Geology of the Waterford quadrangle, Virginia and Maryland, and the Virginia part of the Point of Rocks quadrangle
Links
- Document: Report (pdf)
- Plate: Plate 1 (pdf)
- NGMDB Index Page: National Geologic Map Database Index Page
- Download citation as: RIS | Dublin Core
Abstract
The bedrock geology of the Waterford quadrangle and of the Virginia part of the Point of Rocks quadrangle consists of a portion of the Middle Proterozoic basement core and its cover sequence on the eastern limb of the Blue Ridge anticlinorium and the adjacent early Mesozoic Culpeper basin. The three major rock associations in this area are: 1) Middle Proterozoic gneisses intruded by late Proterozoic metadiabase dikes, 2) unconformably overlying late Proterozoic and early Paleozoic metavolcanic and metasedimentary rocks, and 3) Upper Triassic sedimentary strata intruded by early Jurassic diabase. The Triassic and Jurassic rocks are separated from the older rocks by a major normal fault, the Bull Run fault. Late Cenozoic surficial deposits of three major types unconformably overlie the bedrock: colluvium derived from Catoctin Mountain, terrace deposits of the Potomac River, and flood plain alluvium of the Potomac River and its tributaries. -from Authors
Study Area
Publication type | Report |
---|---|
Publication Subtype | USGS Numbered Series |
Title | Geology of the Waterford quadrangle, Virginia and Maryland, and the Virginia part of the Point of Rocks quadrangle |
Series title | Bulletin |
Series number | 2095 |
DOI | 10.3133/b2095 |
Year Published | 1995 |
Language | English |
Publisher | U.S. Geological Survey |
Contributing office(s) | Florence Bascom Geoscience Center |
Description | Report: iv, 35 p.; 2 Plates: 26.50 × 19.00 inches and 40.00 × 30.00 inches |
Country | United States |
State | Maryland, Virginia |
Other Geospatial | Point of Rocks quadrangle, Waterford quadrangle |
Scale | 24000 |
Google Analytic Metrics | Metrics page |