curred, this shielding depth may not have been constant. Third, specimens whose orientation has not changed during the exposure history must be identifiable. We repeat the acknowledgement of Faure and Taylor in this issu

First Page		Document Content
Date: 2011-05-06 22:11:30 Nussbaum Riegel Meserve Glacier Goodspeed Glacier Asgard Range McMurdo Dry Valleys Geography of Antarctica Sollas Glacier		curred, this shielding depth may not have been constant. Third, specimens whose orientation has not changed during the exposure history must be identifiable. We repeat the acknowledgement of Faure and Taylor in this issu Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 1,20 MB Share Document on Facebook