I have the pleasure of conversing with V. Garth Norman frequently. He is one of the most astute students of the Book of Mormon in our generation. He, along with many others, believes the narrow neck of land referenced in
Alma 63:5,
Ether 10:20 and possibly
Alma 22:32 is the entire Isthmus of Tehuantepec in southern Mexico. I do not believe the text supports that correlation. This article will place Tehuantepec in context among the isthmuses of the world to lay the foundation for relevant Book of Mormon exegesis.
Geographers identify the Isthmus of Tehuantepec as that land in Mexico between the 94th and 96th meridians of west longitude. Its surface area (including water) is 57,629 square kilometers. That is larger than any of the 9 smallest states in the U.S. and nearly the size of West Virginia.
- 14.40 times larger than Rhode Island, 4,002 square kilometers
- 8.94 times larger than Delaware, 6,447 square kilometers
- 4.01 times larger than Connecticut, 14,357 square kilometers
- 2.55 times larger than New Jersey, 22,588 square kilometers
- 2.38 times larger than New Hampshire, 24,216 square kilometers
- 2.31 times larger than Vermont, 24,901 square kilometers
- 2.11 times larger than Massachusetts, 27,336 square kilometers
- 2.04 times larger than Hawaii, 28,311 square kilometers
- 1.79 times larger than Maryland, 32,133 square kilometers
- 91.83% as large as West Virginia, 62,755 square kilometers
The Isthmus of Tehuantepec is larger than dozens of countries on earth including Croatia (56,594 square kilometers), Denmark (43,094 square kilometers), Taiwan (36,193 squarer kilometers) or Israel (20,770 square kilometers). Placing a north-south transect at the narrowest point, the width of the isthmus between the Gulf of Mexico (Gulf of Campeche) and the Pacific Ocean (Gulf of Tehuantepec) is 216 kilometers. Placing an east-west transect between the 94th and 96th meridians of west longitude, the length of the isthmus is 211 kilometers. The Isthmus of Tehuantepec, as defined by geographers, is shown as a white polygon on the map below. As with all images on this blog, click to enlarge.
|
Isthmus of Tehuantepec in white, surface area 57,629 square kilometers |
Parts of 4 Mexican states are included in the isthmus: Oaxaca, Veracruz, Tabasco and Chiapas. The name comes from the Oaxacan town of Santo Domingo Tehuantepec. The name "Tehuantepec" derives from the Nahuatl "tecuani-tepec" or "jaguar hill". Shortly before the Spanish conquest, the Aztecs conquered Santo Domingo Tehuantepec, but only after a prolonged siege battle. The locals fought ferociously from fortified positions on a prominent hill (summit 120 meters) east of the Tehuantepec River. This Google Earth view shows the hill just above the yellow line representing the Tehuantepec River, on the right hand side of the image with the modern town built up around it.
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Modern town of Santo Domingo Tehuantepec showing jaguar hill |
Because the natives fought like jaguars on their hill, the Aztecs named the place tecuani-tepec.
4 major river systems drained the isthmus during Book of Mormon times: the Papaloapan, Coatzacoalcos, Tehuantepec and Mezcalapa-Grijalva (today the Tonala). On the map below, the Mezcalapa-Grijalva system (as it flowed in Book of Mormon times - see the article "
Wandering River" in this blog) is in blue, the Usumacinta is in red, other rivers are in yellow, the continental divide is in white, and the trans-isthmian railroad is shown in magenta. It requires 302 kilometers of track for the railway to connect Salina Cruz, Oaxaca with Coatzacoalcos, Veracruz. The railroad crosses the continental divide at Chivela Pass, altitude 224 meters.
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Isthmian rivers, continental divide and railroad |
Chivela Pass funnels prevailing winds, known as Tehuanos, from south to north. Occasionally, contrary winds blow through the pass in the opposite direction, from north to south, with such force that they have been known to sandblast paint from ships in the Gulf of Tehuantepec. The largest wind power project in Latin America is currently under development on the Oaxacan side of the isthmus. Elevations within the isthmus range from 2,500 meters to sea level. Five different climatic zones are present in this area. The following map shows the world standard Koppen climate classification system for Mexico.
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Koppen climate map of Mexico showing five zones within the isthmus |
In general, the southern side of the isthmus is much drier than the northern side. This is graphically shown in a
NASA true color satellite image taken in April at the height of the dry season.
|
NASA Blue Marble image of the isthmian region in April |
Satellite images of the earth's lights at night provide a good visual representation of relative population density. Notice that in the Tehuantepec region, both coasts are heavily populated while the interior Selva Zoque remains largely in its natural state.
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NASA image of the earth's lights at night |
This same pattern held true anciently. Plotting archaeological sites known to science from the
EAAMS database, we find settlement activity on both coasts with a large blank spot in the middle.
