Everything about Continental Divide Atlantic Pacific totally explained
» This article is about the Atlantic/Pacific divide of North America, not the Eastern Continental Divide. There are two Triple Continental Divides in the United States, one in the east, and one in the west; the former along the spine of the Appalachian Mountains, the latter along a point in the Rocky Mountains. For continental divides in general, see Continental Divide. For the movie, see Continental Divide (film)
Continental Divide or
Great Divide is the name given to the
North American portion of the
mountainous
ridge which separates the
watersheds that drain into the
Pacific Ocean from, 1) those river systems which drain into the
Atlantic Ocean (including those which drain via the
Gulf of Mexico), and 2) along the northernmost reaches of the Divide, those river systems which drain into the
Arctic Ocean. A secondary, non-mountainous divide further separates other river systems that drain into the Arctic Ocean (including those which drain via
Hudson Bay,
James Bay, and
Ungava Bay) from those which drain into the Atlantic Ocean (including those which drain via the
Great Lakes and
Saint Lawrence Seaway).
Geography
The divide begins at
Cape Prince of Wales in
Alaska. It runs northeast-/eastward across the north of the state into the
Yukon Territory,
Canada, where it turns south and travels through
British Columbia (forming part of the B.C.-
Alberta boundary), in Canada; then through
Montana (forming part of the Montana-
Idaho boundary),
Wyoming,
Colorado, and
New Mexico, in the
United States; then along the crest of the
Sierra Madre Occidental through the
Mexican states of
Chihuahua,
Durango,
Zacatecas,
Aguascalientes,
Jalisco,
Guanajuato,
México and the
Distrito Federal,
Morelos,
Puebla,
Oaxaca, and
Chiapas; thence through southern
Guatemala, southwestern
Honduras, western
Nicaragua, and western/southwestern
Costa Rica, and southern
Panama.
The physical divide continues (though the name "Great Divide" does not) into
South America, where it follows the peaks of the
Andes Mountains, traversing western
Colombia, central
Ecuador, western and southwestern
Peru, and eastern
Chile (essentially conforming to the Chile-
Bolivia and Chile-
Argentina boundaries), southward to the southern end of
Patagonia and
Tierra del Fuego.
In North America,
Triple Divide Peak in
Glacier National Park, in Montana, is the point at which two of the principal continental divides in North America converge, the Great Divide and the
Northern Divide. From this point, waters flow to the Pacific, the Atlantic and the Arctic Oceans. Another triple divide or
triple point occurs in Canada on a prominent peak directly on the border between
Alberta and
British Columbia, called
Snow Dome because the
Columbia Icefield completely covers the summit. Water flows off this mountain into the Pacific, via the
Columbia River system; the Arctic via the
Athabasca River and
MacKenzie River systems; and
Hudson Bay via the
North Saskatchewan River system. Because Canadians consider Hudson Bay to be an extension of the Atlantic Ocean, they consider Snow Dome to be the hydrological apex of North America.
In fact, there are such triple divide points wherever two continental divides meet. North America can be considered to have five major drainage systems: into the Pacific, Atlantic and Arctic Oceans, plus Hudson Bay and the Gulf of Mexico. Within this system there are four continental divides and three triple points, the two mentioned previously and a third near
Hibbing, Minnesota where the
Northern Divide intersects the
Eastern Continental Divide. Since there's no true consensus on what a continental divide is, there's no real agreement on where the triple points are. However, the main Continental Divide described in this article is a far more distinctive geological feature than the others and its two main triple points are much more prominent.
The
Continental Divide Trail follows the divide through the U.S. from the
Mexican border to the
Canadian border. A less-developed Canadian extension called the
Great Divide Trail continues on through five
National Parks of Canada and six
provincial parks to end at Kakwa Lake in northeastern British Columbia.
Exceptions
Many
endorheic regions in North America complicate the simple view of east or west, "ocean-bound" water flow.
The
Great Basin of the Western US, The
Valley of Mexico and
Bolson de Mapimi in Mexico, the
Tularosa Basin in New Mexico and Texas, and the
Salton Trough are examples of internally draining areas. In these cases, water often drains to low basins, where
sedimentation and
evaporation form
salt lakes,
playas,
salt flats, and
alkali flats.
On the
Llano Estacado in Texas and New Mexico, many thousands of seasonal
playa lakes form during wet months, an average of one per square mile. This region is very flat, and water mostly evaporates before draining.
Zuni Salt Lake is one example of a larger, seasonal
maar which doesn't drain to an ocean. There are a number of seasonal lakes of this sort in North America. In areas of
karst topography (such as northern
Florida), isolated drainages can also occur.
The
Great Divide Basin in Wyoming has no natural outlet except as
groundwater, and hence it lies between the Atlantic and Pacific watersheds, being part of neither. Water from the
North Two Ocean Creek in Wyoming flows into both oceans.
Additionally, although
Panama's isthmus provides clear division between Atlantic and Pacific, the boundaries between the Atlantic and Arctic Oceans in
Baffin Bay are not well defined, rendering the easternmost portion of this divide arbitrary.
Images
Image:Continental Divide in Yellowstone-750px.JPG|The Continental Divide as it passes through Yellowstone National Park (7988ft / 2436m)
Image:lovelandPass_CMM.jpg|The Continental Divide as it passes through Colorado at the Loveland Pass
Image:Continental_Divide_in_Colorado_-_July_2005.jpg|The Continental Divide seen from Idaho Springs, Colorado in July 2005
Image:Monarchsign.JPG|Monarch Pass
Image:Continental Divide CO 2005-10-15.jpg|The Continental Divide viewed from northwest of Winter Park, Colorado.
Image:Nmcontdiv.JPG|Divide on US 550 in New Mexico.
Image:Continental Divide and I-40.jpg|Divide on I-40 in New Mexico.
Image:Hoosier Pass Sign.jpg|Hoosier Pass Colorado on May 29, 2006.
Image:Logan Pass-27527.jpg|Logan Pass crosses the Continental Divide in Glacier National Park, Montana.
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