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  2. The Continental Divide of the Americas (also known as the Great Divide, the Western Divide or simply the Continental Divide; Spanish: Divisoria continental de América, Gran Divisoria) is the principal, and largely mountainous, hydrological divide of the Americas.

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  3. The Continental Divide of the Americas, also called the Great Divide, and, especially in Alaska, the Pacific-Arctic Divide, separates the watersheds of the Pacific Ocean from those of the Atlantic and Arctic Oceans.

  4. Continental Divide, fairly continuous ridge of north-southtrending mountain summits in western North America which divides the continents principal drainage into that flowing eastward (either to Hudson Bay in Canada or, chiefly, to the Mississippi and Rio Grande rivers in the United States) and that flowing westward (into the Pacific Ocean).

    • The Editors of Encyclopaedia Britannica
  5. Nov 9, 2009 · The Continental Divide . On April 7, 1805, Lewis and Clark sent some of their crew and their keelboat loaded with zoological and botanical samplings, maps, reports and letters back to St. Louis ...

  6. Oct 19, 2023 · A continental divide is a naturally occurring boundary or ridge separating a continents river systems. Each river system feeds into a distinct ocean basin, bay, or sea. Continental divides are broad, continent -wide example of drainage divides, sometimes just called divides.

  7. The Eastern Continental Divide, Eastern Divide or Appalachian Divide is a hydrological divide in eastern North America that separates the easterly Atlantic Seaboard watershed from the westerly Gulf of Mexico watershed. The divide nearly spans the United States from south of Lake Ontario through the Florida peninsula, and consists of raised ...

  8. Apr 23, 2021 · The Continental Divide of the Americas, also known as the Great Divide or the Western Continental Divide, is a large mountainous divide that passes through most of the continents of North America and South America, extending from the Bering Strait to the Strait of Magellan.

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