|
Known archaeological sites |
The point is that the Isthmus of Tehuantepec is a very large place with a great deal of physiographic and cultural diversity. How large is it? It is the widest isthmus on the planet (Panama is the longest). Geographers consider anything wider than Tehuantepec part of a continental land mass rather than an isthmus. Some geographers even consider Tehuantepec too wide to be classified as an isthmus. Here is a comprehensive, although not exhaustive, list of generally accepted isthmuses (aka isthmi) organized in ascending order by width at the narrowest point:
Isthmuses
of the World |
Isthmus |
Between |
and |
Width (km) |
Notes |
Bruny Island, Tasmania |
North Bruny |
South Bruny |
0.04 |
|
Olympia, Washington |
West Olympia |
East Olympia |
0.04 |
|
Nahant, Massachusetts |
Nahant |
Masachusetts |
0.06 |
|
Quetrihue, Argentina |
Quetrihue Peninsula |
Neuquen, Argentina |
0.09 |
|
Mavis Grind, Shetland Islands |
North Mavine Peninsula |
Shetland |
0.11 |
|
La Coupee, Sark, Channel Islands |
Little Sark |
Sark |
0.12 |
|
Eaglehawk Neck, Tasmania |
Tasman Peninsula |
Tasmania |
0.14 |
|
Portland Beach, U.K. |
Portland Bill |
Dorset, England |
0.16 |
|
Bardsey Island, U.K. |
North Bardsey |
South Bardsey |
0.19 |
|
Derbyhaven, U.K. |
Langness Peninsula |
Isle of Man |
0.20 |
|
Coronado, California |
Coronado Island |
California |
0.25 |
|
Saint Pierre and Miquelon, Newfoundland |
Island of Miquelon |
Langlade Island |
0.25 |
|
Sutton, Dublin, Ireland |
Howth |
Ireland |
0.37 |
|
Cape Clear Island, Ireland |
Gathabawn |
Cape Clear |
0.43 |
|
Kushimoto, Japan |
Cape Shiono-Misaki |
Honshu Island |
0.47 |
|
Catalina Island, California |
Western Catalina |
Eastern Catalina |
0.61 |
|
Munoz Gamero Peninsula, Chile |
Munoz Gamero |
Chile |
0.80 |
|
Madison, Wisconsin |
Lake Mendota |
Lake Monona |
0.93 |
|
Bolbs, Spain |
Gibraltar |
Spain |
1.08 |
|
Potidea, Greece |
Kassandra Peninsula |
Greece |
1.08 |
|
East Falkland Island |
Northern East Falkland |
Southern East Falkland |
1.24 |
|
Sechelt, British Columbia |
Sechelt Peninsula |
Canada |
1.25 |
|
Llondudno, Wales |
Great Orme |
Wales |
1.29 |
|
Rongotai, New Zealand |
Miramar Peninsula |
North Island, N.Z. |
1.31 |
|
Similk Beach, Washington |
Fidalgo Island |
Washington |
1.75 |
|
Tarbert, Scotland |
Kintyre Peninsula |
Scotland |
2.17 |
|
|
|
|
2.96 |
median |
Auckland, New Zealand |
Northern Peninsula |
North Island, N.Z. |
3.75 |
|
Seattle, Washington |
Puget Sound |
Lake Washington |
4.00 |
|
Medanos, Venezuela |
Medanos Peninsula |
Venezuela |
4.05 |
|
Summerside, Prince Edward Island |
Western P.E.I. |
Prince Edward Island |
4.12 |
|
Carlos Ameghino, Argentina |
Valdes Peninsula |
Chubut, Argentina |
5.07 |
|
Avalon, Newfoundland |
Avalon Peninsula |
Newfoundland |
5.75 |
|
Corinth, Greece |
Peloponnese Peninsula |
Greece |
5.80 |
etymological origin |
Perekop, Crimea |
Crimea |
Ukraine |
9.46 |
|
Westfjords, Iceland |
Westfjords Peninsula |
Iceland |
9.47 |
|
Rhins of Galloway, Scotland |
Galloway Peninsula |
Scotland |
9.60 |
|
Maui, Hawaii |
West Maui |
Maui |
11.00 |
|
Quezon, Philippines |
Bicol Peninsula |
Luzon |
12.00 |
|
Punta Arenas, Chile |
Brunswick Peninsula |
Chile |
15.00 |
|
Rivas, Nicaragua |
Lake Nicaragua |
Pacific Ocean |
18.00 |
|
|
|
|
20.20 |
mean |
Ofqui, Chile |
Taitao Peninsula |
Chile |
21.00 |
|
Chignecto, Nova Scotia |
Nova Scotia |
Canada |
24.00 |
|
Adam's Bridge (former isthmus), India |
India |
Sri Lanka |
29.00 |
|
Catanzaro, Italy |
Calabria Peninsula |
Italy |
30.00 |
|
Kra Isthmus, Thailand |
Malay Peninsula |
Asia |
43.00 |
|
Karelian Isthmus, Russia |
Gulf of Finland |
Lake Ladoga |
46.00 |
|
Forth-Clyde, Scotland |
Scottish Highlands |
Central Lowlands |
50.00 |
|
Panama |
Central America |
South America |
57.00 |
|
Suez, Egypt |
Sinai Peninsula |
Egypt |
122.00 |
|
Olonets, Russia |
Lake Onega |
Lake Ladoga |
125.00 |
|
Onega, Russia |
Lake Onega |
White Sea |
154.00 |
|
Tehuantepec, Mexico |
North America |
Central America |
216.00 |
|
|
|
|
20.20 |
mean |
|
|
|
2.96 |
median |
If you want to play around with the data, you can download the Excel spreadsheet
here by clicking on file, then download.
The word "isthmus" derives from the Greek "isthmos" meaning "neck". The use of the term in geography originated with the Isthmus of Corinth which is 5.80 kilometers wide at its narrowest point.
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Isthmus of Corinth (Korinthos) in Greece |
The Isthmus of Corinth joins the Peloponnese Peninsula to the Greek mainland. It is about 7.45 kilometers long and has a surface area of approximately 56 square kilometers. The modern Greek village of Isthmia is at the narrowest point of the isthmus.
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Isthmus of Corinth closeup |
The Isthmus of Paracas in Peru, 4.61 kilometers wide, is typical. The atypical Isthmus of Tehuantepec is 37 times wider (216 kilometers/5.80 kilometers) than the Isthmus of Corinth which defines the genre.