's Vineyard are not quite in the right place. The talk calls the idea that Columbus's contemporaries thought the world was flat a myth, offers the round shadow on the moon as proof of the world's rotundity, and describes how Eratosthenes, as long ago as 200 BC, used the sun at Syene and a shadow angle at Alexandria to estimate the Earth's circumference, off by 9%. It presents Claudius Ptolemy as the most influential cartographer who ever lived, covering his Geographia, his view of the oikoumine as one quarter of a sphere, his two projections, his world map plus 26 regional maps, and his methods for latitude and longitude, including the quadrant, longest-day differences, eclipse timing, and adjusted itinerary distances, and closes with Martin Behaim's 1492 globe, noting there is no evidence Columbus ever saw it, though it is not unlikely he saw it or something like it. Later segments trace how Ptolemy's Geography survived as digital data—a textbook on projections plus a list of 8,000 coordinates—was rediscovered in Constantinople in the late 1300s and became the standard world atlas around 1400 for at least 100 years; how Mediterranean sailors used portolan charts, the compass, log and line, and Travers board, with the Compasso de Navigare plotted into a Mediterranean map pretty close to the modern outline; how similar methods and instruments were used on a larger scale to map Africa down to Diaz rounding the Cape of Good Hope in 1488; and how the Great Lakes were mapped, arguing that cartographic progress was not linear, with the 1671 Jesuit map of Lake Superior very accurate, imaginary islands borrowed between cartographers, the Mitchell map's non-existent islands cited in the 1783 treaty, and the problem eventually solved on land through the Northwest Territory grid first tried in the Seven Ranges in 1787.
附時間戳的章節摘要
Opening thanks and map exhibit introduction
- [0:00] Speaker thanks Jeff and the McClung Museum staff for inviting him and hosting him for a couple of days.
- [0:12] He asks how many have seen the map exhibit and, after a fair number raise hands, urges those who haven't to go see it.
- [0:27] He calls it a really fine collection of very important maps, including great maps of North America and the world and interesting maps of Tennessee and the area.
- [0:40] He hopes his talk will help listeners appreciate the exhibit more.
- [0:49] His topic is titled "How did they do that?"
How Altitude Expands Map-Making Vision
- [1:00] A basic map-making question is how one would map the spot where you are standing.
- [1:15] From a flat surface, a six-foot-tall person can see about three miles, which is too limited to show much topographic detail.
- [1:35] At about 500 feet, visibility increases to about 27 miles, far enough to pick out coves.
- [1:50] From a 10,000-foot mountain like Mount San Jacinto, visibility extends to about 125 miles, enough for a fairly good sketch on a clear day if you know how.
- [2:13] At 30,000 feet in an airplane, you can see something like 212 miles and begin to pick out considerable topographic detail.
- [2:36] From the shuttle Columbia in 1993 at 163 miles up, you can see about 1,200 miles, out to the middle of the Arabian Peninsula.
- [3:15] A map from a Portuguese atlas of about 1565 in the Newberry collections shows the Horn of Africa and Arabian Peninsula and appears to align with the aerial photograph.
Historical Maps vs. Satellite Images
- [4:17] The Blue Marble photo was taken from Apollo 17 in 1972 at a height of 28,000 miles.
- [4:32] In this famous shot the entire globe is visible, and the whole continent of Africa can be seen except for a little bit obscured by clouds.
- [4:47] An Italian map by a man named Forlani from about 1565 overlays fairly well on the aerial photograph.
- [5:13] A map of New England looking from the east (looking west) shows Cape Cod, Lake Winnipesaukee, Rhode Island and the Connecticut River.
- [5:35] It is the first map published in America, in 1677 in John Hubbard's book history of New England.
- [5:46] Laid next to a modern satellite photo it is pretty remarkable, though Nantucket and Martha's Vineyard aren't quite in the right place and Rhode Island is further out.
- [6:18] General Smith's map of the Tennessee government, from about 1825, shows Knoxville's position between two northeast-southwest trending rivers and the mountain lines.
Eratosthenes Measures the Earth
- [7:02] The idea that Columbus's contemporaries thought the world was flat is a myth; anyone with scholarly pretensions or practical navigation experience knew the world was not flat.
- [7:34] A cosmography text offers a proof of the world's rotundity: the Earth's shadow on the moon is round, unlike the shapes a tetrahedron, pyramid, or cube would cast.
- [8:23] As long ago as 200 BC, Eratosthenes was able to measure a pretty good estimate of the Earth's actual circumference.
- [8:36] Eratosthenes knew that in Syene, near the Aswan Dam, the sun was directly above a well on a certain day, visible as a reflection down the well.
- [9:07] On that same day in Alexandria, Eratosthenes measured the angle of the shadow cast by a perpendicular pole.
- [9:22] He assumed Syene and Alexandria were more or less on a north-south line, which they roughly are, and used elementary mathematics.
- [10:19] He calculated the angle as 7.2 degrees, or a 50th of a circle, and reckoned the distance as 5,000 stadia.
- [10:33] Multiplying 5,000 stadia by 50 gave about 24,860 or 24,000 miles; the actual figure is 24,860, so he was off by 9%, which is pretty reasonable given his instrumentation.
Ptolemy and His World Maps
- [11:08] Claudius Ptolemy is described as the most influential cartographer who ever lived.
- [11:15] Ptolemy lived in the second century AD and worked around 125 AD.
- [11:32] Ptolemy was a polymath who wrote treatises on astronomy, music, and mathematics, and is probably most known as an astronomer.
- [11:42] He wrote a treatise called Geographia on the mapping of the world.
- [11:53] Ptolemy knew the Earth was a round sphere and held the general Greek view that the oikoumine, the inhabited area, was one quarter of a sphere.
- [12:31] Ptolemy invented his first projection, a cylindrical projection showing 180 degrees.
- [12:43] The Western end of the map was the Fortunate Isles, which some think were the Canaries and Madeira and some think were Cape Verde.
- [13:36] Ptolemy's second projection suggests more of the globular shape and was used for his world map.
- [14:03] On the map, Africa was largely unknown in the south, and the assumption was that the Indian Ocean was a closed sea.
- [14:36] Ptolemy made a world map plus 26 regional maps: 10 of Europe, 4 of Africa, and 12 of Asia.
Ptolemy's Map-Making Methods
- [14:53] Ptolemy discusses how to make a map, starting ideally with a big ball, then a slice of a ball, before settling on flat paper with two projections.
- [15:27] He plots all the places he knew about in the world on these projections.
- [15:32] A quadrant was one of the main tools available at the time, sighting through it with a weighted plumb to read latitude directly, e.g. from the North Star.
- [15:53] Latitude was relatively easy, and ancient astronomers had very large operational quadrants that could probably read latitude quite accurately.
- [16:11] He also determined north-south position from the difference between longest day and night length, which is equal at the equator but grows with latitude (about 1 hour at Meroe, 2 at southern Egypt, 3.5 at Alexandria, 9+ in Denmark).
- [17:00] He would have gathered longest-day information from Roman legions operating in England, Germany, Spain and France.
- [17:19] He knew Alexandria was 31 degrees north quite accurately, and calculated it as about 60 degrees 30 minutes east of the Fortunate Islands.
- [17:39] Longitude is time: one hour equals 15 minutes of longitude; the accurate clock solution wasn't finalized until John Harrison in the 1780s, but Ptolemy was aware of eclipse-timing as an alternative.
- [18:46] A lot of information had been gathered about distances of places, partly from Romans wandering their empire and being active in Britain shortly before Ptolemy's time.
Ptolemy's Map-Making Method
- [19:04] London's position was fixed, and most of Ptolemy's longitudes were probably cobbled together from distance measurements.
- [19:18] Ptolemy had access to the Alexandrian library and presumably to Roman records and itineraries, virtually all now lost.
- [19:36] He knew itinerary distances such as Alexandria to Algiers or Tunis in Roman miles.
- [19:54] Because any road is a little windy, he allowed for one-fifth error, counting 500 Roman miles as 400.
- [20:12] He used the adjusted distance to establish the longitude of Tunis, London, or other cities.
- [20:21] He likely worked slowly and painstakingly on one huge map, perhaps on a wall or a floor.
- [20:49] By gradually shifting and moving places around, he produced his world map.
Behaim Globe and Columbus's Voyage
- [21:03] The globe was made in 1492 by German Martin Behaim, who was working in Portugal.
- [21:06] There is no evidence Columbus ever saw this globe, though it is not unlikely he saw it or something like it.
- [21:28] The globe wraps Ptolemy's world around a sphere.
- [21:35] Ptolemy did not accept Eratosthenes' measurement for the size of the globe and posited a somewhat smaller sphere.
- [21:51] Ptolemy exaggerated the longitudinal length of the oikumene, so wrapping it around a smaller globe produces a Pacific Ocean view.
- [22:24] The globe shows Sipangu (Japan) and islands off China, information that came from Marco Polo.
- [22:30] The globe shows what Columbus thought he was doing: sailing west past the Atlantic islands until he hit islands off the coast of China.
- [23:01] Columbus reportedly went to his grave thinking he had discovered those islands.
Ptolemy's Map of Britain and Its Influence
- [23:13] Ptolemy's detailed map-making process is examined using his first regional map of Europe, the British Isles.
- [23:28] Ptolemy's ordering of regional maps, starting with the British Isles then Iberia, became entrenched in atlas tradition, including Abraham Ortelius's 1570 atlas and most atlases until the 20th century.
- [24:27] Ptolemy's map of Great Britain records many place names of towns, river locations, names of peoples, and physical features like mountains and a forest in Scotland.
- [25:10] Ptolemy began with a projection of the region and placed his best guess for London's latitude and longitude.
- [25:21] Roman legions traveled throughout Great Britain and Ptolemy had itineraries giving distances between places, especially towns.
- [26:03] Several places were established fairly accurately relative to one another, such as Ratae (Leicester), Deva (Chester), Lindum (Lincoln), and Eboracum (York).
- [26:34] Some people think the Romans had a kind of triangulation for surveying, and Ptolemy may have had a map of England from someone in the army.
- [27:03] Using the best information he had, Ptolemy produced the outline and plotted river mouths and places on his big map.
Ptolemy's Geography Survived Through Coordinates
- [27:34] Maps are extremely fragile and subject to wear and tear, both then and today.
- [27:45] Most maps get used to death, if they're used at all.
- [27:53] Had Ptolemy made a big world map and 26 regional maps on parchment or papyrus, maybe copies would have been made and survived the millennia.
- [28:15] Ptolemy at least made one big map, but his Geography survived because he digitized it.
- [28:25] He started with latitudes and longitudes of towns, then read off other coordinates from his base map.
- [28:47] He recorded coordinates such as 53 degrees 30 minutes latitude and about 22 degrees 10 minutes longitude.
- [29:02] He did this for river mouths, promontories, and other features, recording dozens, perhaps as many as a couple hundred points for the British Isles.
Ptolemy's Geography and Its Revival
- [29:26] The Latin manuscript shown is a copy of Ptolemy's Geography, originally written in Greek with some Greek manuscripts still extant.
- [29:39] Ptolemy's Geography as it came down through the ages contained no maps, but a textbook on projections, a general description of mapping, and a list of 8,000 coordinates.
- [29:53] Each entry lists a place with latitude and fraction and longitude and fraction.
- [30:04] Ptolemy expressed minutes as fractions of a degree, saying 50 degrees and a half for 50 degrees 30 minutes, and 50 degrees and a half and a quarter for 50 degrees 45 minutes.
- [30:23] They did not have the concept of a unified fraction.
- [30:38] The Geography as it came down consisted of just numeric, alphanumeric data, essentially digital data.
- [30:44] There is some evidence the Arabs had access to Ptolemy's Geography, but it was pretty much lost to Western culture until the late 1300s.
- [31:01] A Greek manuscript was discovered in Constantinople, and a geographer there followed Ptolemy's instructions to plot the 8,000 places and produce an atlas.
- [31:15] It is unknown whether he made one big map or regional maps, but he followed Ptolemy's instructions.
- [31:28] The atlas was quickly translated into Latin, many copies were made, and it became the first standard atlas of the world around 1400.
Ptolemy's Atlas and the Bent Scotland Map
- [31:44] Ptolemy's atlas stayed the standard atlas of the world for at least 100 years.
- [31:52] Ptolemy's geography was one of the first books published, with the first edition with maps in 1477, and multiple editions appeared through the 16th century.
- [32:04] Ortelius's Theatrum Orbis Terrarum around 1570 is thought of as the first modern atlas, but until at least the 1520s Ptolemy's maps from 125 AD were pretty much it for understanding world geography.
- [32:27] When new discoveries happened, mapmakers had to think on their feet; one exhibit map shows a basically Ptolemaic world with some American stuff tacked on.
- [32:47] The speaker is convinced, though has not read anyone saying it explicitly, that Scotland appears bent because that bit of Scotland should be turned up on end 90 degrees.
- [33:08] Turned 90 degrees, the map is not a bad rendition of Scotland, showing the peninsula, the Moray Firth, and fjord-like features on the west side.
- [33:25] It is not bad for 125 AD, drawn by a guy a couple thousand miles away who never left Alexandria, probably working from verbal descriptions.
Ptolemy's Bent Britain and Thule
- [33:40] Ptolemy had to bend Britain because of the island of Thule, shown on a 1539 map as the northernmost habitable place.
- [34:00] Some think Thule may have been Iceland or possibly another faraway island in the North Atlantic.
- [34:08] Ptolemy's information traced back to Pythias, who said Thule was six days' sail north of Britain and near the frozen sea.
- [34:19] The idea was that much beyond 60 degrees north the entire sea was frozen and therefore uninhabitable.
- [34:27] Ptolemy had much information from the Roman legions about Britain and Scotland and knew there was more land further north.
- [34:45] Ptolemy had plotted Thule at a location, but Pythias's six days' sail north of Britain did not fit if placed that way.
- [35:02] Like many scientists today, Ptolemy tried to adjust and understand the data in the way that seemed to make the most sense.
- [35:09] He tried to preserve the length of Britain while recognizing Thule as pretty much the northern limit of habitation, so he simply bent it.
Ptolemy and Portolan Charts
- [35:54] The discovery of Ptolemy's geography around 1400 was epochal in cartography history.
- [36:02] Grid-based mapping with latitude and longitude comes from Ptolemy.
- [36:14] Another parallel Mediterranean tradition began a couple hundred years earlier.
- [36:20] That parallel tradition is the portolan chart.
Earliest Portland Chart Features
- [36:31] The earliest known copy of a Portland chart is shown.
- [36:38] Portland charts were almost all drawn on animal skin, on vellum.
- [36:41] The neck of the animal is visible in the outline.
- [36:44] The map depicts the Mediterranean, with the Strait of Gibraltar, North Africa, and the boot of Italy labeled.
- [37:05] The Black Sea was almost always included in portolan charts, though it has been somewhat eroded here.
- [37:16] This map, one of the most important in cartography history, was found in a Paris junk shop in the 1840s and now lives in the Bibliothek Nassau.
- [37:41] Portland charts invariably have a circular grid, with great circles inscribed and wind roses radiating in the middle.
Portolan Charts: Features and Physical Evidence
- [37:59] Rhumb lines (R-H-U-M-V) radiate across portolan charts.
- [38:04] Place names on portolan charts are always written inland, keeping water spaces as open as possible.
- [38:14] Rhumb lines were typically different colors—green, red, or black depending on the chart.
- [38:25] Charts showed tiny symbols for rocks.
