Fingerprinting of glacial silt in lake sediments yields continuous records of alpine glaciation (35-15ka), western USA

Joseph G. Rosenbaum, Richard L. Reynolds, Steven M. Colman

Research output: Contribution to journalArticlepeer-review

6 Scopus citations

Abstract

Fingerprinting glacial silt in last glacial-age sediments from Upper Klamath Lake (UKL) and Bear Lake (BL) provides continuous radiocarbon-dated records of glaciation for the southeastern Cascade Range and northwestern Uinta Mountains, respectively. Comparing of these records to cosmogenic exposure ages from moraines suggests that variations in glacial flour largely reflect glacial extent. The two areas are at similar latitudes and yield similar records of glacial growth and recession, even though UKL lies less than 200. km from the ocean and BL is in the continental interior. As sea level began to fall prior to the global Last Glacial Maximum (LGM), existing glaciers in the UKL area expanded. Near the beginning of the global LGM (26.5 ka), the BL record indicates onset of glaciation and UKL-area glaciers underwent further expansion. Both records indicate that local glaciers reached their maximum extents near the end of the global LGM, remained near their maxima for ~1000. yr, and underwent two stages of retreat separated by a short period of expansion.

Original languageEnglish (US)
Pages (from-to)333-340
Number of pages8
JournalQuaternary Research (United States)
Volume78
Issue number2
DOIs
StatePublished - Sep 2012
Externally publishedYes

Bibliographical note

Funding Information:
We thank M. Hudson, E. Leonard, and an anonymous reviewer for their constructive criticism of earlier versions of the manuscript. Funding was provided by the Climate and Land Use Change Research Program of the U.S. Geological Survey .

Copyright:
Copyright 2012 Elsevier B.V., All rights reserved.

Keywords

  • Bear Lake
  • Cascade Range
  • Glacial silt
  • Lake sediment
  • Last glacial interval
  • Magnetic properties
  • Uinta Mountains
  • Upper Klamath Lake

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