Write the names of landforms made by continental glacier?
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As the glaciers expand, due to their accumulating weight of snow and ice they crush and abrade and scour surfaces such as rocks and bedrock. The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines, U-shaped valleys, roches moutonnées, overdeepenings and hanging valleys.
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U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.Nunataks, Arêtes, and Horns. ...
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.Nunataks, Arêtes, and Horns. ...Lateral and Medial Moraines. ...
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.Nunataks, Arêtes, and Horns. ...Lateral and Medial Moraines. ...Terminal and Recessional Moraines. ...
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.Nunataks, Arêtes, and Horns. ...Lateral and Medial Moraines. ...Terminal and Recessional Moraines. ...Glacial Till and Glacial Flour. ...
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.Nunataks, Arêtes, and Horns. ...Lateral and Medial Moraines. ...Terminal and Recessional Moraines. ...Glacial Till and Glacial Flour. ...Glacial Erratics. ...
U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.Cirques.Nunataks, Arêtes, and Horns. ...Lateral and Medial Moraines. ...Terminal and Recessional Moraines. ...Glacial Till and Glacial Flour. ...Glacial Erratics. ...Glacial Striations.
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