- [38:30] Portolan charts have no fixed 'up'; lettering is oriented to be read from different directions, so going around an island meant turning the chart.
- [38:59] The Newberry's earliest portolan chart is from 1456, made by Rosselli from Majorca, who signed it in the neck.
- [39:20] Charts outline the Mediterranean with the Black Sea, and most went up the west coast of Europe, usually including the British Isles.
- [39:31] Flags were very often placed around the border.
- [39:38] Some surviving portolan charts are pristine and lovely, probably made for rich clients, parlor use, or library use.
- [40:04] Some charts show evidence of having been to sea, including holes where one was nailed to a wooden roller and a neck hole for a leather thong to tie it rolled up.
- [40:25] This chart shows wear from being rolled and unrolled, and some flags show signs of ink pigment having gotten wet.
Using a Portolan Chart to Plot a Course
- [40:42] A Newberry atlas opening, with digitally joined sheets, is used to show how a mariner might use a portolan chart.
- [41:02] The example route runs from Melilla, thought to be on the north coast of Africa, to Cabo da Gata.
- [41:22] The mariner could draw the course or lay a parallel ruler between the two places.
- [41:27] One arm of the parallel ruler is placed on the route and the other is swung until it lines up with a wind rose.
- [41:43] The resulting bearing falls between north by east and north-northeast.
- [41:47] The mariner would try to get the compass to read a little east of North by East, hopefully striking his point.
- [42:07] The chart indicates a big rock there, and similar marks are used on modern nautical charts to indicate hazards to navigation, with little dots indicating shoals.
Early Navigation: Portolan Charts and Compasses
- [42:25] Some portolan charts include a small ship skeleton to mark a wreck or sunken ship.
- [42:35] The main navigational tool was the compass.
- [42:39] Very few really ancient compasses survive.
- [42:46] The compass was once said to be invented in China and carried to the Mediterranean, but now people think it may have been independently invented.
- [42:50] Textual evidence mentions sailing by the magnetized needle in the early 1200s.
- [43:04] The cart Pisan comes out around the late 1200s, about the same time.
- [43:10] The earliest compasses may have been just a needle floating on water held up by surface tension, sometimes pushed through a straw to keep it afloat.
- [43:24] By a very early age they had devised a card with the needle attached underneath.
- [43:31] They would have needed an hourglass, or in some cases a minute glass or a half-minute glass.
Log and Line Speed Measurement at Sea
- [43:39] Navigators from at least the late Middle Ages up until well into the 18th century used a log and line to gather information about their speed.
- [43:57] The method required a spool with a lot of line, a log or chip, and a glass good for half a minute.
- [44:11] It likely needed at least three men: one holding the log reel, one holding the 30-second glass, and one holding the weighted chip.
- [44:43] A red rag tied to the line indicated the chip was far enough behind the ship to be free of the wake.
- [45:01] When the red line went over the rail, the glass was turned and they counted how many knots went over until the glass ran out.
- [45:34] The speed was recorded on a Travers board, a simple device usable by an illiterate seaman familiar with the points of the compass and numbers 1 to 12.
- [46:01] Each concentric row of circles on the Travers board represented a half hour, up to the four hour watch.
- [47:08] Every hour they used the chip log and plotted speed down here, with each line being one hour of the watch.
- [47:55] They could record down to the quarter of a knot, giving a fairly accurate estimate of speed.
- [48:01] At the end of a four hour watch, the seaman could hand the board over with a complete record of distance, direction and speed.
Portolani and the Compasso de Navigare
- [48:39] Much of the Siemens information about distances from ports was recorded in itinerary form.
- [49:05] These records are called Portolani, books of sailing directions between ports.
- [49:16] The most famous Portolani is the Compasso de Navigare from the late 1200s.
- [49:23] It lists entries such as 30 miles to the northwest from one port to another, with occasional notes about the place.
- [50:06] Retired physician Jonathan Landman converted all the measurements in the Compasso da Navigare into standard distances and directions.
- [50:50] Plotting those distances and bearings does in fact generate a map of the Mediterranean.
- [51:08] Surveying involves an error of closure, but a closed area like the Strait of Gibraltar can be adjusted to fit.
- [51:43] The result is pretty close to the modern outline of the Mediterranean.
- [51:58] The basic portolan chart was likely generated from these tables over a long procedure involving many errors and partial maps.
Navigation instruments for mapping Africa
- [52:47] Similar methods using many of the same instruments occur on a larger scale when mapping a continent.
- [53:04] Portuguese efforts to map the West Coast of Africa involved instruments beyond the quadrant.
- [53:14] The cross staff works by aligning a bar with the horizon and the cited object, then reading an angle off a sliding bar.
- [53:35] The exhibit includes a model and many instruments, some never seen before by the speaker.
- [53:44] The backstaff uses the same principle as the cross staff but you turn your back to the sun and read its shadow via a mirror or vane.
Ptolemy's Africa and Portuguese Exploration
- [54:12] Instruments like the quadrant or cross staff were used to measure latitude.
- [54:20] The Portuguese gradually began to map Africa.
- [54:28] A portion of a 1489 map shows the Africa that Ptolemy knew, consisting of the northwest, the north coast, and the North Shore of the Mediterranean.
- [54:43] Ptolemy knew about the Nile and they knew or thought they knew its source was in the mountains of the moon, somewhere far south in Africa.
- [54:54] They also knew or thought they knew about big lakes near the end of the Nile, which the speaker has no doubt were Lake Victoria and Lake Nyazaland.
- [55:16] The Portuguese made a dedicated effort to see if they could get around Africa and whether it enclosed the Indian Ocean.
- [55:32] They sailed down the West Coast in a very long process, reaching the River of Gold a few years after 1432.
- [56:01] It took the Portuguese something like 50 years to nail down the bulge of Africa, using latitude readings at river mouths and keeping track of distances and directions.
- [56:28] There was finally a big push to get around the continent, in 1485, no 1480.
Diaz's Voyage and Martellus's 1489 World Map
- [56:40] Bartolomeo Diaz rounds the Cape of Good Hope and reaches the Great Fish River, where the coastline can be seen trending north.
- [56:53] This is the Africa known after Diaz's 1488 expedition.
- [57:00] The map is a world map made by the German Henricus Martellus in 1489, held as a manuscript at the British Library.
- [57:06] Another copy of the Martellus map with very much the same geography is at Yale.
- [57:16] The map still shows Ptolemy's truncated South Asia and his very huge Ceylon, Caprobana.
- [57:26] It does include some indication, from Marco Polo, that there are islands off the coast of China.
- [57:39] This illustrates how continents are mapped in a very basic way, and North America was ultimately mapped the same way.
Great Lakes Mapping and Cartographic Borrowing
- [57:50] The interior of continents, illustrated by the Great Lakes, may have been mapped differently from the Mediterranean circuit method.
- [58:03] Mapping the Great Lakes by making a circuit of each lake and stringing the measurements together would have been a tall order.
- [58:28] For hundreds of years the only people on these lakes were voyagers in birch bark canoes, so the circuit method did not happen.
- [58:35] The result was fairly crude maps of the Great Lakes; one shown is the first map to show all five Great Lakes.
- [58:42] Near the Straits of Mackinac they knew a big lake opened up but did not know how big it was or where it ended.
- [59:20] There is no such thing as nice linear progressions in cartography; early maps show stumbling and making things up.
- [59:44] Cartographers have always borrowed wildly from other cartographers, and most maps are actually made from other maps.
- [1:00:03] Until very recently, a cartographer asked to map an area first found another map of that area to use as a base map.
Early Maps of the Great Lakes
- [1:00:36] Defining the shape of Michigan's southern and northern peninsulas nearly completes a map of the Great Lakes.
- [1:00:51] Michigan was a hard peninsula to map, showing that progression in cartography is not linear.
- [1:01:05] The first map of Lake Superior dates to 1671, made by the Jesuits and published in the Jesuit relations, though the individual maker is unknown; Father Alouez was one and Father Marquette may have been involved.
- [1:01:22] That 1671 map is a very accurate map of Lake Superior, including Isle Royale and a couple of minor islands, because the Jesuits made a nearly complete circuit of the lake in canoes, estimating distance and taking latitude readings with an astrolabe or quadrant.
- [1:02:01] On early maps Lake Michigan is distorted, appearing at varying angles, like a pendulum.
- [1:02:20] French mapmaker Franck Hollande seems to have relied a little on the Jesuit map, and Italian cartographer Cornelli's 1680s map looks copied from it except made much wider.
- [1:02:52] In the late 17th century, French manuscript maps added imaginary islands to Lake Superior named after influential figures in France, and those islands were picked up on later maps.
- [1:03:22] Hennepin was generally not considered a very reliable traveler or cartographer, while D'Elia was one of the best map makers and clearly used the Jesuit map for Lake Superior.
- [1:03:51] Captain Cyprian Southack's 1717 Boston map was the first map of North America published in America, but its Great Lakes are very strange and the source is unknown.
- [1:04:09] Henry Popple's map is one of the best 18th-century maps of North America, but on Lake Superior it adds three to five islands named after French officials to flatter them.
- [1:05:00] The Mitchell map, perhaps the most important 18th-century map of North America, was used in 1783 by the commissioners in Paris who drew the Treaty of Peace and marked the border with a red line.
- [1:05:31] The Newberry's colored copy of the Mitchell map shows the southern colonies' western borders extending to the Pacific according to their colonial charters.
John Cary's Maps and the Nonexistent Islands
- [1:06:32] Focus shifts to maps by English cartographer John Cary, who published a series of US regional maps beginning in 1805.
- [1:06:51] Cary's maps still show the fake islands, including Isle Royale and Isle Philippot.
- [1:07:00] The Mitchell map was used to draw the Treaty of Peace border line.
- [1:07:26] The treaty cited two islands, Philippot and Pontchartrain, that did not exist.
- [1:07:44] For about 70 years the British and Americans argued over which islands the treaty meant.
- [1:07:54] It was not until the 1840s that it was ruled those islands did not exist.
- [1:08:02] Cary's 1805 map still shows the border crossing the non-existent island.
- [1:08:12] Cary's 1805 map would have served fine, except Ohio became a state in 1805, so later editions had to add Ohio.
- [1:08:34] By 1825 Ohio, Indiana, and Illinois had all become states and had to be fit in without better geographic information.
- [1:08:56] On the 1825 map Illinois is landlocked with no lake, and Fort Dearborn in Chicago is placed in Wisconsin.
- [1:09:38] Cary's longitude for the west end of Lake Superior (about 92 degrees west) and the east end of Lake Ontario is accurate.
- [1:09:53] The western border of Pennsylvania is accurate because of the Mason-Dixon line, surveyed on the ground.
Land Surveys and the Northwest Territory Grid
- [1:10:46] Unlike earlier examples, this problem was solved on land by dragging chains and orienting them with compasses.
- [1:11:10] The Northwest Territory was decided to be divided completely into parcels, rather than using the metes and bounds system.
- [1:11:30] They devised a system of public lands of six-mile square townships divided into 36 square sections.
- [1:11:42] This was first done in the Seven Ranges in eastern Ohio in 1787, largely as an experiment.
- [1:12:02] Ohio's land surveys have slightly different orientations and don't match up perfectly, with no standard meridian at first.
- [1:12:15] By the time they reached Indiana, they began establishing a standard meridian for numbering ranges and townships.
- [1:12:30] Indiana and Illinois became states in 1816 and 1818, but their northern parts were lightly populated and lacked township and range surveys.
- [1:13:00] In Illinois by about 1830, a survey extension was made to build the Illinois-Michigan Canal from Chicago to the Illinois River.
- [1:13:25] Only when the survey reached the area around 1830 could the western shore of Lake Michigan be located with considerable certainty and accuracy.
- [1:14:03] Starting with the Mason-Dixon line measured by chain and compass, the general land office surveys were extended west, north, and east and west.
Great Lakes Mapped from Land
[0:00] . I want to thank Jeff and the McClung Museum generally, the staff, for inviting me down here and being such wonderful hosts for the couple days I've been here. How many of you have actually seen the map exhibit? Can you raise your hands? A fair number. Okay. Well, I urge those of you who haven't seen it yet to go and see it. It's a really fine collection of very important maps to be assembled in this, in this spot. Some great maps of North America and the world and some very interesting maps of Tennessee and your area.
[0:40] by all means go and see it and hopefully a few of the things that I'll talk about today will help you to appreciate it more. My topic today, "How did they do that?" comes from what I think is a very basic question that people ask when they look at maps. We've all had the experience of standing in a field or on a seashore and looking out and thinking, now, how would you go about mapping where I'm standing, how could that happen? and uh...
[1:11] The fact of the matter is if we're standing on a flat surface like this and we look out, we can see something like three miles. That is if you're six feet tall. For me it's more like, two and three quarter miles. But that's not really a wide enough scope to get you get you to see much topographic detail. If we climb up to about 500 feet, we increase our visibility to about 27 miles.
[1:43] which is getting far enough to be able to You pick coves and things like that. If we go up to the top of a 10,000 foot mountain, like this is Mount San Jacinto outside of Palm Springs, your visibility extends to about 125 miles. which is on a clear day enough to be able to generate a fairly good sketch of the surrounding area, if you know how to do that. I can't say that I do. If we're at 30,000 feet in an airplane, we can see something like 212 miles.
[2:20] There you really begin to be able to pick out considerable, topographic detail and Many of you who enjoy window seats on your flights, sometimes think that it's like a map going by underneath you. Well, If we go up even higher, this is the Horn of Africa taken from the shuttle Columbia in 1993. at 163 miles up. and we're looking north.
[2:51] There's the Horn of Africa. This little projecting thing, I don't remember the name of it, but it's actually the eastern most point of the African continent. From 163 miles up, you can see about 1,200 miles. So when we get out to the horizon here, we're looking into the middle of the Arabian Peninsula. And there you begin to see a real recognizable piece of geography. In fact, here's a map from the Newberry collections from a Portuguese atlas of about 1565.
[3:23] showing that very area. You see we have the Horn of Africa. There's that little projecting point and there's the Arabian Peninsula. I think that's supposed to be I was going to say it's Mecca, but I guess not. uh, Judah. Judah. That's probably Judah. And if we were to wrap this part of the map on our aerial photograph. we'd see that kind of congruence, which I don't know, I think is pretty amazing. Here you've got the horn. There's this little projecting thing.
[4:02] Here's the island of Socotro, which belongs to Yemen. It's actually out here, but I don't know. It seems to me it's pretty good and it makes me ask the question, How did they do that? This is the famous blue marble picture taken from Apollo 17. in 1972 and they were at a height of 28,000 miles. So here, of course, you can see the entire globe. And on this particular shot, one of the more famous ones from that mission you can actually see the entire continent of Africa except for a little bit obscured by clouds.
[4:47] This is an Italian map by a man named Forlani from about 15, 65. And I think you'll recognize what it shows. And in fact, if we... layer it over That aerial photograph. you see that it fits fairly well. so well that we might ask, how did they do that? This is a map of, how many of you recognize this? I want to turn your head this way. It's New England looking from the east.
[5:24] We're looking west. Here's Cape Cod. This is actually Lake Winnipesaukee in New Hampshire. Here's Rhode Island. I think this is the Connecticut River. It's actually the first map published in America, 1677 in John Hubbard's book. history of New England. We're going to lay it next to a modern, satellite photo and I think you have to agree it's pretty remarkable. I mean, if you start looking at details, well, okay, Nantucket isn't Martha's Vineyard, and Nantucket aren't quite in the right place, and Rhode Island is actually further out there, but Generally speaking, it's not bad.
