Cuyahoga River, Ohio Restoration Study. Third Interim Preliminary Feasibility Report on Erosion and Sedimentation. Volume I. Main Report PDF Download
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Author: CORPS OF ENGINEERS BUFFALO NY BUFFALO DISTRICT. Publisher: ISBN: Category : Languages : en Pages : 136
Book Description
The purpose of this appendix is to identify the sources of sediment in the Cuyahoga River Basin between Independence, Ohio (river mile 13.8) and old Portage, Ohio (river mile 40.25). The sediment entering the river system is derived from erosion of the streambanks and the upland area. The highly erodible principal soil types are composed of silts and sands. Geologic, climatic, and hydrologic factors affect the rate at which soil erosion occurs. For example, soils with steep slopes that are unprotected by vegetative cover erode faster than those on flatter slopes. Erosion is also greater for areas with high annual precipitation and long, cold winters, where vegetation is either dormant or destroyed. The Cuyahoga River Basin historically has had serious erosion and sedimentation as displayed by onsite physical evidence, complaints, and various attempts of remedical actions by local interests. The problem is demonstrated by the naming of the Cuyahoga River which is derived from Indian words meaning 'Crooked River', and the original settler naming of the tributary streams in the area such as Mud Brook, Sand Run, and Yellow Creek. (Author).
Author: CORPS OF ENGINEERS BUFFALO NY BUFFALO DISTRICT. Publisher: ISBN: Category : Languages : en Pages : 136
Book Description
The purpose of this appendix is to identify the sources of sediment in the Cuyahoga River Basin between Independence, Ohio (river mile 13.8) and old Portage, Ohio (river mile 40.25). The sediment entering the river system is derived from erosion of the streambanks and the upland area. The highly erodible principal soil types are composed of silts and sands. Geologic, climatic, and hydrologic factors affect the rate at which soil erosion occurs. For example, soils with steep slopes that are unprotected by vegetative cover erode faster than those on flatter slopes. Erosion is also greater for areas with high annual precipitation and long, cold winters, where vegetation is either dormant or destroyed. The Cuyahoga River Basin historically has had serious erosion and sedimentation as displayed by onsite physical evidence, complaints, and various attempts of remedical actions by local interests. The problem is demonstrated by the naming of the Cuyahoga River which is derived from Indian words meaning 'Crooked River', and the original settler naming of the tributary streams in the area such as Mud Brook, Sand Run, and Yellow Creek. (Author).
Author: Richard Aguglia Publisher: ISBN: Category : Languages : en Pages : 105
Book Description
The purpose of this supplement report is to document the results of the additional upland erosion studies completed subsequent to the Cuyahoga River, Ohio, restoration study third interim preliminary feasibility report (PFR) on erosion and sedimentation, November 1979. These additional studies include studies to identify and quantify indentifiable (Gully) and diffuse (Sheet) nonpoint sources of erosion, and development of management programs to control erosion in the critical areas identified. (Author).
Author: CORPS OF ENGINEERS BUFFALO NY BUFFALO DISTRICT. Publisher: ISBN: Category : Languages : en Pages : 448
Book Description
The purpose of this appendix is to identify the sources of sediment in the Cuyahoga River Basin between Independence, Ohio (river mile 13.8) and old Portage, Ohio (river mile 40.25). The sediment entering the river system is derived from erosion of the streambanks and the upland area. The highly erodible principal soil types are composed of silts and sands. Geologic, climatic, and hydrologic factors affect the rate at which soil erosion occurs. For example, soils with steep slopes that are unprotected by vegetative cover erode faster than those on flatter slopes. Erosion is also greater for areas with high annual precipitation and long, cold winters, where vegetation is either dormant or destroyed. The Cuyahoga River Basin historically has had serious erosion and sedimentation as displayed by onsite physical evidence, complaints, and various attempts of remedial actions by local interests. The problem is demonstrated by the naming of the Cuyahoga River which is derived fom Indian words meaning 'Crooked River', and the original settler naming of the tributary streams in the area such as Mud Brook, Sand Run, and Yellow Creek. (Author).
Author: United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Public Lands, Reserved Water, and Resource Conservation Publisher: ISBN: Category : National parks and reserves Languages : en Pages : 384
Author: United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Public Lands, Reserved Water, and Resource Conservation Publisher: ISBN: Category : National parks and reserves Languages : en Pages : 256
Author: CORPS OF ENGINEERS BUFFALO NY BUFFALO DISTRICT.
Author: CORPS OF ENGINEERS BUFFALO NY BUFFALO DISTRICT.
Author: Richard Aguglia
Author: CORPS OF ENGINEERS BUFFALO NY BUFFALO DISTRICT.
Author: United States. Army. Corps of Engineers. Buffalo District
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Author: United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Public Lands, Reserved Water, and Resource Conservation
Author: United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Public Lands, Reserved Water, and Resource Conservation
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