Glacial age marsh, Lafayette Park, Washington, D.C.
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.
Citation Information
Publication Year | 1969 |
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Title | Glacial age marsh, Lafayette Park, Washington, D.C. |
Authors | A.S. Knox |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Science |
Index ID | 70010241 |
Record Source | USGS Publications Warehouse |