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<br /> <br />1 <br /> <br />1 <br />LJ <br />1 <br /> <br />1 <br />1 <br />i <br />1 <br /> <br />1 <br />1 <br />1 <br />1 <br />1 <br /> <br />• EXHIBIT D (Cont'd) <br />useable ~~~hen mixed with clays from the other three zones. Clay <br />Zone 1 is approximately 99 feet thick. Clay Zone 2 is approximately <br />14 feet thick. Clay Zone 3 is slightly more than 55 feet thick, <br />and Clay Zone 4 is approximately 35 feet thick. The apparent <br />Y~orizontal thicknesses are considerably greater, being 70 feet, <br />20 feet, 80+ feet and 50 feet, respectively. <br />,~~ - - <br />\~ ~_-`___ _ __ I(~ <br />- , - _FO4(t c[AYMEm g6 QS-oF rHE~ _ ~ -_ <br />Kn ~ - ARA MIE_ _ - ~ - _ = ~ - <br />k h ---'~ - _ - ;-- <br />P ~'- - <br />West to East Cross-Section ------- Sketch 1 <br />~; <br />C<nY <br />Kz <br />.~ Kf h::~:... K <br />.' <br />C~nY C~nY CcnY <br />#+AtONF ~I Q #y <br />KI or+c K I <br />KI <br />t+.Io 3o Yo <br />~1 <br />\ CLq`( <br />#3 <br />KI <br />5a 80. <br />.:-- <br />West to East Cross-Section -- Detail of Clay - Sketch 2 <br />Underlying the Laramie is the Fox Hill formation (see Sketch 1). <br />The Fox Hill is a sandstone of Upper Cretaceous age. This sand- <br />stone is porous and permeable in most areas within the Louisville <br />7 <br />