[6:10] You wonder how they did that. And I want to just have a little local example. Uh-- General Smith's map of the Tennessee comfort, government, I think it's 1825, And of course, you can see Knoxville. And here is the modern satellite image. Now of course I don't want to make any claims that this is an incredibly accurate map, but It does show -- there's Knoxville there -- it does definitely show it's position between these two northeast, southwest trending rivers, and you certainly do see the North, East, southwest trending mountain lines.
[6:51] So-- How did they do that? Well... To begin with, I want to go way back to the ancient, times and uh... answer a question that many people, I don't know, when I grew up I learned that at the time of Columbus everybody thought the world was flat and you know, this kind of thing. The fact is that-- Anybody with any scholarly pretensions or even any practical navigation experience knew very well that the world wasn't flat.
[7:23] But it's a hard thing to realize when you're standing on the world, standing on a beach. And this is a little from a cosmography. 15:24 that attempts to explain to people to give them one proof for the rotundity of the world. And what he's, in effect, saying here is here's the moon. Here's the earth and here's the sun. If the Earth were a-- what, a tetrahedron or something like that. the shadow that the sun cast on the moon would be this shape.
[7:56] If the earth were pyramidal, the shadow would be this shape. If the Earth were a cube, you'd get a shadow like that. But in fact, the Earth is round, and so you get a shadow like that. So it's not Certainly not the case that everybody knew the world was round, but it was well known. And in fact, as long ago as 200 BC, a fellow named Eratosthenes, was able to actually measure I've come up with a pretty good estimate of the actual circumference of the Earth. And this is the way he did that.
[8:34] This is Egypt. He understood, he knew that in Syene, a place which is actually very close to the Aswan Dam, There was a well. And on... a certain day of the year, the sun was said to be directly above that well. And you knew that because if you looked down this very deep well, in the desert, you could see the reflection of the sun. So he did an experiment. uh... body He lived-- Ertasanes lived in Alexandria.
[9:07] And he did an experiment in which on the same day that that well was supposed to be illuminated in that way, He measured the angle. of the shadow cast by a pole, a perpendicular pole, in Alexandria. And through some fairly elementary mathematics, he assumed that, in fact, They were more or less on a north-south line, and in fact, they are more or less on a north-south line. And so he did this experiment. Here's a side view of what he did. Here's the well- Actually, this is graduated in miles. It's about 480 miles.
[9:46] And here in Alexandria, when the sun is - the sun's rays, of course, absolutely parallel because the Sun is so far away and the Earth is so small by comparison. So when the sun's rays penetrated to the bottom of the well in Syene, they cast a shadow this big in Alexandria. and The geometry of it is pretty simple. Um. Thank you. If you measure the angle cast by the shadow, it's the same as this angle here.
[10:16] this sector of the Earth. And he calculated that that was-- Seven and a half. 7.2 degrees or a 50th of a circle. So if you take... uh He reckoned the distance as 5,000 stadia. If you take 5,000 stadia and multiply it by 50, you get-- Uh-- you get a figure which translated into miles is about 24,860 or 24,000 miles.
[10:50] And the actual figure is 24,860. So he's off by 9%, but I think pretty reasonable calculation, considering the instrumentation he had available. We're going to move now quickly to the first The first really... important and in many ways the most influential cartographer who ever lived, and that's Claudius Ptolemy. He lived in the second century AD, worked right around 125 AD.
[11:21] Of course, we don't really know what he looked like, but this is a 16th century imaginary portrait. And Ptolemy was a polymath. He wrote treatises on astronomy, on music, on mathematics. He's actually most known as an astronomer, probably. One of the treatises he wrote was called "Geographia," on geography, by which he meant the mapping of the world, geo- Graphy, the writing of the world.
[11:53] And he conceived-- he knew, of course, the world, the Earth was round, and he-- it was a sphere-- and he conceived that the and this was the general Greek view-- The area in which people live, the oikoumine, was one quarter of a sphere. And they assumed-- They knew a little bit about about what was down here. Well, actually they didn't because here's the top part of Africa. They really didn't know much about that, but they assumed that that there had to be four other pieces of a landscape on this globe to balance it out.
[12:30] Thank you. So he came up with-- one of the things he invented was this projection. This is called Ptolemy's first projection. It's a cylindrical-- projection, and it shows 180 degrees from-- His Western end, which was the Fortunate Isles, People aren't sure whether, some people think it was the Canaries and Madeira. Some people think it was Cape Verde. But whatever it was, it was sort of the farthest out thing in the Atlantic that Ptolemy and other Greek geographers knew of. And-- He drew it 180 degrees, in other words, halfway around the globe.
[13:06] And the extent north and south is from a little bit north of 60 degrees. the parallel of two Li, to-- the parallel opposite Mero. Mero is a town in North Sudan. or was a town in North Sudan at about 15 degrees uh below the equator. There's the, there's the equator. No, I'm sorry, there's the Econaut line. We're all north of the equator here. Thank you. So his second projection is a little more interesting.
[13:40] Suggests a little more of the globular shape. This is Ptolemy's second projection. And... This is the world map. that he came up with. Um And it shows the 180 degrees here, the fortunate isles out here, whatever they are. And you notice Africa is it's, pretty unknown down here. All we knew about was this part. And the assumption was that the Indian Ocean was a closed sea. C. just to orient you a little bit, and of course orient comes from the fact that many older maps were oriented with east at the top, hence orient.
[14:20] But to put you in the picture a little bit, This sort of misshapen thing is the Indian subcontinent. And this is the island of Sri Lanka. So long. This is probably the Mele Peninsula. Thank you. So he came up with a world map and also 26 regional maps. He made a map of Um. He made 10 maps of Europe, 4 maps of Africa, and 12 maps of Asia.
[14:53] Now, how did he place things? He talks actually about how to make a map. And the first thing he says is, well, Because of the earth, You really should start with a big ball. But that's kind of difficult. It would be hard for us today, too, to make to start with a big blank ball. So and then he said the next best thing is to start with a slice of a ball. So you have a big curved surface like that. And then you can make your map on that. But he says that also is difficult. So let's just work with flat paper. So he comes up with these two projections, and he proceeds to plot on them.
[15:26] Thank you. all the places he knew about. in the world. One of the main tools that would have been available at that time was was a quadrant. looking more or less like this, a device that you could sight through on this side and a little weighted plum hung down. And if you cited, say, the North Star, that would read directly to your latitude. Latitude was relatively easy. And in the ancient world, some astronomers had very huge...
[16:00] models of these things, very large operational quadrants. And they could probably read quite quite accurately the latitude. Another way that he determined how far north and south the place was by knowing something about the difference between the longest, the length of day and the length of night at the equator. It's equal. A day is as long as a night. uh... Yes, at certain times of the year.
[16:33] But then as you go north, Here's the day of Miro, that place in northern Sudan. There's a one-hour difference between the longest day and the Shortest date. at Tsai Ing, a place in southern Egypt. There's a-- a two-hour difference. At Alexandria, it's about 3 and 1/2. By the time you get up here to the far north, like Denmark, It's about nine hours or more. So this is the kind of information he would have gathered from Roman legions operating in England and Germany and Spain and France, how long the longest day was in various places.
[17:14] So that would be how he would how he would uh... would set his latitude. So here, this is how he would plot the latitude. He knew that Alexandria... was 31 degrees north. He knew that quite accurately. he calculated that it was about 60 degrees and 30 minutes east of the Fortunate Islands. Now, how would he have known that? He talks about one way, of course, longitude is time. One hour of time is 15 minutes of longitude.
[17:47] And what we've learned, we know now that the most accurate way to understand longitude is to be able to carry an accurate clock from one place to another. Of course, it took thousands of years for that just to be finalized. It wasn't until John Harrison in the 1780s. that they actually had a chronometer accurate enough to carry time that way. But even in Ptolemy's day, he was aware of other solutions. He said if you had accurate information about the timing of eclipses.
[18:18] If you knew that... that an eclipse observed over here in Damascus, happened at midnight and it happened and it was observed at like 1:30 in the morning in Alexandria or I don't know in in Cadiz or something, then you would be able to use that as a as an instant of time and calculate the distance. So, you-- and he had some information like that. There was a little bit of information about eclipses. But a lot of information had been gathered about the distances of places.
[18:50] Of course, the Romans were wandering all over their empire. And they were very active in Britain. a little before Ptolemy's time. And so a place like London was nailed down. And it's probable that most of Ptolemy's longitudes are actually... uh... cobbled together from distance measurements. So from Alexandria here, he would have-- of course, he had access to the Alexandrian library.
[19:24] which was full of information and access presumably to all sorts of Roman records and itineraries and things like that. virtually all of which is lost to us now. But he knew that, for instance, if you went from Alexandria to Algiers or Tunis, that it was so far. They reckoned it was so many Roman miles. He actually had a system whereby if he had an itinerary distance between two places, he knew, of course, that they were far. any road is going to be a little windy, he allowed for one-fifth error. So he said if he had a distance of, of there was 500-- or 500 Roman miles, say, from Alexandria to Tunis, He said, well, OK, I'm going to count that as 400.
[20:12] And then he would establish the-- the longitude of Tunis. or of London, or of some other city. So in a very... in a very slow and painstaking way. I'd like to actually, I'd like to envision Ptolemy as working on one huge map. maybe on a wall or maybe even more conveniently on a floor like this. And having drawn out his projection, and saying, OK, here's Alexandria. And I know Damascus is this far away and it's at this Latitude, then I'm going to say it's here.
[20:49] and gradually shifting back and forth and moving things around he came up with his world map, which you saw earlier. um just a sort of a sideline in a way about the discovery of America Ptolemies, this is a globe made in 1492. by a German named Martin Boeheim, who was working in Portugal. Now, there's no evidence that Columbus ever saw this globe, although If there was one globe, there may have been more. I mean, I'm sure it wasn't a unique object. So it's not at all unlikely that you saw this globe or something like it, you know, at least.
[21:24] This was a concept that was clearly out there. And basically what this globe does is it takes Ptolemy's world and wraps it around. a globe. It happens though that because Ptolemy actually didn't accept Eratosthenes measurement, apparently, for the size of the globe. I don't remember what the reasons were, but he posited a somewhat smaller sphere for the earth. and he actually ended up exaggerating the longitudinal length of the oikumene. So when you wrap Ptolemies a little too large, around a little too small globe, You get a what we would call Pacific Ocean view that looks like this. This is a projection of the Boeheim globe uh... looking with Europe over here, And here's China.
[22:17] And these islands off of China, maybe that's could be the Philippines or some idea of that. Here's Sipangu, which is Japan. This is all information that came from Marco Polo. But what you can see is, I love this example because it shows you exactly what Columbus thought he was doing when he sailed. from Spain, His idea was to sail west until-- and these are the islands, the Canaries and the other islands in the Atlantic. was to sail past all those islands until he hit Other islands, off the coast of China.
[22:53] And indeed, he thought when he hit Hispaniola and those other places that those were some of these islands. I believe the story is that Columbus actually went to his grave thinking that he had, in fact, discovered these-- these East Indies. Thank you. So, um... Thank you. I want to show you in a little more detail how Ptolemy went about mapping, making one of his detailed maps. Ptolemy's first map of Europe, is the British Isles. And interestingly, the His arrangement of these regional maps, starting with the British Isles and the second map being the Iberian Peninsula.
[23:36] tradition became very firmly entrenched so that when the first modern atlas came out in 1570, Abraham Ortelius, He had a world map. And then his first... regional map, was the British Isles. and the second regional map, was Iberia. And in fact, most atlases made until the 20th century followed that pattern. It was Great Britain. It was Spain, then it was France, and then so on. The order kind of...
[24:12] falls apart after that, but that was how influential Ptolemy was. So this is a satellite view of-- of of Great Britain. And this is Ptolemy's map of Great Britain. And-- This is the kind of information that Ptolemy recorded. Lots of place names. OF TOWNS. A number of locations of rivers. We're not to take this interior detail at all seriously, but supposedly the river mouth would have been It's something that he plotted.
[24:50] Um. There are some names of peoples here. sort of general names. This is where the I can't read these names on here, but this is where this tribe lives, and this is where these people live. and a few physical features like some mountains, and even a big forest here in Scotland. Thank you. So how did he do that? Well, he started with a projection of that part of the world. And he put down his best guess as to where London was located, latitude and longitude. The Roman legions, of course, were all over Great Britain, and they undoubtedly had regular-- traveled between all these places and he had itineraries telling him how far certain things were.
[25:33] especially towns. Tamara actually I think is a river in Cornwall. MR. Corinium is-- I have to look at my crib sheet. Corinium is-- Sirincester? Um... Maridunum is a carmarthen in Wales. This is the promontory of Kent, which was apparently fairly well established because it was where the the Roman troops, the Roman ships, that would be the first landfall there in Britain. And so there were a number of places that he had Ratier, is Lester.
[26:09] Diva is Cheshire. Lindum is Lincoln. And Eboracum is York. And he adds the note in his geography that this is where the Sixth Legion. won a victory. So-- There were a number of places that he was able to establish fairly accurately. in relation to one another, where they were. And from these from some of these fixed locations. Some people even think that the Romans had a kind of a triangulation, had a kind of a a standard triangle that they worked off of here in surveying in making maps of England. And Ptolemy may actually have had a map of England that he got from from someone in the army. It's not at all unthinkable.
[26:57] that there was a sketch map and they said, "Yeah, well this is what this Southwest Promontory looks like. So anyway, using the best information he had, he came up with this outline. on his big map. Let's picture it on the floor here. And he also put in the river mouths. They said, well, this river is up here. so many miles north of this spot. point here and you know And so he plotted all these places on his map. Now, if he had just done that, and made these wonderful maps.
[27:29] That would have been enough. had they survived. But the problem with maps then and still today is that they're extremely Fragile. and extremely subject to wear and tear. And any of you who have a a car with a glove compartment, you can testify that, in fact, most maps get used to death, if they're used at all. So had Ptolemy made a big world map on parchment or on papyrus or something. And had he made a set of 26 regional maps, Maybe they would have survived. Maybe copies would have been made.
[28:08] and they would have survived the millennia. But-- and he undoubtedly did make, such maps. I mean he at least made one big map, we know that. But the reason Ptolemy's geography survived is because he digitized it. He took all of these, he started with these latitudes and longitudes of towns, and then he started plotting the a reading off of his book, his base map on the floor, let's say, he started reading off other coordinates. So if you'll follow these dots that I've placed around here, he would say, okay, well at this speed point of this bulge.
[28:47] It's 53 degrees, 30 minutes. Uh... of of latitude and about 22 degrees, 10 minutes of longitude. And he'd write that down. and He'd do this for the river mouths, for the promontories. for all these different features around the island. Um. dozens, perhaps as many as a couple hundred points for the British Isles. And he recorded those in Thank you.
[29:21] Tabular format. like this. This happens to be a Latin manuscript of Ptolemy's Geography. He would have written in Greek, and there are some extant Greek manuscripts. But basically, Ptolemy's geography as we know it, as it came down through the ages consisted of no maps, But-- a a textbook of how to do the projections, and a general description of how to map, and a list of 8,000 coordinates like this.
