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•~ ~~ <br />i f't [y Exhibit Dio. 7, would you step down to this exhibit:, ]d r. <br />Aro, and with the pointer indicate to the court w2iere you <br />went upon these premises, the route that you took; <br />A [•?ell, I approached the quarry by the access <br />road, indicated here, I would presume, and I am ~Tt~inq to <br />have to get down to the fire points, and proceeded across <br />roughly through here across over to the western portion <br />of this area, which is in the form of an "L" here, and <br />~..ti,..., then returning back over to this road again, and then coming <br />'a ~ s <br />back to the area transversing a good deal of the e:ocalled, <br />I guess it is proper to say I20 acres by confininc• it to <br />the east side of tailliama Canyon. <br />Q [•?ill you tell the court what you observed in the <br />way of a soil mantle of the area? <br />A The soils of the area that I examined were very <br />shallow, ranging from essentially zero, that 1s bedrock, to <br />perhaps a profile, if you could call it that, of about six <br />inches of soil material. Below the top probably n:oze like <br />3 : i~ <br />three to six inches of a weathered soil material u~as weathered <br />limestone bedrock. <br />4 Approximately what thickness on that dic'. you <br />observe to exist before reaching I believe what you call <br />parent source? <br />A well, this limestone -- <br />:•SR. MORRISON: -- that is very leading, the witness <br />didn't mention parent source. <br />THE COIIRT; Let him proceed. <br />A The term parent material as I used it in my <br />1266 <br />