Glacial Age Marsh, Lafayette Park, Washington, D.C
Author:
- 22 August 1969
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 165 (3895) , 795-797
Abstract
Organic sediments beneath historic Lafayette Park mark the site of a freshwater marsh which bordered the Potomac River when it was 15 meters above its present level. Plant microfossils and ice-rafted boulders indicate a climate much colder than now. The carbon-14 age of more than 45,000 years and palynological studies suggest an early Wisconsin age.Keywords
This publication has 4 references indexed in Scilit:
- Littoral of the Northeastern United States: Late Quaternary WarpingScience, 1968
- U.S. Geological Survey Radiocarbon Dates IXRadiocarbon, 1967
- Possible Late Pleistocene Uplift Chesapeake Bay EntranceThe Journal of Geology, 1965
- Pleistocene Sea Levels, Southeastern VirginiaScience, 1963