[29:53] Here's a place. Here's the latitude. and fraction and longitude and fraction. And actually, the way he indicated. uh degrees I mean minutes and, well he didn't really get into seconds, but the way he indicated minutes was, he would say if it was, we would call it 50 degrees 30 minutes, he would say, 50 degrees and a half. And if it was 50 degrees 45 minutes, he would say 50 degrees and a half and a quarter. uh They didn't have the concept of unified fraction.
[30:27] So... that the geography as it came down through the ages consisted of just Uh... data, just numeric, alphanumeric data. digital data, if you will. And it wasn't, there seems, there is some evidence that the Arabs had access to Ptolemy's geography, but it was pretty much lost to Western culture until the late 1200s, I'm sorry, the late 1300s, when a copy was discovered in, Constantinople.
[31:03] a Greek manuscript and a geographer in Constantinople said, here's a direction for how to make a world map. And he proceeded to plot out these eight having drawn We don't know if he did one big map or made regional maps, but he followed Ptolemy's instructions. He plotted out all these 8,000 places and produced This atlas. Well, that was a revolutionary thing. And that atlas very quickly got translated into Latin. and many, many copies were made of it.
[31:35] And it became... it became the first standard atlas of the world. This in about 1400. And it-- In many ways, it stayed the standard atlas of the world for at least 100 years. Ptolemy's geography was one of the first books to be published. The first edition with maps was 1477. a very early illustrated book. And there were multiple editions all through the 16th century. It wasn't until about 1570 when Ortelius came out with his Theatrum Orvis Terrarum, thought of as the first modern atlas. But until that time, at least until the 1520s, Ptolemy's maps from 125 AD, we're pretty much it.
[32:23] for understanding the geography of the world. Thank you. Of course, when the new discoveries happened, they had to think on their feet and there are several maps There's one map in particular I'm thinking of in the exhibit where you see what's basically a Ptolemaic world with some American stuff tacked on it. But to get back to-- to his map of Britain. Many of you may have wondered why Scotland is bent over like that. Um... I haven't read actually anywhere anyone saying this explicitly, but I'm pretty convinced this is what happened. If you turn that bit of Scotland up on end like this, 90 degrees.
[33:06] you'll see that It actually-- is not a bad rendition of Scotland. I mean, you get the basic... peninsula up here, this Moray Firth. You get this peninsula here. these little fjord-like things over on the west side. It's-- It's not bad for... 125 AD, drawn by a guy a couple thousand miles away who never left Alexandria. working from Verbal, uh... Descriptions, probably.
[33:40] But the reason he had to bend it was because of the island of Tuli. You remember that zonal diagram? It showed the sort of northernmost habitable place as the latitude of Thule. Well, truly, this is from a map of 1539 showing this. imaginary island. Some people think it actually might have been Iceland, or possibly some other faraway island in the North Atlantic. Basically, Ptolemy's information went back to Pythias, who said that Thule was six days sail north of Britain and is near the frozen sea. The idea was that when you got that far north, much beyond beyond 60 degrees north that the entire sea was frozen, then it would obviously be uninhabitable.
[34:26] So-- Ptolemy was in a pickle because he had He had a lot of information from the Roman legions about Britain. and about Scotland, and he clearly knew that when you got up here, there was still about this much more to go. But he had the problem that here was his Thule. He had-- He had plotted Thule as this location. And according to Pythias, it had to be It had to be six days sail north of Britain. and if he put it up this way it just didn't fit. So he did what a lot of scientists do today. They try to uh...
[35:05] adjust that you know understand the data and the way that's most that seems to make the most sense. And for him, he tries to preserve the length of Britain while at the same time recognizing that Thule is pretty much the northern limit of of habitation. So he simply bent it. Thank you. That's my view and I challenge anyone. If anyone has another explanation, they're welcome to give it. So anyway, this is Ptolemy's world. The same world that's wrapped around that Boeheim globe, although the Boeheim globe also includes information from Marco Polo, which extends beyond uh... trying out here gives us Japan.
[35:44] Thank you. Moving now to the Mediterranean. Um... We're going to talk about another... great Ptolemies, the discovery of Ptolemies geography in 1400 or thereabouts, is just an epochal thing in the history of cartography. The whole idea of mapping on a grid, latitude and longitude, that all comes from from Ptolemy. But there was another tradition that had started a couple hundred years earlier.
[36:20] that in the Mediterranean that is even-- that is sort of a parallel tradition. And that's the tradition of the portal on chart. This is the first the earliest known copy of a Portland chart. And some of the characteristics of Portland charts, well, they're almost... all was drawn on an animal skin, on vellum. This is the neck of the animal. Can you see the outline here? This is that we're looking at the Mediterranean. Down here is the uh...
[36:52] uh... the uh... Straight of Gibraltar. And here's North Africa, here's the Italian, the boot of Italy, Here's the eastern... the Eastern Shore, the Mediterranean, and actually the Black Sea was almost always included in portal and charts. And the Black Sea has been somewhat eroded here. This map, one of the most important maps in the history of cartography, was found in a Paris junk shop in 1840-something.
[37:26] and now lives in the bibliothek Nassau. Thank you. Here's a detail of-- of the cartesan, as it's called, which shows you in greater detail some of the characteristics. invariably have a circle, a circular, grid If you step back, you can actually see um You can see a couple of great circles here inscribed that have wind roses in the middle and radiating radiating wind lines or rum lines as they're called, R-H-U-M-V.
[38:04] The place names on portal and charts are always written inland. They tried to leave the water spaces as open as possible. Um... Typically, the rum lines were different colors. Some were green, some were red, some charts have black ones. Um... Another characteristic-- oh, they have-- they show-- They showed tiny little rocks. There's another example that I can show you some more. symbols. But-- and the other thing is that there is no up on a portal and chart. There's just no, you can't say, "Oh, this is meant to be up." The lettering, if you'll see, these are meant to be read from that way, And then down here...
[38:45] Thank you. I can't quite make that out. They're still read that way, but over here they're read this way. If you go around an island, you'd have to turn the chart around like that. It didn't really have-- It didn't really have a natural pulpy. Thank you. This is another portal and chart. This is from the Newberry's collection. This is our earliest portal and we have a couple dozen portal and charts and atlases. This is 1456 done by a Rosselli from Majorca, he signs it up here in the neck.
[39:16] And again, it's the outline of-- the Mediterranean with the Black Sea. Some of them also went up-- most of them went up the west coast of Europe, included the British Isles usually. Um... Very often they would put these maps, these flags around the around the border. Um, This, many of the portal and charts that have survived, obviously the Cart-Pizan is a pretty pretty tattered and torn thing and was not probably terribly attractive when it was made.
[39:51] Some of the portal and charts that have survived are very pristine, lovely things that probably were made for for you know, rich clients or for parlor use or library use. But there are some that give evidence of having been to sea, and I think this is one of them. Over here on this side. There are these holes. That's where it was nailed onto a wooden roller. And over here on the neck is a little hole. There would have been a leather thong through there. So you'd roll it up and tie it with that thong.
[40:22] stick it in a cubbyhole on board ship. And it's definitely seen some wear here from being rolled and unrolled. Even some of these flags have obvious signs of ink the-- the pigment having having gotten wet. So I don't know. I like to think this one may actually have gone to sea. Okay. Anyway, How were they used? This is another portal and atlas from the Newberry. It's actually a, this is an atlas, this is an opening of two pages I've had to join the sheets here, the digital copies.
[40:56] But to show you how a mariner might use a Portland chart like this, If you wanted to go from This Melilla, I think it is, on the north coast of Africa. to this point over here, Cabo da Gata. CAP. Yeah, a cape of-- cat cape. He-- In other words, he wanted to sail a course more or less like that. He could draw his course on there or lay a parallel ruler between those places.
[41:27] There's one side of the parallel ruler, and then he'd swing out the other arm of the ruler until he till he lined it up with a wind rose. And in this case, As you can see, That's the north line. North by east. north-northeast, it's actually in between north by east and north-northeast. The mariner starting out from here would try to get his compass to read a little bit east of North by East. hopefully would strike his point.
[41:59] but hopefully not. Not literally, because as a matter of fact, there is a-- There's an indication here that there's a big rock there. And I think if you're familiar with modern nautical charts, Something very like that is used today to indicate a hazard to navigation like a rock, little dots like this to indicate shoals. Some of these portal and charts even have a little ship skeleton to indicate a wreck, a sunken ship.
[42:35] So the main tool was a compass. such as this one. We don't really have any really ancient compasses. The compass was Uh... They used to say that it was invented in China and carried to the Mediterranean. Now people think that It may have been independently invented. But anyway, there's textual evidence that people talking about sailing with compasses sailing by the magnetized needle in the early 1200s. And so that's about the time the cart Pisan comes out, sometime in the late 1200s.
[43:10] The earliest compasses may have been just a needle actually floating on water, held up by surface tension. Sometimes they would push the needle through a straw, And that would keep it afloat, but I'm sure by a very early age they had a They had devised this method of a card with the needle attached underneath. And they would have needed an hourglass or, in some cases, a minute glass or a half-minute glass. And navigators from at least the late Middle Ages up until well into the uh...
[43:46] 18th century, we're using a log and line to gather information about their speed. Basically, you needed-- you needed-- a spool with a lot of line on it. You needed this log here or chip. and you needed a a glass that-- was good for half a minute. And the way it worked was something like this. I think you must have needed at least three men. One guy is holding the log real.
[44:18] Another guy is holding the 30 second glass. And another guy is holding the actual chip here, which is weighted at the bottom. He throws this thing over the back of the ship. And it hits the water and starts bobbing along. And, of course, the water catches it here, so it's... sort of riding up in the water. And he waits until... Uh-- about the length of the ship. There's a red rag tide there, and that indicates that the thing is now far enough behind the ship so that it's free of the wake of the ship and supposedly it's it's kind of digging into more untroubled waters.
[44:57] And when that red line goes over, the goes over the rail, he says, "Turn." And the guy with the 30-second glass turns the glass, And then they start counting how many knots go over. And the knots are placed, well... Apparently there were a couple different lengths of knot, but the knots are placed at regular intervals along there. You count how many knots go over and when the glass runs out, the guy says stop. And then the guy holding the reel holds it. They count how many knots have gone over.
[45:30] and they record that information. on this device, which is a Travers board. and This is a wonderfully simple device that It didn't require any great learning. An illiterate seaman could use it as long as he was familiar with the points of the compass and could read the numbers, I guess, from 1 to 12. The idea is this: here are all the points of the compass that you could possibly steer each of these concentric rows of circles is a half hour.
[46:05] So this would be the first half hour of a watch. the second half hour, the third half hour, and so on. up to the four hour watch. a very standard way of breaking up the day at sea. from early on. And attached to the middle, there is a cord. and you have a bunch of little pegs. to go along with it, which you can push next to the cord into a hole. So what this tells us is that in the first half hour of the watch, They were sailing north by West.
[46:40] on that course. And in the second half hour of the watch, they were still sailing north by west. But when the Third half hour came along, they had shifted their course to-- this point of the compass. And in the fourth half hour-- After two hours of sailing, They had shifted it to this point. So you'd keep doing this, and for the four hours of a watch, you'd have a perfect record of the course you had steered. Now, how fast were you going? Well, every hour they would do this business with the log.
[47:14] the chip log. And they would plot those down here. Each of these lines is one hour of the watch. First hour. second hour. Third hour. the fourth dollar. What this tells us is that in the first hour of the watch, They were going six knots. So they put the little peg there. In the second hour of the watch, I'm doing all this pointing, and I made this elaborate slide to show you this. I forgot about it. Um... So there's the first hour, 6 knots. In the second hour, 8 knots, but a little more than 8 knots.
[47:54] Eight and a half knots. they could record down to the quarter of a knot. So that's a fairly accurate example estimate of your speed. So at the end of a four hour watch, the seaman could hand this board over to the captain and or whoever was-- keeping records. and they would have a complete record of distance and direction and speed FOR-- for that watch, which they could write down into a log. Well, um... How did Portland-- I see-- Jeff looking at his watch. Yeah, okay, that clock is right. I'm doing all right.
[48:31] How did-- How did this information get recorded? Ultimately, a lot of A lot of this, of Siemens information about distances from ports and things like that, got recorded in itinerary form like this. It's strictly-- well, I will say, I will call it, again, a digital record. I mean, it certainly uses numbers. Here's a Roman-- there are Roman numerals in here, and alphanumeric characters to record certain information. And this is the kind of information they record. These are called Portolani.
[49:07] books of sailing directions between ports. And this is the most famous Portolani painting. is the Compasso de Navigare from the, again, the late 1200s. And here's just one of the indications that go from Fennaro, this port, to Felia. It's 30 miles to the northwest. And then there's sometimes notes about about the place, but it's just one thing like that after another going around the whole course of the Mediterranean and the Black Sea.
[49:44] That's what's in the Compasso del Navigare. Now, people have long-- imagined that there had to be some connection between these these portalani, these books of directions like that, and the finished portal and charts. But it wasn't until-- A couple decades ago, there had a retired physician. Jonathan Landman, actually took the trouble to convert all of the measurements, all of the information in the Compasso da Navigare into into distances, standard distances and directions. He took, when he read Northwest, he turned that into so many degrees. When he read North by Northwest, he converted that into so many degrees. And then he plotted down the distances and those bearings and started to see what would happen.
[50:38] And in fact, he discovered that-- the Compasso del Navigare, If you plot down all those distances and directions, It does, in fact... I didn't mean to do that. What do I do? Just do this. It does in fact generate a map of the Mediterranean. Now, of course, it didn't... come out exactly like this. Any of you know anything about surveying know that there's something called error of closure whenever you survey around an area.
[51:17] it's not going to end up perfectly like that. some of this may be way down here or something. But as long as you're working with a closed area And this is virtually closed here at the Strait of Gibraltar. you know how to adjust it. So you just kind of adjust a little bit on every on every angle to make it fit like this. Well, how close was it? Well... Pretty close. There's the modern outline of the Mediterranean. So, we're pretty sure this is how the basic portal and chart was generated from these from these tables, really, or verbal lists of distances and directions.
[51:58] And of course it didn't happen all at once like that. It wasn't that somebody There was suddenly this Compasso della Navagari and somebody took that and plotted it and voila, Portland chart. I mean, it must have been a long procedure involving many, many errors and many mistakes many partial maps, I suppose, of different areas. But it's pretty clear, I think, that that is the -- That is the-- the source arm And now I'm going to say a little bit about a more continental approach.
[52:33] the The Mediterranean, we discovered, is pretty much mapped through very accurate, very small-scale Uh-- measurements of distance and direction around the perimeter. Um-- Much the same thing using many of the same instruments is happening on a larger scale when we come to a continent. One early map of this part of Africa. Now we're going to look at the-- at the young some of the Portuguese efforts to map the West Coast of Africa. Now, one other instrument that would have been involved besides the quadrant that we saw, Ptolemy was holding a quadrant, There was an instrument called the cross staff, which works the same way. You cite an object and you align this bar of this thing with the horizon.
[53:25] and this top of the bar with whatever you're citing, North Star or Sun, and you read an angle off of this sliding bar. Um. There's a model in the exhibit here. There are lots of wonderful instruments in this exhibit that are Some of which I've never seen before, very neat. addition to the exhibit. And in there is a backstaff, which is the same principle as this cross-staff, but instead of having to look directly at the sun. you turn your back to the sun, and this has a little mirror on it here, or a little vein, and you can read the shadow.
[54:01] the shadow of the sun instead of directly. accomplishes the same thing. So using logs and lines and, um, instruments like the quadrant or the cross staff to measure latitude and Um... the Portuguese gradually began to map Africa. Now this is a portion of a 1489 map, and I've trimmed everything else away. except what Ptolemy knew. This is pretty much the Africa that Ptolemy knew.
