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Geology of the Chesapeake and Ohio Canal National Historical Park and Potomac River corridor, District of Columbia, Maryland, West Virginia, and Virginia

Author: Scott Southworth; United States. National Park Service.
Publisher: Reston, Va. : U.S. Dept. of the Interior, U.S. Geological Survey, 2008.
Series: U.S. Geological Survey professional paper, 1691.
Edition/Format:   eBook : Document : National government publication : EnglishView all editions and formats
Summary:
The Chesapeake and Ohio Canal National Historical Park is 184.5 mi long and extends from Washington, D.C., to Cumberland, Md. The canal passes through three physiographic provinces including the Piedmont, Valley and Ridge, and the Blue Ridge; the map area also includes rocks of the Coastal Plain and Appalachian Plateaus provinces. Each province contains unique packages of rocks that influenced the character of the  Read more...
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Additional Physical Format: Paper version:
Geology of the Chesapeake and Ohio Canal National Historical Park and Potomac River corridor, District of Columbia, Maryland, West Virginia, and Virginia
(DLC) 2005040051
(OCoLC)58051246
Material Type: Document, Government publication, National government publication, Internet resource
Document Type: Internet Resource, Computer File
All Authors / Contributors: Scott Southworth; United States. National Park Service.
OCLC Number: 264703138
Notes: Title from title screen (viewed Oct. 29, 2008).
Description: 1 online resource ([154] pages) : color illustrations, maps.
Series Title: U.S. Geological Survey professional paper, 1691.
Responsibility: by Scott Southworth [and others] ; prepared in cooperation with the National Park Service [and others].

Abstract:

The Chesapeake and Ohio Canal National Historical Park is 184.5 mi long and extends from Washington, D.C., to Cumberland, Md. The canal passes through three physiographic provinces including the Piedmont, Valley and Ridge, and the Blue Ridge; the map area also includes rocks of the Coastal Plain and Appalachian Plateaus provinces. Each province contains unique packages of rocks that influenced the character of the canal and towpath. The ages of the bedrock encountered along the length of the park range from Mesoproterozoic to Jurassic and represent a variety of tectonic and depositional environments. The different rock types and surficial deposits dictated the various construction methods for the canal, which was excavated in Quaternary flood-plain deposits as well as through bedrock. The ancient course of the Potomac River and the deposits it left behind also influenced the location of the canal and towpath. The engineers made good use of the many rock types to construct the locks, dams, aqueducts, and culverts that guided water from the Potomac River into the canal and maintained the water level as canal boats traveled between higher elevations in western Maryland to sea level in Washington, D.C. The canal and towpath provide a unique transect across the central Appalachian region for examining the rich geologic diversity and history.

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