Palouse 04
The peculiar and picturesque silt dunes which characterize the Palouse Prairie were formed during the ice ages (Alt and Hyndman 1989). Blown in from the glacial outwash plains to the west and south, the Palouse hills consist of more or less random humps and hollows. The steepest slopes, which may reach 50% slope, face the northeast. The highly productive loess ranges from 5 to 130 cm deep.[8] Large areas of level land are rare. wikepedia
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