[54:32] It consisted of the northwest, the north coast here, the North Shore of the Mediterranean. You know about the Atlas Mountains. He knew about the Nile, and they knew, or... thought they knew that the Nile had its source in the mountains of the moon, somewhere way down south in Africa. They also-- knew or thought they knew about some big lakes here, which I have no doubt were uh, Lake Victoria and Lake Nyazaland, you know, or whatever.
[55:03] like our-- just, you know, The word was there were big lakes down there towards the end of the Nile. So that was Ptolemy's Africa. Well-- by the time the Portuguese really started to make a a dedicated effort to try to see if they could get around Africa, if it was in fact Um. if it in fact did not enclose the the Indian Ocean. they started to sail down the West Coast and This is...
[55:37] This was a very long process. 1432, another A few years later, they get a little further to the River of Gold. Um... Now we're-- 10 years later. Here we are. A long time later, It took the Portuguese-- something like 50 years. to get to get the bulge of Africa really nailed down.
[56:11] But, and so they would have done this in exactly the same way by getting-- by getting latitude readings on these various river mouths and things like that and then by keeping track of their distances and directions. And finally, the big push to see if they couldn't get around the continent, and in 1485, no 1480 seven, eight, Bartolomeo Diaz actually rounds the cape of good faith.
[56:44] hope and gets as far as the Great Fish River, where he can see the coastline trending north. So this is the Africa that-- that is known after Diaz's expedition in 1488, and in fact this map is a world map. made by a German called Henricus Martellus in 1489. This is a manuscript at the British Library. There's another copy of the Martellus map, which with very much the same geography at Yale.
[57:16] And of course, you can see this is still Ptolemy's truncated South Asia and his very huge Ceylon, Caprobana. And the -- but here it does have some indication that there is from Marco Polo that there are these islands off the coast of China. So that is... That is how continents are mapped in a very basic way, and that is how North America ultimately was mapped too. Now, I want to conclude with a-- a case study of how-- how the interior of continents might have been mapped.
[57:53] or was in this case how it was mapped. These are the Great Lakes. OF COURSE. And I think you can see that it would be-- It would be a much different proposition to try to map the Great Lakes by coming in here and making a circuit of the lake and then measuring this distance down here and they're making a circuit of this lake and circuit of this lake and stringing those all together into a, you know, in the way we did with the Mediterranean, that would have been a tall order. And in fact, it didn't happen because the only people On these lakes for hundreds of years were voyagers in birch bark canoes.
[58:34] So-- You ended up with fairly crude maps of the Great Lakes. This is actually the first map to show all five of the Great Lakes. And you can see Lake Superior, they obviously were up here in in near this traits of Mackinaw and They knew there was a big lake opening up there, but they didn't know. how big or where it ended. This is presumably-- Lake Michigan, although Lac de Pouin, the name of Green Bay is usually Bay de Pouin, So that would be Lake Michigan, Huron, Ontario and Erie.
[59:09] But I'm showing you a series of maps attempt to represent the Great Lakes to show you that There's no such thing as as uh... nice linear progressions in cartography. We like to think that in general, you know, every map is an improvement on the last map and, you know, and I suppose in some cases that is the case. But if you look at a lot of early maps, you'll see a lot of a lot of stumbling, a lot of just plain I don't know, making things up.
[59:44] Cartographers have always borrowed wildly from other cartographers. I mean, until Until very recently, when we can actually go to something like Google Earth or Google NASA and get or the sub-- digital image laboratory and get up TODAY. photographs of the Earth's surface until very recently, When a cartographer was asked to make a map of such and such area, the first thing he did was find another map of that area. and use it as a base map and maybe adapt it or change the scale or something like that.
[1:00:14] Most maps are actually made from other maps. And-- At this time, two people were copying each other. So as we go through these various images, of the Great Lakes, you'll see some some things that look the same, you'll say, "Oh, that looks like he copied that from so-and-so." One of the things that I'm always interested in is when it comes to the Great Lakes, If you can define the shape of Michigan, both its southern peninsula and its northern peninsula. You have almost completed a map of the Great Lakes.
[1:00:46] And if you'll watch Michigan through this series of slides, I think you'll see that It was a very hard little peninsula to map. Surprisingly, this is a nice example of how uh... progression is not linear in cartography. This happens to be a very early-- in fact, the first map of like superiors. 1671. We know it was done by the Jesuits. It's published in the Jesuit relations. We don't really know who did it. Father Alouez was one. Father Marquette may actually have been involved. He was up here at at the mission on the Apostle Islands.
[1:01:22] But it's actually a very accurate map of Lake Superior. It has Isle Royale here. It has just a couple of little minor islands that are actually there. And the reason they were able to do this is we know that the Jesuits actually made a pretty much complete circuit. of the lake in canoes. Yeah. Counting paddle strokes perhaps, I don't know, but estimating the distance in some way. and taking readings of latitude.
[1:01:55] with an astrolabe or with a quadrant. Um... Here again, Michigan is a little distorted. Look at Lake Michigan. On many of these early maps, actually there are some where it's, It's swinging way less weight. Some where it's almost straight up and down, and some where it's way over at this angle. Michigan is like a pendulum. Um... Franck Hollande, very influential French mapmaker. He seems to have relied, I think, a little bit on the Jesuit map. He knew about it anyway.
[1:02:28] um... cornelli Italian cartographer, 1680s. MR. This looks like it's copied from the Jesuit map, except for some reason he thought he had to make it much wider. Bye. Thank you. Um. Some fairly outlandish figures here. where this comes from. This is the beginning of the of adding islands to Lake Superior. In the late 17th century, there were a couple of French manuscript maps made that just suddenly put in imaginary islands and named them after influential characters in France. And those islands got picked up on later maps. It's always the bad stuff that gets copied.
[1:03:13] First. So-- Um... These depictions, I don't know where they come from. Hennepin was generally not considered very reliable traveler or cartographer. D'Elia was one of the best map makers. And actually, it's not a bad representation of the Great Lakes. He's clearly using the Jesuit map here. for Lake Superior. And Lake Michigan is actually fairly reasonably oriented. uh... herman mall one of the more imaginative cartographers.
[1:03:51] Captain Cyprian Southak, the first First map of North America published in America. published in Boston in 1717, but Where he got his Great Lakes from, I do not know. Very strange. I don't think there was a model for that. Um. Popple, a part of Henry Popple's map, the southern sheets showing the Gulf of Mexico is in the exhibit. One of the-- one of the best maps of North America. in the 18th century.
[1:04:22] I have fairly reasonable... Michigan and Lake Michigan, but Notice Lake Superior. Here he's got Isle Royale and then here's Isle Filippo Pontchartrain, and I can't quite read it, but there were three or four or five islands just thrown in there to flatter the French officials. In fact, each one is named after another official. It's nice to have an island named after you. Thank you. Here again, Lake Michigan, way off to the southwest.
[1:04:55] Michigan Peninsula, just a little point. This is the Mitchell map, the second, maybe the most important 18th century map of North America. most important map in American history. largely because this is the map that in 1783 was laying in front of the the commissioners in Paris who drew the Treaty of Peace, and they drew a red line on this map showing the border. dividing the United States from-- British colonies.
[1:05:27] Mitchell's map is interesting in that this is the This is actually the Newberry's copy. badly reproduced, but our copy is colored so that you can see that the uh... the uh... colonies were, at least the southern colonies were shown with their western borders extending to the Pacific, according to the colonial charters. There's a wonderful copy of the Mitchell map upstairs in the exhibit too. It isn't colored quite this dramatically. If you see, the Charter of North Carolina was supposed to extend to the Pacific. Now if you're wondering where where Western Tennessee would have been had that actually happened. This is how it would sort out. Monterey would be in West Tennessee and San Luis Obispo, nice wine country in there.
[1:06:22] Could have been great. um So a couple more maps. Ah... attempting to show the Great Lakes. I'm going to concentrate on a couple of maps by this English cartographer named John Kerry. who publishes a series of maps. of regions of the United States like this. beginning in 18.5. and I guess if you look at the great, well they're recognizable and he's gotten rid of the fake-- no, he hasn't gotten rid of the fake islands. They're still there.
[1:06:54] There's Royale, but there's Philippot. In fact, this actually... Um... went back to the Mitchell map. The Mitchell map was used as I said to draw the Treaty of Peace. Can I get back there? How far away was it? Um. It's when they drew the line for the border, they drew it up here and they said, okay, They drew it across this island and to Isle Royale. And they went south of Isle Royale. And then they went up a river here. And in the treaty it said, Uh...
[1:07:26] It said north of the isles Philippot and Pontchartrain. and Isle Royale or something. And so they cited in the actual treaty document two islands that just didn't exist. And so for the next uh 70 years. They were looking and the British were arguing that, "Oh, this is what Isle Pontchartrain was." And the Americans said, "No, no, no, it was this island." Finally, it took a long-- it wasn't until the 1840s when they finally ruled that, in fact, those islands didn't exist.
[1:08:02] But here they are, 1805, it still shows the border going across the non-existent. Island. So anyway, this is Cary's 1805 map. And that would have served fine, except when in 1805, Ohio became a state. And so in later editions, he had to add Ohio. Here, the general geography is pretty good. There's Chicago. The portage. St. Joseph, Michigan. Detroit. Thank you. Thank you.
[1:08:34] But when he got to 1825, By that time, there were already-- Ohio had become a state. Indiana had become a state. Illinois had become a state. And He had to fit them in somehow. He didn't change the basic geography. He didn't have any better information. But-- you can see it gave him some problems because Here, for instance, is the bottom of Lake Michigan. Um, Well, Illinois, first of all, is landlocked. It has no lake. This is Illinois. Um...
[1:09:05] Fort Dearborn in Chicago is in Wisconsin, California. what's not Wisconsin. Um, Indiana is here. It just, it was very hard to fit in. And the reason was he had He actually had a very good observation for the Oh, yeah. This is... indicating his basic difficulties. How do you fit three states? like that. into that space between the Mississippi and the western border of Pennsylvania.
[1:09:36] Thank you. Thank you. Now he knew for a certainty about, he actually, his longitude for the west end of Lake Superior is pretty good. It's actually right about 92 degrees west, which is what he shows. His longitude for the east end of Lake Ontario is also Right on. also the western border of Pennsylvania. The reason that's right on is because of the Mason-Dixon line. which of course was surveyed on the ground with guys lugging chains and blazing through trees and making paths.
[1:10:07] and marking on the ground the how many hundred miles to the western border of Pennsylvania. So he had those three people those things pretty well fixed. But he was very vague about the Mississippi River. There weren't any accurate observations out there. and this this lake system in here was just uh, Very, very-- little known. That's the western border of Ohio. This is the western border of Indiana, and this is the westernmost bulge of the of Illinois on the Mississippi.
[1:10:45] So how did this... little problem gets solved. Well, unlike our other examples, it wasn't solved from the water. It was solved on land, and it was solved by people dragging chains like this. across the country and orienting them with compasses like this. The general-- in the Northwest Territory, which was this area here. was was decided to divide it completely, into parcels. Of course, you folks down here, you have the meets and bounds system, where you just sort of said from this tree to that rock to the river and then back.
[1:11:24] but they decided they wanted something a little more orderly for the Northwest Territories, and so they devised this... system of public lands consisting of six-mile square townships and divided into 36. square sections. And they first did this in the very early eastern part of Ohio in what was called the Seven Ranges. That was done in 1787. They were just kind of experimenting, really. They didn't quite know how they were going to expand this grid across the Northwest Territories, And Ohio is really very much a...
[1:12:00] experiment. If you look at the the land surveys of Ohio. There are slightly different orientations and they don't match up perfectly. They didn't really have a standard meridian. But by the time they got into Indiana, they started establishing a standard meridian. So you'd have one north-south line there, where you would number all the ranges and all the townships. And Indiana and Illinois were both settled from the south. So, They became states 1816, 1818. But at the time they attained statehood, All the whole northern part of the states were or on Well, they weren't unpopulated, but they were lightly populated.
[1:12:46] did not have the benefit of the township and range surveys. In Illinois-- uh... by eighteen 30 about, they had actually surveyed a little extension up here because They wanted to build a canal from Chicago down to the Illinois River, the Illinois-Michigan Canal. And so they divided that. and the federal government started getting rid of that land. Meanwhile, on either side of it, it was still Indian territory. country. So as these surveys progressed, they bumped up into the water.
[1:13:21] And it was only really when This survey got up here in about 1830. that they were able to say, with considerable certainty and accuracy This is where... the western shore of Lake Michigan hits at that point. And as the survey Continues. Wisconsin becomes a state in '48. gradually the entire lower peninsula of Michigan, and of course the entire Lake Michigan, and the location of the Mississippi River, They're all determined.
[1:13:55] accurately by measurements on the ground. Briefly, this is what happened. Starting with the Mason-Dixon line, which after all starts in tidewater, and was measured uh... by chain, and compass and then extending the general land office surveys west and north. and east and west. They finally... were able to determine the outline of the Great Lakes. And that's how this little bit of geography got mapped, strictly from the land.
[1:14:35] So... That's all I have to say, but I'm happy to answer questions if you have any. I'll try to answer them, that is. Yes? Thank you.
查看原始字幕
[0:00] . I want to thank Jeff and the McClung Museum generally, the staff, for inviting me down here and being such wonderful hosts for the couple days I've been here. How many of you have actually seen the map exhibit? Can you raise your hands? A fair number. Okay. Well, I urge those of you who haven't seen it yet to go and see it. It's a really fine collection of very important maps to be assembled in this, in this spot. Some great maps of North America and the world and some very interesting maps of Tennessee and your area.
[0:40] by all means go and see it and hopefully a few of the things that I'll talk about today will help you to appreciate it more. My topic today, "How did they do that?" comes from what I think is a very basic question that people ask when they look at maps. We've all had the experience of standing in a field or on a seashore and looking out and thinking, now, how would you go about mapping where I'm standing, how could that happen? and uh...
[1:11] The fact of the matter is if we're standing on a flat surface like this and we look out, we can see something like three miles. That is if you're six feet tall. For me it's more like, two and three quarter miles. But that's not really a wide enough scope to get you get you to see much topographic detail. If we climb up to about 500 feet, we increase our visibility to about 27 miles.
[1:43] which is getting far enough to be able to You pick coves and things like that. If we go up to the top of a 10,000 foot mountain, like this is Mount San Jacinto outside of Palm Springs, your visibility extends to about 125 miles. which is on a clear day enough to be able to generate a fairly good sketch of the surrounding area, if you know how to do that. I can't say that I do. If we're at 30,000 feet in an airplane, we can see something like 212 miles.
[2:20] There you really begin to be able to pick out considerable, topographic detail and Many of you who enjoy window seats on your flights, sometimes think that it's like a map going by underneath you. Well, If we go up even higher, this is the Horn of Africa taken from the shuttle Columbia in 1993. at 163 miles up. and we're looking north.
[2:51] There's the Horn of Africa. This little projecting thing, I don't remember the name of it, but it's actually the eastern most point of the African continent. From 163 miles up, you can see about 1,200 miles. So when we get out to the horizon here, we're looking into the middle of the Arabian Peninsula. And there you begin to see a real recognizable piece of geography. In fact, here's a map from the Newberry collections from a Portuguese atlas of about 1565.
