Hammer, W.RTriassic terrestrial vertebrate faunas of Antarctica. In T.N. Taylor and E.L. Taylor (Eds.), Antarctic paleobiology. New York: Springer-Verlag. Hammer, W.R., J.W. Collinson, and W.J. Ryan, IIIA

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Date: 2011-05-06 21:17:48 Vinson Massif Nimitz Glacier Minnesota Glacier Gildea Glacier Donnellan Glacier Geography of Antarctica Ellsworth Mountains West Antarctica		Hammer, W.RTriassic terrestrial vertebrate faunas of Antarctica. In T.N. Taylor and E.L. Taylor (Eds.), Antarctic paleobiology. New York: Springer-Verlag. Hammer, W.R., J.W. Collinson, and W.J. Ryan, IIIA Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 1,84 MB Share Document on Facebook

	3 Most moraines are formed by a combination of processes. Some rock debris is carried at the base of the ice and stacked at the ice margin. Other debris accumulates on the ice surface and slumps off DocID: 1fFmI - View Document
	The Minnesota and Union Glaciers cut across the dominant structural trend of the mountains, while the Newcomer and Nimitz Glaciers follow it. We also sounded along six gravity profiles made earlier by U.S. scientists stu DocID: 159Nu - View Document
	(Bockheim and WilsonThe Ross Sea glaciation has been dated by Stuiver, Denton, and Hughesat 17,000 to 21,000 years ago. In conjunction with the findings of Denton, Rutford, and Andersen (Antarctic Journal DocID: 14bcR - View Document
	Hammer, W.RTriassic terrestrial vertebrate faunas of Antarctica. In T.N. Taylor and E.L. Taylor (Eds.), Antarctic paleobiology. New York: Springer-Verlag. Hammer, W.R., J.W. Collinson, and W.J. Ryan, IIIA DocID: 148t4 - View Document
	900 difference in declination is due to rapid changes in the paleomagnetic field with respect to Antarctica during the Lower Paleozoic cannot be discounted at the present level of coverage. A solid data base from the Pal DocID: 13LE1 - View Document