Reinterpretation of the Burmester core, Bonneville basin, Utah

Charles G. Oviatt, Robert S. Thompson, Darrell S. Kaufman, Jordon Bright, Richard M. Forester

Research output: Contribution to journalArticle

77 Scopus citations

Abstract

Initial interpretation of the sediments from the Burmester core (Eardley et al. (1973). Geological Society of America Bulletin 84, 211-216) indicated that 17 deep-lake cycles, separated by shallow-lake and soil-forming intervals, occurred in the Bonneville basin during the Brunhes Chron (the last 780 x 103 yr). Our re-examination of the core, along with new sedimentological, geochronological, and paleontological data, indicate that only four deep-lake cycles occurred during this period, apparently correlative with marine oxygen-isotope stages 2, 6, 12, and 16. This interpretation suggests that large lakes formed in the Bonneville basin only during the most extensive of the Northern Hemisphere glaciations.

Original languageEnglish (US)
Pages (from-to)180-184
Number of pages5
JournalQuaternary Research
Volume52
Issue number2
DOIs
StatePublished - Sep 1999

ASJC Scopus subject areas

  • Arts and Humanities (miscellaneous)
  • Earth-Surface Processes
  • Earth and Planetary Sciences(all)

Fingerprint Dive into the research topics of 'Reinterpretation of the Burmester core, Bonneville basin, Utah'. Together they form a unique fingerprint.

  • Cite this

    Oviatt, C. G., Thompson, R. S., Kaufman, D. S., Bright, J., & Forester, R. M. (1999). Reinterpretation of the Burmester core, Bonneville basin, Utah. Quaternary Research, 52(2), 180-184. https://doi.org/10.1006/qres.1999.2058