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Carie Paget Channel

This is a typical channel deposit in the vicinity of the K-T boundary. The whitish sediments are sands that have filled a channel cut into the underlying tan sediments.

Meander Bend

A typical modern analog for this system is seen here in a meandering stream in Yellowstone. You may click on any part of this image to identify features in the picture, or you may examine this modern system more closely.

You may return to a view of the Iridium hill area, or click anywhere on the section at right to explore further.

Copyright © 1998 Athro, Limited. All Rights Reserved.
Written by Paul J. Morris
Maintained by Athro Limited Date Created: 2 Jan 1998