Formation of ice-stream rafts by recrystallization RICHARD B. ALLEY

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Date: 2011-05-06 20:44:32 Metallurgy Glaciology Ice sheet dynamics Glacier Ford Ranges Mount Lockhart Bird Bluff Mercer Ice Stream Whillans Ice Stream Geography of Antarctica Physical geography Marie Byrd Land		Formation of ice-stream rafts by recrystallization RICHARD B. ALLEY Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 2,90 MB Share Document on Facebook

	Ice stream C, which is next to ice stream B, is in contrast, virtually stagnant. Its velocity is less than 10 meters per year (McDonald and Whillans, in press), and it must be thickening. The net mass accumulation for th DocID: 159ou - View Document
	phy was directed largely to determining if annual strata can be reliably counted (with a view to possible deep drilling later). The strain grid at the Upstream B camp was remeasured (figure). The weather at the camps sho DocID: 159ln - View Document
	Land ice studies Transient behavior of ice stream B and Crary Ice Rise, West Antarctica R.A. BINDSCHADLER National Aeronautics and Space Administration Goddard Space Flight Center DocID: 14gLa - View Document
	Formation of ice-stream rafts by recrystallization RICHARD B. ALLEY DocID: 14eMp - View Document
	Sticky spots under ice streams RICHARD B. ALLEY DocID: 14eLg - View Document