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KameA steep conical hill composed of glaciofluvial sediments. This feature develops when glacial crevasses and depressions in stagnant glacial ice are filled with sand and gravel deposits from sediment lo [..]
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KameStratified drift deposited in depressions and cavities in stagnant ice and left as irregular, steep sided hills when the ice is melts.
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Kamen. A short, steep-sided knoll of glacial sediment.
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KameMonticule ou butte de forme irrégulière constitué de couches de gravier et de sable déposées par l'eau de courant des glaciers en fonte.
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KameAn irregular shaped hill or ridge of sand or gravel that is deposited by stream water from melting glaciers.
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KameA mound of material marking the former edge of an ice-sheet or glacier.
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KameA deposit, composed largely of material sorted by moving water, formed in direct contact with glacier ice. See esker, moulin kame, kame delta, and kame terrace.
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KameJapanese for “turtle”, the term KAME is used in computing circles to refer to the KAME Project, who work on an implementation of IPv6.
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Kamea short ridge, hill, or mound of stratified drift deposited by glacial meltwater.
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Kamea short ridge, hill, or mound of stratified drift deposited by glacial meltwater. kame terrace
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