Document Type

Article

Publication Title

Northeastern Geology

Rights and Access Note

This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s).

Publication Date

1980

First Page

7

Last Page

12

Issue Number

1

Volume Number

2

Abstract/ Summary

Study of stratified glacial deposits near Farmington, New Hampshire reveals that the retreat of Late Wisconsin ice in this area proceeded by means of ice-marginal stagnation. Eskers in t his area were formed within localized ice masses a t or near the base of thin ice by streams which had dendritic patterns and were subaerially exposed.

Citation/Publisher Attribution

Coupland, D., and Mayewski, P.A. (1980). An example of eskers formed in stagnant ice, Northeastern Geology 2(1): 7-12.

Publisher Statement

© Copyright 1980 by Northeastern Science Foundation

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In Copyright - Educational Use Permitted.