[3:23] showing that very area. You see we have the Horn of Africa. There's that little projecting point and there's the Arabian Peninsula. I think that's supposed to be I was going to say it's Mecca, but I guess not. uh, Judah. Judah. That's probably Judah. And if we were to wrap this part of the map on our aerial photograph. we'd see that kind of congruence, which I don't know, I think is pretty amazing. Here you've got the horn. There's this little projecting thing.
[4:02] Here's the island of Socotro, which belongs to Yemen. It's actually out here, but I don't know. It seems to me it's pretty good and it makes me ask the question, How did they do that? This is the famous blue marble picture taken from Apollo 17. in 1972 and they were at a height of 28,000 miles. So here, of course, you can see the entire globe. And on this particular shot, one of the more famous ones from that mission you can actually see the entire continent of Africa except for a little bit obscured by clouds.
[4:47] This is an Italian map by a man named Forlani from about 15, 65. And I think you'll recognize what it shows. And in fact, if we... layer it over That aerial photograph. you see that it fits fairly well. so well that we might ask, how did they do that? This is a map of, how many of you recognize this? I want to turn your head this way. It's New England looking from the east.
[5:24] We're looking west. Here's Cape Cod. This is actually Lake Winnipesaukee in New Hampshire. Here's Rhode Island. I think this is the Connecticut River. It's actually the first map published in America, 1677 in John Hubbard's book. history of New England. We're going to lay it next to a modern, satellite photo and I think you have to agree it's pretty remarkable I mean if you start looking at details well okay Nantucket isn't Martha's Vineyard and Nantucket aren't quite in the right place and Rhode Island is actually further out there but Generally speaking, it's not bad.
[6:10] You wonder how they did that. And I want to just have a little local example. Uh-- General Smith's map of the Tennessee comfort, government, I think it's 1825, And of course, you can see Knoxville. And here is the modern satellite image. Now of course I don't want to make any claims that this is an incredibly accurate map, but It does show -- there's Knoxville there -- it does definitely show it's position between these two northeast, southwest trending rivers, and you certainly do see the North, East, southwest trending mountain lines.
[6:51] So-- How did they do that? Well... To begin with, I want to go way back to the ancient, times and uh... answer a question that many people, I don't know, when I grew up I learned that at the time of Columbus everybody thought the world was flat and you know, this kind of thing. The fact is that-- Anybody with any scholarly pretensions or even any practical navigation experience knew very well that the world wasn't flat.
[7:23] But it's a hard thing to realize when you're standing on the world, standing on a beach. And this is a little from a cosmography. 15:24 that attempts to explain to people to give them one proof for the rotundity of the world. And what he's, in effect, saying here is here's the moon. Here's the earth and here's the sun. If the Earth were a-- what, a tetrahedron or something like that. the shadow that the sun cast on the moon would be this shape.
[7:56] If the earth were pyramidal, the shadow would be this shape. If the Earth were a cube, you'd get a shadow like that. But in fact, the Earth is round, and so you get a shadow like that. So it's not Certainly not the case that everybody knew the world was round, but it was well known. And in fact, as long ago as 200 BC, a fellow named Eratosthenes, was able to actually measure I've come up with a pretty good estimate of the actual circumference of the Earth. And this is the way he did that.
[8:34] This is Egypt. He understood, he knew that in Syene, a place which is actually very close to the Aswan Dam, There was a well. And on... a certain day of the year, the sun was said to be directly above that well. And you knew that because if you looked down this very deep well, in the desert, you could see the reflection of the sun. So he did an experiment. uh... body He lived-- Ertasanes lived in Alexandria.
[9:07] And he did an experiment in which on the same day that that well was supposed to be illuminated in that way, He measured the angle. of the shadow cast by a pole, a perpendicular pole, in Alexandria. And through some fairly elementary mathematics, he assumed that, in fact, They were more or less on a north-south line, and in fact, they are more or less on a north-south line. And so he did this experiment. Here's a side view of what he did. Here's the well- Actually, this is graduated in miles. It's about 480 miles.
[9:46] And here in Alexandria, when the sun is - the sun's rays, of course, absolutely parallel because the Sun is so far away and the Earth is so small by comparison. So when the sun's rays penetrated to the bottom of the well in Syene, they cast a shadow this big in Alexandria. and The geometry of it is pretty simple. Um. Thank you. If you measure the angle cast by the shadow, it's the same as this angle here.
[10:16] this sector of the Earth. And he calculated that that was-- Seven and a half. 7.2 degrees or a 50th of a circle. So if you take... uh He reckoned the distance as 5,000 stadia. If you take 5,000 stadia and multiply it by 50, you get-- Uh-- you get a figure which translated into miles is about 24,860 or 24,000 miles.
[10:50] And the actual figure is 24,860. So he's off by 9%, but I think pretty reasonable calculation, considering the instrumentation he had available. We're going to move now quickly to the first The first really... important and in many ways the most influential cartographer who ever lived, and that's Claudius Ptolemy. He lived in the second century AD, worked right around 125 AD.
[11:21] Of course, we don't really know what he looked like, but this is a 16th century imaginary portrait. And Ptolemy was a polymath. He wrote treatises on astronomy, on music, on mathematics. He's actually most known as an astronomer, probably. One of the treatises he wrote was called "Geographia," on geography, by which he meant the mapping of the world, geo- Graphy, the writing of the world.
[11:53] And he conceived-- he knew, of course, the world, the Earth was round, and he-- it was a sphere-- and he conceived that the and this was the general Greek view-- The area in which people live, the oikoumine, was one quarter of a sphere. And they assumed-- They knew a little bit about about what was down here. Well, actually they didn't because here's the top part of Africa. They really didn't know much about that, but they assumed that that there had to be four other pieces of a landscape on this globe to balance it out.
[12:30] Thank you. So he came up with-- one of the things he invented was this projection. This is called Ptolemy's first projection. It's a cylindrical-- projection, and it shows 180 degrees from-- His Western end, which was the Fortunate Isles, People aren't sure whether, some people think it was the Canaries and Madeira. Some people think it was Cape Verde. But whatever it was, it was sort of the farthest out thing in the Atlantic that Ptolemy and other Greek geographers knew of And-- He drew it 180 degrees, in other words, halfway around the globe.
[13:06] And the extent north and south is from a little bit north of 60 degrees. the parallel of two Li, to-- the parallel opposite Mero. Mero is a town in North Sudan. or was a town in North Sudan at about 15 degrees uh below the equator. There's the, there's the equator. No, I'm sorry, there's the Econaut line. We're all north of the equator here. Thank you. So his second projection is a little more interesting.
[13:40] Suggests a little more of the globular shape. This is Ptolemy's second projection. And... This is the world map. that he came up with. Um And it shows the 180 degrees here, the fortunate isles out here, whatever they are. And you notice Africa is it's, pretty unknown down here. All we knew about was this part. And the assumption was that the Indian Ocean was a closed sea. C. just to orient you a little bit, and of course orient comes from the fact that many older maps were oriented with east at the top, hence orient.
[14:20] But to put you in the picture a little bit, This sort of misshapen thing is the Indian subcontinent. And this is the island of Sri Lanka. So long. This is probably the Mele Peninsula. Thank you. So he came up with a world map and also 26 regional maps. He made a map of Um. He made 10 maps of Europe, 4 maps of Africa, and 12 maps of Asia.
[14:53] Now, how did he place things? He talks actually about how to make a map. And the first thing he says is, well, Because of the earth, You really should start with a big ball. But that's kind of difficult. It would be hard for us today, too, to make to start with a big blank ball. So and then he said the next best thing is to start with a slice of a ball. So you have a big curved surface like that. And then you can make your map on that. But he says that also is difficult. So let's just work with flat paper. So he comes up with these two projections, and he proceeds to plot on them.
[15:26] Thank you. all the places he knew about. in the world. One of the main tools that would have been available at that time was was a quadrant. looking more or less like this, a device that you could sight through on this side and a little weighted plum hung down And if you cited, say, the North Star, that would read directly to your latitude. Latitude was relatively easy. And in the ancient world, some astronomers had very huge...
[16:00] models of these things, very large operational quadrants. And they could probably read quite quite accurately the latitude. Another way that he determined how far north and south the place was by knowing something about the difference between the longest, the length of day and the length of night at the equator. It's equal. A day is as long as a night. uh... Yes, at certain times of the year.
[16:33] But then as you go north, Here's the day of Miro, that place in northern Sudan. There's a one-hour difference between the longest day and the Shortest date. at Tsai Ing, a place in southern Egypt. There's a-- a two-hour difference. At Alexandria, it's about 3 and 1/2. By the time you get up here to the far north, like Denmark, It's about nine hours or more. So this is the kind of information he would have gathered from Roman legions operating in England and Germany and Spain and France, how long the longest day was in various places.
[17:14] So that would be how he would how he would uh... would set his latitude. So here, this is how he would plot the latitude. He knew that Alexandria... was 31 degrees north. He knew that quite accurately. he calculated that it was about 60 degrees and 30 minutes east of the Fortunate Islands. Now, how would he have known that? He talks about one way, of course, longitude is time. One hour of time is 15 minutes of longitude.
[17:47] And what we've learned, we know now that the most accurate way to understand longitude is to be able to carry an accurate clock from one place to another. Of course, it took thousands of years for that just to be finalized. It wasn't until John Harrison in the 1780s. that they actually had a chronometer accurate enough to carry time that way. But even in Ptolemy's day, he was aware of other solutions. He said if you had accurate information about the timing of eclipses.
[18:18] If you knew that... that an eclipse observed over here in Damascus, happened at midnight and it happened and it was observed at like 1:30 in the morning in Alexandria or I don't know in in Cadiz or something, then you would be able to use that as a as an instant of time and calculate the distance. So, you-- and he had some information like that. There was a little bit of information about eclipses. But a lot of information had been gathered about the distances of places.
[18:50] Of course, the Romans were wandering all over their empire. And they were very active in Britain. a little before Ptolemy's time. And so a place like London was nailed down. And it's probable that most of Ptolemy's longitudes are actually... uh... cobbled together from distance measurements. So from Alexandria here, he would have-- of course, he had access to the Alexandrian library.
[19:24] which was full of information and access presumably to all sorts of Roman records and itineraries and things like that. virtually all of which is lost to us now. But he knew that, for instance, if you went from Alexandria to Algiers or Tunis, that it was so far. They reckoned it was so many Roman miles. He actually had a system whereby if he had an itinerary distance between two places, he knew, of course, that they were far. any road is going to be a little windy, he allowed for one-fifth error. So he said if he had a distance of, of there was 500-- or 500 Roman miles, say, from Alexandria to Tunis, He said, well, OK, I'm going to count that as 400.
[20:12] And then he would establish the-- the longitude of Tunis. or of London, or of some other city. So in a very... in a very slow and painstaking way. I'd like to actually, I'd like to envision Ptolemy as working on one huge map. maybe on a wall or maybe even more conveniently on a floor like this. And having drawn out his projection, and saying, OK, here's Alexandria. And I know Damascus is this far away and it's at this Latitude, then I'm going to say it's here.
[20:49] and gradually shifting back and forth and moving things around he came up with his world map, which you saw earlier. um just a sort of a sideline in a way about the discovery of America Ptolemies, this is a globe made in 1492. by a German named Martin Boeheim, who was working in Portugal. Now, there's no evidence that Columbus ever saw this globe, although If there was one globe, there may have been more. I mean, I'm sure it wasn't a unique object. So it's not at all unlikely that you saw this globe or something like it, you know, at least.
[21:24] This was a concept that was clearly out there. And basically what this globe does is it takes Ptolemy's world and wraps it around. a globe. It happens though that because Ptolemy actually didn't accept Eratosthenes measurement, apparently, for the size of the globe. I don't remember what the reasons were, but he posited a somewhat smaller sphere for the earth. and he actually ended up exaggerating the longitudinal length of the oikumene. So when you wrap Ptolemies a little too large, around a little too small globe, You get a what we would call Pacific Ocean view that looks like this. This is a projection of the Boeheim globe uh... looking with Europe over here, And here's China.
[22:17] And these islands off of China, maybe that's could be the Philippines or some idea of that. Here's Sipangu, which is Japan. This is all information that came from Marco Polo. But what you can see is, I love this example because it shows you exactly what Columbus thought he was doing when he sailed. from Spain, His idea was to sail west until-- and these are the islands, the Canaries and the other islands in the Atlantic. was to sail past all those islands until he hit Other islands, off the coast of China.
[22:53] And indeed, he thought when he hit Hispaniola and those other places that those were some of these islands. I believe the story is that Columbus actually went to his grave thinking that he had, in fact, discovered these-- these East Indies. Thank you. So, um... Thank you. I want to show you in a little more detail how Ptolemy went about mapping, making one of his detailed maps. Ptolemy's first map of Europe, is the British Isles. And interestingly, the His arrangement of these regional maps, starting with the British Isles and the second map being the Iberian Peninsula.
[23:36] tradition became very firmly entrenched so that when the first modern atlas came out in 1570, Abraham Ortelius, He had a world map. And then his first... regional map, was the British Isles. and the second regional map, was Iberia. And in fact, most atlases made until the 20th century followed that pattern. It was Great Britain. It was Spain, then it was France, and then so on. The order kind of...
[24:12] falls apart after that, but that was how influential Ptolemy was. So this is a satellite view of-- of of Great Britain. And this is Ptolemy's map of Great Britain. And-- This is the kind of information that Ptolemy recorded. Lots of place names. OF TOWNS. A number of locations of rivers. We're not to take this interior detail at all seriously, but supposedly the river mouth would have been It's something that he plotted.
[24:50] Um. There are some names of peoples here. sort of general names. This is where the I can't read these names on here, but this is where this tribe lives, and this is where these people live. and a few physical features like some mountains, and even a big forest here in Scotland. Thank you. So how did he do that? Well, he started with a projection of that part of the world. And he put down his best guess as to where London was located, latitude and longitude. The Roman legions, of course, were all over Great Britain, and they undoubtedly had regular-- traveled between all these places and he had itineraries telling him how far certain things were.
[25:33] especially towns. Tamara actually I think is a river in Cornwall. MR. Corinium is-- I have to look at my crib sheet. Corinium is-- Sirincester? Um... Maridunum is a carmarthen in Wales. This is the promontory of Kent, which was apparently fairly well established because it was where the the Roman troops, the Roman ships, that would be the first landfall there in Britain. And so there were a number of places that he had Ratier, is Lester.
[26:09] Diva is Cheshire. Lindum is Lincoln. And Eboracum is York. And he adds the note in his geography that this is where the Sixth Legion. won a victory. So-- There were a number of places that he was able to establish fairly accurately. in relation to one another, where they were. And from these from some of these fixed locations. Some people even think that the Romans had a kind of a triangulation, had a kind of a a standard triangle that they worked off of here in surveying in making maps of England. And Ptolemy may actually have had a map of England that he got from from someone in the army. It's not at all unthinkable.
[26:57] that there was a sketch map and they said, "Yeah, well this is what this Southwest Promontory looks like. So anyway, using the best information he had, he came up with this outline. on his big map. Let's picture it on the floor here. And he also put in the river mouths. They said, well, this river is up here. so many miles north of this spot. point here and you know And so he plotted all these places on his map. Now, if he had just done that, and made these wonderful maps.
[27:29] That would have been enough. had they survived. But the problem with maps then and still today is that they're extremely Fragile. and extremely subject to wear and tear. And any of you who have a a car with a glove compartment, you can testify that, in fact, most maps get used to death, if they're used at all. So had Ptolemy made a big world map on parchment or on papyrus or something. And had he made a set of 26 regional maps, Maybe they would have survived. Maybe copies would have been made.
