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<br />I <br /> <br />f'~~~..,~~ <br />, ", .~, ." j ,) <br /> <br />I <br /> <br />I <br /> <br />C~mponents of the agricultural water supply system which <br /> <br /> <br />r~ly on surface water as a supply source include both ditches <br /> <br />a~d reservoirs. In the 72.5 mile reach of the South Platte <br /> <br /> <br />Rfver from Kersey to Balzac, there exist 17 ditch and/or <br /> <br /> <br />r~servoir diversions. Specific features of the surface water <br /> <br /> <br />sy;stem will be inventoried and evaluated in detail in a <br /> <br /> <br />s~bsequent section of this report. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />GROUND WATER <br /> <br />I <br /> <br />T~e South Platte River Valley encompasses the main-stem South <br /> <br /> <br />Plhtte aquifer as well as portions of alluvial ground water <br /> <br /> <br />baains underlying major tributaries. These alluvial aquifers <br /> <br /> <br />typically consist of an ancient stream channel eroded in the <br />1 <br /> <br />beprock, partly filled in with unconsolidated sand, gravel, <br /> <br /> <br />anti clay. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Th~ lower aquifer systems which underlie alluvial deposits are <br /> <br /> <br />us~ally comprised of water bearing formations of low <br /> <br />permeability. Yields from wells penetrating the lower <br /> <br /> <br />aqhifers are smaller than those tapping the alluvial system. <br /> <br /> <br />Repharge of the lower aquifer OCCllrs through outcroppings where <br /> <br /> <br />th~ aquifer material is exposed on the land surface, or from <br /> <br /> <br />percolating water from overlying formations. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Water bearing characteristics of geologic formations in the South <br />Pl~tte River Valley are depicted in Table 2-1. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />2-7 <br /> <br />",.1... il <br /> <br />~. / <br /> <br />_ <-_,,'.....'.,..k__,iJ._=.',L <br /> <br />q <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />, <br />:\ <br />