Glacial geology Late Quaternary geology of the Rennick Glacier area, northern Victoria Land GEORGE

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Date: 2011-05-06 05:44:21 Geology Ross Dependency Glacial landforms Sediments Glacier Rennick Bay Moraine Old and Young Drift Mesa Range Pennell Coast Geography of Antarctica Glaciology		Glacial geology Late Quaternary geology of the Rennick Glacier area, northern Victoria Land GEORGE Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 3,32 MB Share Document on Facebook

	Access Antarctica Gateway Antarctica, Centre for Antarctic Studies and Research June 2016 DocID: 1pC4p - View Document
	dently, this clast was once at the base of the east antarctic ice sheet which may be more than 3 kilometers thick, according to the ice-flow model of Whillans and Cassidy (1983), although an extrapolation of the radar so DocID: 159iP - View Document
	present. Orientations of abundant striations on fault surfaces (slickensides) and other features clearly indicate normal or reverse faulting with little or no strike-slip movement (figure 3). The last of these appears re DocID: 1586N - View Document
	farther north during the maximum stages of these glaciations, respectively (Mayewski et alRetreat from the maximum position held by Rennick ice continues to be characterized by inland migration of the Rennick Gl DocID: 14xuZ - View Document
	References Faure, C., M. L. Kalistrom, and T. M. MensingClassification and age of terrestrial boulders in the Elephant and Reckling moraines. Antarctic Journal of the U.S., 19(5):Faure, C. and K. S. Taylo DocID: 14rWR - View Document