[28:08] and they would have survived the millennia. But-- and he undoubtedly did make, such maps. I mean he at least made one big map, we know that. But the reason Ptolemy's geography survived is because he digitized it. He took all of these, he started with these latitudes and longitudes of towns, and then he started plotting the a reading off of his book, his base map on the floor, let's say, he started reading off other coordinates. So if you'll follow these dots that I've placed around here, he would say, okay, well at this speed point of this bulge.
[28:47] It's 53 degrees, 30 minutes. Uh... of of latitude and about 22 degrees, 10 minutes of longitude. And he'd write that down. and He'd do this for the river mouths, for the promontories. for all these different features around the island. Um. dozens, perhaps as many as a couple hundred points for the British Isles. And he recorded those in Thank you.
[29:21] Tabular format. like this. This happens to be a Latin manuscript of Ptolemy's Geography. He would have written in Greek, and there are some extant Greek manuscripts. But basically, Ptolemy's geography as we know it, as it came down through the ages consisted of no maps, But-- a a textbook of how to do the projections, and a general description of how to map, and a list of 8,000 coordinates like this.
[29:53] Here's a place. Here's the latitude. and fraction and longitude and fraction. And actually, the way he indicated. uh degrees I mean minutes and, well he didn't really get into seconds, but the way he indicated minutes was, he would say if it was, we would call it 50 degrees 30 minutes, he would say, 50 degrees and a half. And if it was 50 degrees 45 minutes, he would say 50 degrees and a half and a quarter. uh They didn't have the concept of unified fraction.
[30:27] So... that the geography as it came down through the ages consisted of just Uh... data, just numeric, alphanumeric data. digital data, if you will. And it wasn't, there seems, there is some evidence that the Arabs had access to Ptolemy's geography, but it was pretty much lost to Western culture until the late 1200s, I'm sorry, the late 1300s, when a copy was discovered in, Constantinople.
[31:03] a Greek manuscript and a geographer in Constantinople said, here's a direction for how to make a world map. And he proceeded to plot out these eight having drawn We don't know if he did one big map or made regional maps, but he followed Ptolemy's instructions. He plotted out all these 8,000 places and produced This atlas. Well, that was a revolutionary thing. And that atlas very quickly got translated into Latin. and many, many copies were made of it.
[31:35] And it became... it became the first standard atlas of the world. This in about 1400. And it-- In many ways, it stayed the standard atlas of the world for at least 100 years. Ptolemy's geography was one of the first books to be published. The first edition with maps was 1477. a very early illustrated book. And there were multiple editions all through the 16th century. It wasn't until about 1570 when Ortelius came out with his Theatrum Orvis Terrarum, thought of as the first modern atlas. But until that time, at least until the 1520s, Ptolemy's maps from 125 AD, we're pretty much it.
[32:23] for understanding the geography of the world. Thank you. Of course, when the new discoveries happened, they had to think on their feet and there are several maps There's one map in particular I'm thinking of in the exhibit where you see what's basically a Ptolemaic world with some American stuff tacked on it. But to get back to-- to his map of Britain. Many of you may have wondered why Scotland is bent over like that. Um... I haven't read actually anywhere anyone saying this explicitly, but I'm pretty convinced this is what happened. If you turn that bit of Scotland up on end like this, 90 degrees.
[33:06] you'll see that It actually-- is not a bad rendition of Scotland. I mean, you get the basic... peninsula up here, this Moray Firth. You get this peninsula here. these little fjord-like things over on the west side. It's-- It's not bad for... 125 AD, drawn by a guy a couple thousand miles away who never left Alexandria. working from Verbal, uh... Descriptions, probably.
[33:40] But the reason he had to bend it was because of the island of Tuli. You remember that zonal diagram? It showed the sort of northernmost habitable place as the latitude of Thule. Well, truly, this is from a map of 1539 showing this. imaginary island. Some people think it actually might have been Iceland, or possibly some other faraway island in the North Atlantic. Basically, Ptolemy's information went back to Pythias, who said that Thule was six days sail north of Britain and is near the frozen sea. The idea was that when you got that far north, much beyond beyond 60 degrees north that the entire sea was frozen, then it would obviously be uninhabitable.
[34:26] So-- Ptolemy was in a pickle because he had He had a lot of information from the Roman legions about Britain. and about Scotland, and he clearly knew that when you got up here, there was still about this much more to go. But he had the problem that here was his Thule. He had-- He had plotted Thule as this location. And according to Pythias, it had to be It had to be six days sail north of Britain. and if he put it up this way it just didn't fit. So he did what a lot of scientists do today. They try to uh...
[35:05] adjust that you know understand the data and the way that's most that seems to make the most sense. And for him, he tries to preserve the length of Britain while at the same time recognizing that Thule is pretty much the northern limit of of habitation. So he simply bent it. Thank you. That's my view and I challenge anyone. If anyone has another explanation, they're welcome to give it. So anyway, this is Ptolemy's world. The same world that's wrapped around that Boeheim globe, although the Boeheim globe also includes information from Marco Polo, which extends beyond uh... trying out here gives us Japan.
[35:44] Thank you. Moving now to the Mediterranean. Um... We're going to talk about another... great Ptolemies, the discovery of Ptolemies geography in 1400 or thereabouts, is just an epochal thing in the history of cartography. The whole idea of mapping on a grid, latitude and longitude, that all comes from from Ptolemy. But there was another tradition that had started a couple hundred years earlier.
[36:20] that in the Mediterranean that is even-- that is sort of a parallel tradition. And that's the tradition of the portal on chart. This is the first the earliest known copy of a Portland chart. And some of the characteristics of Portland charts, well, they're almost... all was drawn on an animal skin, on vellum. This is the neck of the animal. Can you see the outline here? This is that we're looking at the Mediterranean. Down here is the uh...
[36:52] uh... the uh... Straight of Gibraltar. And here's North Africa, here's the Italian, the boot of Italy, Here's the eastern... the Eastern Shore, the Mediterranean, and actually the Black Sea was almost always included in portal and charts. And the Black Sea has been somewhat eroded here. This map, one of the most important maps in the history of cartography, was found in a Paris junk shop in 1840-something.
[37:26] and now lives in the bibliothek Nassau. Thank you. Here's a detail of-- of the cartesan, as it's called, which shows you in greater detail some of the characteristics. invariably have a circle, a circular, grid If you step back, you can actually see um You can see a couple of great circles here inscribed that have wind roses in the middle and radiating radiating wind lines or rum lines as they're called, R-H-U-M-V.
[38:04] The place names on portal and charts are always written inland. They tried to leave the water spaces as open as possible. Um... Typically, the rum lines were different colors. Some were green, some were red, some charts have black ones. Um... Another characteristic-- oh, they have-- they show-- They showed tiny little rocks. There's another example that I can show you some more. symbols. But-- and the other thing is that there is no up on a portal and chart. There's just no, you can't say, "Oh, this is meant to be up." The lettering, if you'll see, these are meant to be read from that way, And then down here...
[38:45] Thank you. I can't quite make that out. They're still read that way, but over here they're read this way. If you go around an island, you'd have to turn the chart around like that. It didn't really have-- It didn't really have a natural pulpy. Thank you. This is another portal and chart. This is from the Newberry's collection. This is our earliest portal and we have a couple dozen portal and charts and atlases. This is 1456 done by a Rosselli from Majorca, he signs it up here in the neck.
[39:16] And again, it's the outline of-- the Mediterranean with the Black Sea. Some of them also went up-- most of them went up the west coast of Europe, included the British Isles usually. Um... Very often they would put these maps, these flags around the around the border. Um, This, many of the portal and charts that have survived, obviously the Cart-Pizan is a pretty pretty tattered and torn thing and was not probably terribly attractive when it was made.
[39:51] Some of the portal and charts that have survived are very pristine, lovely things that probably were made for for you know, rich clients or for parlor use or library use. But there are some that give evidence of having been to sea, and I think this is one of them. Over here on this side. There are these holes. That's where it was nailed onto a wooden roller. And over here on the neck is a little hole. There would have been a leather thong through there. So you'd roll it up and tie it with that thong.
[40:22] stick it in a cubbyhole on board ship. And it's definitely seen some wear here from being rolled and unrolled. Even some of these flags have obvious signs of ink the-- the pigment having having gotten wet. So I don't know. I like to think this one may actually have gone to sea. Okay. Anyway, How were they used? This is another portal and atlas from the Newberry. It's actually a, this is an atlas, this is an opening of two pages I've had to join the sheets here, the digital copies.
[40:56] But to show you how a mariner might use a Portland chart like this, If you wanted to go from This Melilla, I think it is, on the north coast of Africa. to this point over here, Cabo da Gata. CAP. Yeah, a cape of-- cat cape. He-- In other words, he wanted to sail a course more or less like that. He could draw his course on there or lay a parallel ruler between those places.
[41:27] There's one side of the parallel ruler, and then he'd swing out the other arm of the ruler until he till he lined it up with a wind rose. And in this case, As you can see, That's the north line. North by east. north-northeast, it's actually in between north by east and north-northeast. The mariner starting out from here would try to get his compass to read a little bit east of North by East. hopefully would strike his point.
[41:59] but hopefully not Not literally, because as a matter of fact, there is a-- There's an indication here that there's a big rock there. And I think if you're familiar with modern nautical charts, Something very like that is used today to indicate a hazard to navigation like a rock, little dots like this to indicate shoals. Some of these portal and charts even have a little ship skeleton to indicate a wreck, a sunken ship.
[42:35] So the main tool was a compass. such as this one. We don't really have any really ancient compasses. The compass was Uh... They used to say that it was invented in China and carried to the Mediterranean. Now people think that It may have been independently invented. But anyway, there's textual evidence that people talking about sailing with compasses sailing by the magnetized needle in the early 1200s. And so that's about the time the cart Pisan comes out, sometime in the late 1200s.
[43:10] The earliest compasses may have been just a needle actually floating on water, held up by surface tension. Sometimes they would push the needle through a straw, And that would keep it afloat, but I'm sure by a very early age they had a They had devised this method of a card with the needle attached underneath. And they would have needed an hourglass or, in some cases, a minute glass or a half-minute glass. And navigators from at least the late Middle Ages up until well into the uh...
[43:46] 18th century, we're using a log and line to gather information about their speed. Basically, you needed-- you needed-- a spool with a lot of line on it. You needed this log here or chip. and you needed a a glass that-- was good for half a minute. And the way it worked was something like this. I think you must have needed at least three men. One guy is holding the log real.
[44:18] Another guy is holding the 30 second glass. And another guy is holding the actual chip here, which is weighted at the bottom. He throws this thing over the back of the ship. And it hits the water and starts bobbing along. And, of course, the water catches it here, so it's... sort of riding up in the water. And he waits until... Uh-- about the length of the ship. There's a red rag tide there, and that indicates that the thing is now far enough behind the ship so that it's free of the wake of the ship and supposedly it's it's kind of digging into more untroubled waters.
[44:57] And when that red line goes over, the goes over the rail, he says, "Turn." And the guy with the 30-second glass turns the glass, And then they start counting how many knots go over. And the knots are placed, well... Apparently there were a couple different lengths of knot, but the knots are placed at regular intervals along there. You count how many knots go over and when the glass runs out, the guy says stop. And then the guy holding the reel holds it. They count how many knots have gone over.
[45:30] and they record that information. on this device, which is a Travers board. and This is a wonderfully simple device that It didn't require any great learning. An illiterate seaman could use it as long as he was familiar with the points of the compass and could read the numbers, I guess, from 1 to 12. The idea is this: here are all the points of the compass that you could possibly steer each of these concentric rows of circles is a half hour.
[46:05] So this would be the first half hour of a watch. the second half hour, the third half hour, and so on. up to the four hour watch. a very standard way of breaking up the day at sea. from early on. And attached to the middle, there is a cord. and you have a bunch of little pegs. to go along with it, which you can push next to the cord into a hole. So what this tells us is that in the first half hour of the watch, They were sailing north by West.
[46:40] on that course. And in the second half hour of the watch, they were still sailing north by west. But when the Third half hour came along, they had shifted their course to-- this point of the compass. And in the fourth half hour-- After two hours of sailing, They had shifted it to this point. So you'd keep doing this, and for the four hours of a watch, you'd have a perfect record of the course you had steered. Now, how fast were you going? Well, every hour they would do this business with the log.
[47:14] the chip log. And they would plot those down here. Each of these lines is one hour of the watch. First hour. second hour. Third hour. the fourth dollar. What this tells us is that in the first hour of the watch, They were going six knots. So they put the little peg there. In the second hour of the watch, I'm doing all this pointing, and I made this elaborate slide to show you this. I forgot about it. Um... So there's the first hour, 6 knots. In the second hour, 8 knots, but a little more than 8 knots.
[47:54] Eight and a half knots. they could record down to the quarter of a knot. So that's a fairly accurate example estimate of your speed. So at the end of a four hour watch, the seaman could hand this board over to the captain and or whoever was-- keeping records. and they would have a complete record of distance and direction and speed FOR-- for that watch, which they could write down into a log. Well, um... How did Portland-- I see-- Jeff looking at his watch. Yeah, okay, that clock is right. I'm doing all right.
[48:31] How did-- How did this information get recorded? Ultimately, a lot of A lot of this, of Siemens information about distances from ports and things like that, got recorded in itinerary form like this. It's strictly-- well, I will say, I will call it, again, a digital record. I mean, it certainly uses numbers. Here's a Roman-- there are Roman numerals in here, and alphanumeric characters to record certain information. And this is the kind of information they record. These are called Portolani.
[49:07] books of sailing directions between ports. And this is the most famous Portolani painting. is the Compasso de Navigare from the, again, the late 1200s. And here's just one of the indications that go from Fennaro, this port, to Felia. It's 30 miles to the northwest. And then there's sometimes notes about about the place, but it's just one thing like that after another going around the whole course of the Mediterranean and the Black Sea.
[49:44] That's what's in the Compasso del Navigare. Now, people have long-- imagined that there had to be some connection between these these portalani, these books of directions like that, and the finished portal and charts. But it wasn't until-- A couple decades ago, there had a retired physician. Jonathan Landman, actually took the trouble to convert all of the measurements, all of the information in the Compasso da Navigare into into distances, standard distances and directions. He took, when he read Northwest, he turned that into so many degrees. When he read North by Northwest, he converted that into so many degrees. And then he plotted down the distances and those bearings and started to see what would happen.
[50:38] And in fact, he discovered that-- the Compasso del Navigare, If you plot down all those distances and directions, It does, in fact... I didn't mean to do that. What do I do? Just do this. It does in fact generate a map of the Mediterranean. Now, of course, it didn't... come out exactly like this. Any of you know anything about surveying know that there's something called error of closure whenever you survey around an area.
[51:17] it's not going to end up perfectly like that. some of this may be way down here or something. But as long as you're working with a closed area And this is virtually closed here at the Strait of Gibraltar. you know how to adjust it. So you just kind of adjust a little bit on every on every angle to make it fit like this. Well, how close was it? Well... Pretty close. There's the modern outline of the Mediterranean. So, we're pretty sure this is how the basic portal and chart was generated from these from these tables, really, or verbal lists of distances and directions.
