Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota PDF Download

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Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota

Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota PDF Author: John Truesdale Stewart
Publisher:
ISBN:
Category : Drainage
Languages : en
Pages : 66

Book Description


Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota

Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota PDF Author: John Truesdale Stewart
Publisher:
ISBN:
Category : Drainage
Languages : en
Pages : 66

Book Description


Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota

Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota PDF Author: John T. Stewart
Publisher:
ISBN:
Category : Drainage
Languages : en
Pages : 71

Book Description


Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota (Classic Reprint)

Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota (Classic Reprint) PDF Author: John T. Stewart
Publisher: Forgotten Books
ISBN: 9781528124942
Category :
Languages : en
Pages : 106

Book Description
Excerpt from Report on the Drainage of the Eastern Parts of Cass, Traill, Grand Forks, Walsh, and Pembina Counties, North Dakota The outlet for the drainage of the territory under consideration is the Red River of the North, which rises in Lake Traverse and flows north, forming the boundary between Minnesota and N orth Dakota. It has an average fall of about 6 inches per mile and has a tortuous channel winding in short loops back and forth across a strip of country almost a mile wide. It has a range of 16 to 50 feet between high and low water and at times overflows its banks in places. This usually occurs in the spring, when the ground is frozen and the run - ofi excessive by reason of the sudden melting of the snow at a time when the channel is obstructed by snow and ice. When the water in the river reaches the level of the land adjoining, it retards the drainage of the entire valley, particularly the area near the stream, and causes many of the tributary streams to overflow their banks. The physical features of this river, as compiled from the reports of the engineering corps of the Army and from other sources, are represented in the following table. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.

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Publisher:
ISBN:
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