Diatom evidence for the persistence of stagnant glacial ice in minnesota

Maj Britt Florin, Jr E. Wright

Research output: Contribution to journalArticlepeer-review

62 Scopus citations

Abstract

The basal organic deposit in many Minnesota lakes includes wood fragments and other coarse plant material of terrestrial origin, along with diatoms characteristic of soils, moss, and other terrestrial habitats. The material probably represents the floor of a superglacial forest; it is overlain by similar material deposited in shallow pools that formed when buried Wisconsin dead ice melted beneath a cover of till or outwash.

Original languageEnglish (US)
Pages (from-to)695-704
Number of pages10
JournalBulletin of the Geological Society of America
Volume80
Issue number4
DOIs
StatePublished - 1969

Bibliographical note

Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.

Fingerprint Dive into the research topics of 'Diatom evidence for the persistence of stagnant glacial ice in minnesota'. Together they form a unique fingerprint.

Cite this