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  2. Fjord - Wikipedia

    en.wikipedia.org/wiki/Fjord

    A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. [6] According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end ...

  3. Kenai Fjords National Park - Wikipedia

    en.wikipedia.org/wiki/Kenai_Fjords_National_Park

    Kenai Fjords National Park. Kenai Fjords National Park is a national park of the United States that comprises the Harding Icefield, its outflowing glaciers, and coastal fjords and islands. The park covers an area of 669,984 acres (1,046.9 sq mi; 2,711.3 km 2) [1] on the Kenai Peninsula in south-central Alaska, west of the town of Seward.

  4. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    Glacial landform. Glacial landforms are landforms created by the action of glaciers. Most of today's glacial landforms were created by the movement of large ice sheets during the Quaternary glaciations. Some areas, like Fennoscandia and the southern Andes, have extensive occurrences of glacial landforms; other areas, such as the Sahara, display ...

  5. Overdeepening - Wikipedia

    en.wikipedia.org/wiki/Overdeepening

    Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are hundreds of metres below the lowest continuous surface line (the thalweg) along a valley or watercourse. This phenomenon is observed under modern day glaciers, in salt-water fjords and fresh-water lakes ...

  6. U-shaped valley - Wikipedia

    en.wikipedia.org/wiki/U-shaped_valley

    The glacier visible at the head of the valley is the last remnant of the formerly much more extensive glacier which carved it. U-shaped valley with lake in Myklebustdalen, Nordfjord, Sogn og Fjordane, Norway. U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation.

  7. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    True fjords are formed when valley glaciers retreat and seawater fills the now empty valley. They can be found in mountainous, glaciation-affected terrain. [18] Examples include: Hvalfjörður, Iceland; Hornsund, Svalbard; Sognefjord, Norway; An existing valley glacier of this type is Jakobshavn Glacier in Greenland

  8. List of fjords of the United States - Wikipedia

    en.wikipedia.org/wiki/List_of_fjords_of_the...

    Nassau Fjord [10] Alaska. 60°15′46″N 148°21′25″W  /  60.2628°N 148.3569°W  / 60.2628; -148.3569  (Nassau Fiord) Puget Sound [11] Washington. 47°36′N 122°27′W  /  47.6°N 122.45°W  / 47.6; -122.45  (Puget Sound) Puget Sound is a fjord system of many flooded glacial valleys and is the southernmost ...

  9. Misty Fjords National Monument - Wikipedia

    en.wikipedia.org/wiki/Misty_Fjords_National_Monument

    Misty Fjords National Monument (or Misty Fiords National Monument) is a national monument and wilderness area administered by the U.S. Forest Service as part of the Tongass National Forest. Misty Fiords is about 40 miles (64 km) east of Ketchikan, Alaska , along the Inside Passage coast in extreme southeastern Alaska , comprising 2,294,343 ...