"' Newall Glacier "'is a glacier in the east part of the Asgard Range of Victoria Land, flowing east between Mount Newall and Mount Weyant into the Wilson Piedmont Glacier.
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Alpine glaciers can be straight rivers of ice, long sweeping rivers, spread in a fan-like shape ( Piedmont glaciers ), and curtains of ice that hang from vertical slopes of the mountain peaks.
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The park's glacial features include Malaspina Glacier, the largest piedmont glacier in North America, Hubbard Glacier, the longest tidewater glacier in Alaska, and Nabesna Glacier, the world's longest valley glacier.
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"' Geodetic Glacier "'( ) is a glacier flowing east from Bettle Peak along the north side of the Thomas Heights into Bowers Piedmont Glacier, on the Scott Coast of Victoria Land, Antarctica.
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Montane and piedmont glaciers formed the land by grinding away virtually all traces of the older G�nz and Mindel glaciation, by depositing base moraines and terminal moraines of different retraction phases and loess deposits, and by the pro-glacial rivers'shifting and redepositing gravels.
