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No abstract available.

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Glacial drift and Cretaceous sedimentary rocks are the major aquifers in the Yellow Medicine River watershed unit.

\n

The Yellow Medicine and Minnesota Rivers are the major sources of surface water. For physiographic regions – Upland Plain, Slope, Lowland Plain, and Minnesota River Flood Plain – influence surface drainage, and the flow of ground water through the aquifers. The watershed comprises 1070 square miles, including the drainage basin of the Yellow Medicine River (665 square miles) and 405 square miles drained by small streams tributary to the Minnesota River.

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1969 - Water resources of the Buffalo River Watershed, West-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T09:59:47","indexId":"ha307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"307","title":"Water resources of the Buffalo River Watershed, West-central Minnesota","docAbstract":"

The Buffalo River watershed includes two general physiographic areas – a glacial lake plain and an glacial moraine.

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The lake plain, which was formed by Glacial lake Agassiz more than 9,000 years ago, is extremely flat – sloping only a few feet per mile westward near the Red River of the North. The moraine is largely an area of gently rolling hills, but in the eastern “tail” of the watershed the relief locally is over two hundred feet.

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The watershed has an area of about 1,690 square miles and includes most of Clay County and parts of Wilkin, Otter Tail, Becker, and Norman Counties. The population of the area is about 45,500 – 31,000 urban and 14,500 rural.

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The economy is largely agricultural. Sugar beet and wheat farming are dominant in the areas of clay and silt; potato farming is confined mainly to the sandy areas. Dairying and stock raising is important in the morainal area. The larger industries are located in Moorhead and consist of sugar beet, potato, and dairy product processing.

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Water-based recreation consists mostly of fishing in the larger lakes in the morainal area, and water-fowl hunting in the area of prairie potholes – the western part of the morainal area.

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This hydrologic atlas represents a part of a comprehensive study of the water resources of southeastern Michigan. The purpose of the atlas is to present data on (1) the physical features of the Belle River and its tributaries, (2) the characteristics of streamflow, (3) the quality of ground and surface waters, and (4) an evaluation of the ground-water potential of the area. The atlas is one in a series of atlases on several river basins in southeastern Michigan.

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The land surface of the Pine River basin, an area of 194 square miles, is a relatively flat or gently undulating northwest to southeast trending glacial lake plain.

The plain is interrupted by small streams and by a series of former glacial lake beaches. Other irregularities are the morainal hills in the headwaters and the morainal areas that form a large part of the basin divide. Altitudes range from 850 feet above mean sea level in the northwest corner of the basin to 578 feet at the mouth of the Pine river.

Drainage is not well developed in the basin. Many stream courses are poorly defined, having cut only from 3 to 10 feet below the adjacent plain. For this reason, ditches and drains are necessary to effectively drain parts of the basin. There are a few small scattered ponds, but no lakes within the basin.

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