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Original Articles

Till diskussionen om Gävleproblemen

Pages 409-412 | Published online: 06 Jan 2010
 

Abstract

The author has sinco several years collected proofs that the last ice movement in the district round Gävle has been directed towards SE and SSE. In the following paper further proofs of this are given with the aid of analyses of the glacial surfaces of outcropping rocks and the direction of long till boulders.

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