William W. Shilts | Shilts Geologic Image Gallery Search | Contact Me

Contorted organic layers in closed crevasses

Location: Bylot Island, Nunavut, Canada
Contorted organic layers in closed crevasses

Contorted organic layers in closed crevasses, probably on Aktineq Glacier (B17). Organic materials such as algae and animals (e.g., geese, hares) fall into crevasses when they are open and are compressed in closed crevasses in zones of compression down-ice from the zones of extension that create the crevasses.












Date taken: July 1991
Photo ID: 0076
High resolution image available
Usage statement


Updated 04/05/2010 AW

PRAIRIE RESEARCH INSTITUTE
William W. Shilts, Executive Director
615 E. Peabody Drive, MC-650
Champaign, IL 61820
Phone: 217-333-5111
Fax: 217-265-4678
prairie@illinois.edu

        Terms of use         Privacy statement
Email the Web Administrator with questions or comments.
© 2013 University of Illinois Board of Trustees. All rights reserved.
For permissions information, contact the Prairie Research Institute.