Slope area drainage basin, North Dakota.
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Slope area drainage basin, North Dakota.

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Published in [Bismarck .
Written in English



  • North Dakota.


  • Drainage -- North Dakota.

Book details:

Edition Notes

StatementReport by State Planning Board and Works Progress Administration O.P. no. 665-73-3-67. June 30, 1939.
LC ClassificationsTC977.N9 A5 1939
The Physical Object
Pagination10 p. l., 142 (i.e. 148), 27 p. incl. maps (1 fold.) tables, diagrs.
Number of Pages148
ID Numbers
Open LibraryOL6394018M
LC Control Number39028636

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These two drainages are known as the Missouri River Drainage and the Hudson Bay Drainage. The Missouri River drainage basin in North Dakota includes the major sub-basins of the Missouri River and James Rivers. The Hudson Bay drainage basin includes the Mouse and Red River systems, as well as the Devils Lake Basin. University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects The surface morphology of a small drainage basin in the North Dakota Badlands J. Ladd Hagmaier University of North Dakota Follow this and additional works at: Part of theGeology CommonsCited by: 1. A geomorphic history based on topographic map evidence Abstract: The southwest North Dakota Missouri Slope region is located south and west of the Missouri River and east and south of the Little Missouri River in North Dakota and includes the Knife, Heart, Cannonball River drainage basins and their drainage divides with the Little Missouri River.. North Dakota Administrative Code. V– Contributing Drainage Area. Research of existing plans, files, special studies, etc. shall be performed to determine the drainage area and discharge values used in the previous design. These materials shall also be used if any hydraulic concerns relative to the site have been Size: 5MB.

These beaches and scarps mark the eastern margin of the Red River Valley, and they are the southward continuation of the Pembina Escarpment. The Pembina Escarpment is most prominent in northeastern North Dakota where it rises to above the flat floor of the Red River Valley. Drainage Complaints Drainage Complaints. A complaint of unauthorized construction of a drain may be filed with the WRD of jurisdiction. The WRD will determine if a landowner or tenant constructed a drain without first securing a permit as required under NDCC or , or in conflict with the terms or conditions of a drainage permit. Map 1: North Dakota has three distinct regions based on geography and soil. The Red River Valley is flat with good soil and little drainage. The Drift Prairie is characterized by small ponds, and hills, and rocky soil. The Missouri Plateau is the highest land in North Dakota. Related Topics: drainage, slope, french drains. You create surface drainage by grading an area so that water collects and flows to a lower elevation away from the site. Regardless of surface characteristics, when it comes to surface drainage, slope is the most important issue to g: North Dakota.

Other terms for drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. [5] [6] [7] In North America, the term watershed is commonly used to mean a drainage basin, though in other English-speaking countries, it is used only in its original sense, that of a drainage divide. provide for adequate drainage for constructing and maintaining the State Highway System, it is not its policy nor responsibility to provide improved drainage for the general area traversed by such roads, unless incidental to the drainage of the road or highway itself. Drainage File Size: 1MB. For urban drainage areas the method most generally used by NDDOT is the Rational Method More detail to come Other accepted methods for Hydrologic design FHWA method “Hydrology Manual for North Dakota” published by the Natural Resources Conservation Service Suitable hydrograph methods may be File Size: 1MB. The explanatory basin variables used in the equations are contributing drainage area (CA), in square miles; and main channel slope (S), in feet per mile. The regression equations were developed from peak-discharge records available for continuous- and partial-record streamflow gaging stations and are applicable to rural, unregulated streams.