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Alaska Peninsula

Peninsula extending towards the Aleutian Islands in Southwest Alaska, United States

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Map of Alaska Peninsula National Wildlife Refuge
U.S. Fish and Wildlife Service · Public domain

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Through Continent, Volcano and Erosion

In literature (especially Russian), the term Alaska Peninsula was used to denote the entire north-western protrusion of the North American continent, or all of what is now the state of Alaska, exclusive of its panhandle and islands. The Lake and Peninsula borough, the Alaskan equivalent of a county, is named after the peninsula.

The Alaska/Aleutian Peninsula is also grouped into Southwest Alaska.

The other large peninsulas in Alaska include the Kenai Peninsula and the Seward Peninsula.

Geography

The base of the Alaska Peninsula extends outward from the end of the Alaska Range.

The Aleutian Range is a very active volcanic mountain range which runs along the entire length of the peninsula. Within it lie Wildlife Refuges, including the Katmai National Park and Preserve, the Aniakchak National Monument and Preserve and the Becharof National Wildlife Refuge, the Alaska Peninsula National Wildlife Refuge, and the Izembek National Wildlife Refuge. The most active volcano along the volcanic mountain range is Pavlof Volcano which is more than 8,251 feet (2,515 meters)(see also: Aleutian Arc).

The southern side of the Alaska Peninsula is rugged and mountainous, created by the uplifting tectonic activity of the North Pacific Plate subsiding under a western section of the North American Plate; the northern side is generally flat and marshy, a result of millennia of erosion and general seismic stability. The northern and southern shores are likewise quite different. The northern Bristol Bay coastal side is generally turbid and muddy, experiences tidal extremes, and is relatively shallow; the Pacific side, which is also known as the "ring of fire", has relatively small tidal activity and the water is deep and clear.

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