A geological analysis of this underground reservoir in the Rocky Mountains region.
Written in 2005; 833 words; 3 sources; MLA; $ 29.95
Paper Summary:
Created millions of years of ago through geologic action, the Ogallala aquifer is a vast underground reservoir that runs west of the Mississippi River and east of the Rocky Mountains. This paper examines the evolution and deposition of the aquifer and discusses problems facing it today.
From the Paper:
"The main concern for the Ogallala is the fact that the aquifer has been cut off from most of its natural recharging sources (Ogallala pp). The Rocky Mountains have not supplied the aquifer for more than a thousand years, and the High Plains climate today is classified as semi-arid, receiving only fifteen to twenty inches of rainfall annually, most of which is subject to a high rate of evaporation due to the dry air and high winds (Ogallala pp). Moreover, many of the rivers, such as the Platte, Canadian, and Arkansas, actually drain the aquifer since they have water tables below that of the aquifer (Ogallala pp)."
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