[51:58] And of course it didn't happen all at once like that. It wasn't that somebody There was suddenly this Compasso della Navagari and somebody took that and plotted it and voila, Portland chart. I mean, it must have been a long procedure involving many, many errors and many mistakes many partial maps, I suppose, of different areas. But it's pretty clear, I think, that that is the -- That is the-- the source arm And now I'm going to say a little bit about a more continental approach.
[52:33] the The Mediterranean, we discovered, is pretty much mapped through very accurate, very small-scale Uh-- measurements of distance and direction around the perimeter. Um-- Much the same thing using many of the same instruments is happening on a larger scale when we come to a continent. One early map of this part of Africa. Now we're going to look at the-- at the young some of the Portuguese efforts to map the West Coast of Africa. Now, one other instrument that would have been involved besides the quadrant that we saw, Ptolemy was holding a quadrant, There was an instrument called the cross staff, which works the same way. You cite an object and you align this bar of this thing with the horizon.
[53:25] and this top of the bar with whatever you're citing, North Star or Sun, and you read an angle off of this sliding bar. Um. There's a model in the exhibit here. There are lots of wonderful instruments in this exhibit that are Some of which I've never seen before, very neat. addition to the exhibit. And in there is a backstaff, which is the same principle as this cross-staff, but instead of having to look directly at the sun. you turn your back to the sun, and this has a little mirror on it here, or a little vein, and you can read the shadow.
[54:01] the shadow of the sun instead of directly. accomplishes the same thing. So using logs and lines and, um, instruments like the quadrant or the cross staff to measure latitude and Um... the Portuguese gradually began to map Africa. Now this is a portion of a 1489 map, and I've trimmed everything else away. except what Ptolemy knew. This is pretty much the Africa that Ptolemy knew.
[54:32] It consisted of the northwest the north coast here, the North Shore of the Mediterranean. You know about the Atlas Mountains. He knew about the Nile, and they knew, or... thought they knew that the Nile had its source in the mountains of the moon, somewhere way down south in Africa. They also-- knew or thought they knew about some big lakes here, which I have no doubt were uh Lake Victoria and Lake Nyazaland, you know, or whatever.
[55:03] like our-- just, you know, The word was there were big lakes down there towards the end of the Nile. So that was Ptolemy's Africa. Well-- by the time the Portuguese really started to make a a dedicated effort to try to see if they could get around Africa if it was in fact Um. if it in fact did not enclose the the Indian Ocean. they started to sail down the West Coast and This is...
[55:37] This was a very long process. 1432, another A few years later, they get a little further to the River of Gold. Um... Now we're-- 10 years later. Here we are. A long time later, It took the Portuguese-- something like 50 years. to get to get the bulge of Africa really nailed down.
[56:11] But, and so they would have done this in exactly the same way by getting-- by getting latitude readings on these various river mouths and things like that and then by keeping track of their distances and directions. And finally, the big push to see if they couldn't get around the continent, and in 1485, no 1480 seven, eight, Bartolomeo Diaz actually rounds the cape of good faith.
[56:44] hope and gets as far as the Great Fish River, where he can see the coastline trending north. So this is the Africa that-- that is known after Diaz's expedition in 1488, and in fact this map is a world map. made by a German called Henricus Martellus in 1489. This is a manuscript at the British Library. There's another copy of the Martellus map, which with very much the same geography at Yale.
[57:16] And of course, you can see this is still Ptolemy's truncated South Asia and his very huge Ceylon, Caprobana. And the -- but here it does have some indication that there is from Marco Polo that there are these islands off the coast of China. So that is... That is how continents are mapped in a very basic way, and that is how North America ultimately was mapped too. Now, I want to conclude with a-- a case study of how-- how the interior of continents might have been mapped.
[57:53] or was in this case how it was mapped. These are the Great Lakes. OF COURSE. And I think you can see that it would be-- It would be a much different proposition to try to map the Great Lakes by coming in here and making a circuit of the lake and then measuring this distance down here and they're making a circuit of this lake and circuit of this lake and stringing those all together into a, you know, in the way we did with the Mediterranean, that would have been a tall order. And in fact, it didn't happen because the only people On these lakes for hundreds of years were voyagers in birch bark canoes.
[58:34] So-- You ended up with fairly crude maps of the Great Lakes. This is actually the first map to show all five of the Great Lakes. And you can see Lake Superior, they obviously were up here in in near this traits of Mackinaw and They knew there was a big lake opening up there, but they didn't know. how big or where it ended. This is presumably-- Lake Michigan, although Lac de Pouin, the name of Green Bay is usually Bay de Pouin, So that would be Lake Michigan, Huron, Ontario and Erie.
[59:09] But I'm showing you a series of maps attempt to represent the Great Lakes to show you that There's no such thing as as uh... nice linear progressions in cartography. We like to think that in general, you know, every map is an improvement on the last map and, you know, and I suppose in some cases that is the case. But if you look at a lot of early maps, you'll see a lot of a lot of stumbling, a lot of just plain I don't know, making things up.
[59:44] Cartographers have always borrowed wildly from other cartographers. I mean, until Until very recently, when we can actually go to something like Google Earth or Google NASA and get or the sub-- digital image laboratory and get up TODAY. photographs of the Earth's surface until very recently, When a cartographer was asked to make a map of such and such area, the first thing he did was find another map of that area. and use it as a base map and maybe adapt it or change the scale or something like that.
[1:00:14] Most maps are actually made from other maps. And-- At this time, two people were copying each other. So as we go through these various images, of the Great Lakes, you'll see some some things that look the same, you'll say, "Oh, that looks like he copied that from so-and-so." One of the things that I'm always interested in is when it comes to the Great Lakes, If you can define the shape of Michigan, both its southern peninsula and its northern peninsula. You have almost completed a map of the Great Lakes.
[1:00:46] And if you'll watch Michigan through this series of slides, I think you'll see that It was a very hard little peninsula to map. Surprisingly, this is a nice example of how uh... progression is not linear in cartography. This happens to be a very early-- in fact, the first map of like superiors. 1671. We know it was done by the Jesuits. It's published in the Jesuit relations. We don't really know who did it. Father Alouez was one. Father Marquette may actually have been involved. He was up here at at the mission on the Apostle Islands.
[1:01:22] But it's actually a very accurate map of Lake Superior. It has Isle Royale here. It has just a couple of little minor islands that are actually there. And the reason they were able to do this is we know that the Jesuits actually made a pretty much complete circuit. of the lake in canoes. Yeah. Counting paddle strokes perhaps, I don't know, but estimating the distance in some way. and taking readings of latitude.
[1:01:55] with an astrolabe or with a quadrant. Um... Here again, Michigan is a little distorted. Look at Lake Michigan. On many of these early maps, actually there are some where it's, It's swinging way less weight. Some where it's almost straight up and down, and some where it's way over at this angle. Michigan is like a pendulum. Um... Franck Hollande, very influential French mapmaker. He seems to have relied, I think, a little bit on the Jesuit map. He knew about it anyway.
[1:02:28] um... cornelli Italian cartographer, 1680s. MR. This looks like it's copied from the Jesuit map, except for some reason he thought he had to make it much wider. Bye. Thank you. Um. Some fairly outlandish figures here. where this comes from. This is the beginning of the of adding islands to Lake Superior. In the late 17th century, there were a couple of French manuscript maps made that just suddenly put in imaginary islands and named them after influential characters in France. And those islands got picked up on later maps. It's always the bad stuff that gets copied.
[1:03:13] First. So-- Um... These depictions, I don't know where they come from. Hennepin was generally not considered very reliable traveler or cartographer. D'Elia was one of the best map makers. And actually, it's not a bad representation of the Great Lakes. He's clearly using the Jesuit map here. for Lake Superior. And Lake Michigan is actually fairly reasonably oriented. uh... herman mall one of the more imaginative cartographers.
[1:03:51] Captain Cyprian Southak, the first First map of North America published in America. published in Boston in 1717, but Where he got his Great Lakes from, I do not know. Very strange. I don't think there was a model for that. Um. Popple, a part of Henry Popple's map, the southern sheets showing the Gulf of Mexico is in the exhibit. One of the-- one of the best maps of North America. in the 18th century.
[1:04:22] I have fairly reasonable... Michigan and Lake Michigan, but Notice Lake Superior. Here he's got Isle Royale and then here's Isle Filippo Pontchartrain, and I can't quite read it, but there were three or four or five islands just thrown in there to flatter the French officials. In fact, each one is named after another official. It's nice to have an island named after you. Thank you. Here again, Lake Michigan, way off to the southwest.
[1:04:55] Michigan Peninsula, just a little point. This is the Mitchell map, the second, maybe the most important 18th century map of North America. most important map in American history. largely because this is the map that in 1783 was laying in front of the the commissioners in Paris who drew the Treaty of Peace, and they drew a red line on this map showing the border. dividing the United States from-- British colonies.
[1:05:27] Mitchell's map is interesting in that this is the This is actually the Newberry's copy. badly reproduced, but our copy is colored so that you can see that the uh... the uh... colonies were, at least the southern colonies were shown with their western borders extending to the Pacific, according to the colonial charters. There's a wonderful copy of the Mitchell map upstairs in the exhibit too. It isn't colored quite this dramatically. If you see, the Charter of North Carolina was supposed to extend to the Pacific. Now if you're wondering where where Western Tennessee would have been had that actually happened. This is how it would sort out. Monterey would be in West Tennessee and San Luis Obispo, nice wine country in there.
[1:06:22] Could have been great. um So a couple more maps. Ah... attempting to show the Great Lakes. I'm going to concentrate on a couple of maps by this English cartographer named John Kerry. who publishes a series of maps. of regions of the United States like this. beginning in 18.5. and I guess if you look at the great, well they're recognizable and he's gotten rid of the fake-- no, he hasn't gotten rid of the fake islands. They're still there.
[1:06:54] There's Royale, but there's Philippot. In fact, this actually... Um... went back to the Mitchell map. The Mitchell map was used as I said to draw the Treaty of Peace. Can I get back there? How far away was it? Um. It's when they drew the line for the border, they drew it up here and they said, okay, They drew it across this island and to Isle Royale. And they went south of Isle Royale. And then they went up a river here. And in the treaty it said, Uh...
[1:07:26] It said north of the isles Philippot and Pontchartrain. and Isle Royale or something. And so they cited in the actual treaty document two islands that just didn't exist. And so for the next uh 70 years. They were looking and the British were arguing that, "Oh, this is what Isle Pontchartrain was." And the Americans said, "No, no, no, it was this island." Finally, it took a long-- it wasn't until the 1840s when they finally ruled that, in fact, those islands didn't exist.
[1:08:02] But here they are, 1805, it still shows the border going across the non-existent. Island. So anyway, this is Cary's 1805 map. And that would have served fine, except when in 1805, Ohio became a state. And so in later editions, he had to add Ohio. Here, the general geography is pretty good. There's Chicago. The portage. St. Joseph, Michigan. Detroit. Thank you. Thank you.
[1:08:34] But when he got to 1825, By that time, there were already-- Ohio had become a state. Indiana had become a state. Illinois had become a state. And He had to fit them in somehow. He didn't change the basic geography. He didn't have any better information. But-- you can see it gave him some problems because Here, for instance, is the bottom of Lake Michigan. Um, Well, Illinois, first of all, is landlocked. It has no lake. This is Illinois. Um...
[1:09:05] Fort Dearborn in Chicago is in Wisconsin, California. what's not Wisconsin. Um, Indiana is here. It just, it was very hard to fit in. And the reason was he had He actually had a very good observation for the Oh, yeah. This is... indicating his basic difficulties. How do you fit three states? like that. into that space between the Mississippi and the western border of Pennsylvania.
[1:09:36] Thank you. Thank you. Now he knew for a certainty about, he actually, his longitude for the west end of Lake Superior is pretty good. It's actually right about 92 degrees west, which is what he shows. His longitude for the east end of Lake Ontario is also Right on. also the western border of Pennsylvania. The reason that's right on is because of the Mason-Dixon line. which of course was surveyed on the ground with guys lugging chains and blazing through trees and making paths.
[1:10:07] and marking on the ground the how many hundred miles to the western border of Pennsylvania. So he had those three people those things pretty well fixed. But he was very vague about the Mississippi River. There weren't any accurate observations out there. and this this lake system in here was just uh, Very, very-- little known. That's the western border of Ohio. This is the western border of Indiana, and this is the westernmost bulge of the of Illinois on the Mississippi.
[1:10:45] So how did this... little problem gets solved. Well, unlike our other examples, it wasn't solved from the water. It was solved on land, and it was solved by people dragging chains like this. across the country and orienting them with compasses like this. The general-- in the Northwest Territory, which was this area here. was was decided to divide it completely, into parcels. Of course, you folks down here, you have the meets and bounds system, where you just sort of said from this tree to that rock to the river and then back.
[1:11:24] but they decided they wanted something a little more orderly for the Northwest Territories, and so they devised this... system of public lands consisting of six-mile square townships and divided into 36. square sections. And they first did this in the very early eastern part of Ohio in what was called the Seven Ranges. That was done in 1787. They were just kind of experimenting, really. They didn't quite know how they were going to expand this grid across the Northwest Territories, And Ohio is really very much a...
[1:12:00] experiment. If you look at the the land surveys of Ohio. There are slightly different orientations and they don't match up perfectly. They didn't really have a standard meridian. But by the time they got into Indiana, they started establishing a standard meridian. So you'd have one north-south line there, where you would number all the ranges and all the townships. And Indiana and Illinois were both settled from the south. So, They became states 1816, 1818. But at the time they attained statehood, All the whole northern part of the states were or on Well, they weren't unpopulated, but they were lightly populated.
[1:12:46] did not have the benefit of the township and range surveys. In Illinois-- uh... by eighteen 30 about, they had actually surveyed a little extension up here because They wanted to build a canal from Chicago down to the Illinois River, the Illinois-Michigan Canal. And so they divided that. and the federal government started getting rid of that land. Meanwhile, on either side of it, it was still Indian territory. country. So as these surveys progressed, they bumped up into the water.
[1:13:21] And it was only really when This survey got up here in about 1830. that they were able to say, with considerable certainty and accuracy This is where... the western shore of Lake Michigan hits at that point. And as the survey Continues. Wisconsin becomes a state in '48. gradually the entire lower peninsula of Michigan, and of course the entire Lake Michigan, and the location of the Mississippi River, They're all determined.
[1:13:55] accurately by measurements on the ground. Briefly, this is what happened. Starting with the Mason-Dixon line, which after all starts in tidewater, and was measured uh... by chain, and compass and then extending the general land office surveys west and north. and east and west. They finally... were able to determine the outline of the Great Lakes. And that's how this little bit of geography got mapped, strictly from the land.
[1:14:35] So... That's all I have to say, but I'm happy to answer questions if you have any. I'll try to answer them, that is. Yes? Thank you.
在 Vidleaf 工作台開啟
檢索字幕、選取句子、複製附時間戳的引用,或按需翻譯。
來源署名
「Lecture: "How Did They Make Those Maps"」由 McClung Museum of Natural History and Culture 發布,採用 CC BY 3.0 授權。來源影片:https://www.youtube.com/watch?v=wbwmXKwkgaw。此頁呈現影片的文字字幕,由 Vidleaf 加入段落與時間戳。創作者與 Vidleaf 無隸屬或背書關係。頁面若提供 AI 標點、名稱修正或摘要,會分開標示,原始字幕仍可查看。
若你是創作者或權利人,可申請更正或下架: copyright@vidleaf.app (參閱 關於這些頁面)。
最後更新