Alluvial stratigraphy of the Potomac River valley bottom near Petersburg and Moorefield, West Virginia

1989 ◽  
Author(s):  
R.B. Jacobson ◽  
R.C. Linton ◽  
Meyer Rubin
Keyword(s):  
West Virginia ◽  
River Valley ◽  
Potomac River ◽  
Valley Bottom ◽  
Potomac River Valley

Marcey Creek Site: An Early Manifestation in the Potomac Valley

1948 ◽  
Vol 13 (3) ◽  
pp. 223-227 ◽  
Author(s):  
Carl Manson
Keyword(s):  
River Valley ◽  
National Museum ◽  
Potomac River ◽  
Potomac River Valley ◽  
Early Manifestation

When William Henry Holmes of the U. S. National Museum explored the Potomac River Valley in 1890, he studied and described most of the major village sites and cultures to be found in the area known as "Tidewater."1 The Marcey Creek site is located at the head of Tidewater, overlooking the Little Falls of the Potomac, but was not reported by Holmes.

Lithic technology in the Middle Potomac River Valley of Maryland and Virginia

2004 ◽  
Vol 19 (7) ◽  
pp. 707-709
Author(s):  
Steve Cole
Keyword(s):  
Lithic Technology ◽  
River Valley ◽  
Potomac River ◽  
Potomac River Valley

scholarly journals A Stepwise GIS Approach for the Delineation of River Valley Bottom within Drainage Basins Using a Cost Distance Accumulation Analysis

Water ◽  
2021 ◽  
Vol 13 (6) ◽  
pp. 827
Author(s):  
Gasper L. Sechu ◽  
Bertel Nilsson ◽  
Bo V. Iversen ◽  
Mette B. Greve ◽  
Christen D. Børgesen ◽  
...  
Keyword(s):  
Spatial Data ◽  
Nutrient Loading ◽  
Drainage Basin ◽  
River Valley ◽  
Management Tool ◽  
Drainage Basins ◽  
Valley Bottom ◽  
Management Actions ◽  
Cost Distance ◽  
River Valleys

River valley bottoms have hydrological, geomorphological, and ecological importance and are buffers for protecting the river from upland nutrient loading coming from agriculture and other sources. They are relatively flat, low-lying areas of the terrain that are adjacent to the river and bound by increasing slopes at the transition to the uplands. These areas have under natural conditions, a groundwater table close to the soil surface. The objective of this paper is to present a stepwise GIS approach for the delineation of river valley bottom within drainage basins and use it to perform a national delineation. We developed a tool that applies a concept called cost distance accumulation with spatial data inputs consisting a river network and slope derived from a digital elevation model. We then used wetlands adjacent to rivers as a guide finding the river valley bottom boundary from the cost distance accumulation. We present results from our tool for the whole country of Denmark carrying out a validation within three selected areas. The results reveal that the tool visually performs well and delineates both confined and unconfined river valleys within the same drainage basin. We use the most common forms of wetlands (meadow and marsh) in Denmark’s river valleys known as Groundwater Dependent Ecosystems (GDE) to validate our river valley bottom delineated areas. Our delineation picks about half to two-thirds of these GDE. However, we expected this since farmers have reclaimed Denmark’s low-lying areas during the last 200 years before the first map of GDE was created. Our tool can be used as a management tool, since it can delineate an area that has been the focus of management actions to protect waterways from upland nutrient pollution.

scholarly journals Consequences of the river valley bottom transformation after extreme flood (on the example of the Niida River, Japan)

2018 ◽  
Vol 107 ◽  
pp. 012002
Author(s):  
D Botavin ◽  
V Golosov ◽  
A Konoplev ◽  
Y Wakiyama
Keyword(s):  
River Valley ◽  
Valley Bottom ◽  
Extreme Flood
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