Author: Publisher:
ISBN:
Category : Erosion
Languages : en
Pages : 392
Book Description
Historical Evidence of Ohio River Bank Erosion
Author: Ohio River Bank Erosion Study
Author: United States. Army. Corps of Engineers. Ohio River DivisionPublisher:
ISBN:
Category : Erosion
Languages : en
Pages : 176
Book Description
Ohio River Erosion
Author: Historical Evidence of Ohio River Bank Erosion
Author: A Case Study of Ohio River Bank Erosion
Author: Robert F. TallyPublisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 320
Book Description
The Influence of Tailwater Fluctuation on Ohio River Bank Erosion
Author: Richard J. MazzoniPublisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 274
Book Description
Agriculture and Soil Erosion in the Ohio River Basin
Author: United States. Department of AgriculturePublisher:
ISBN:
Category : Agriculture
Languages : en
Pages : 10
Book Description
Erosion Control of the Ohio River Valley at Lee Bottom in Jefferson Co. Indiana and Payne Hollow in Trimble Co. Kentucky
Author: Jennifer K. FryErosion and Related Land Use Conditions on the Muskingum River Watershed
Author: Herbert Howe MorsePublisher:
ISBN:
Category : Erosion
Languages : en
Pages : 60
Book Description
Cuyahoga River, Ohio Restoration Study. Third Interim Preliminary Feasibility Report on Erosion and Sedimentation. Volume I. Main Report
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).