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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. 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.

  5. 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 ...

  6. 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 ...

  7. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. [1] The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. [2] Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small ...

  8. List of fjords in Canada - Wikipedia

    en.wikipedia.org/wiki/List_of_fjords_in_Canada

    Mountainous glaciated areas in Canada are along the British Columbia Coast: from the Alaskan border along the Portland Canal [ 1 ] to Indian Arm. [ 2 ] Kingcome Inlet is a typical west coast fjord. [ 3 ] In Newfoundland and Labrador, Saglek Fiord, [ 4 ] Nachvak Fiord, [ 5 ] and Hebron Fiord, [ 6 ] are in Labrador.

  9. Geography of Norway - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Norway

    During the last glacial period, as well as in many earlier ice ages, virtually the entire country was covered with a thick ice sheet. The movement of the ice carved out deep valleys. As a result of the ice carving, Sognefjorden is the world's second deepest fjord and Hornindalsvatnet is the deepest lake in Europe.