EXERCISE 38 PROBLEMS-PART I bound in Mip TMfa, a section of the USCIS -Spring Hill Ldaba he take 1:34030 cooler interval 30 feel, and Figure 189, a sicsergeant of the wa is waiting deposit at the food of the Pahammers what evidence shown on the map and stereogiant suggests that the material in the depol des me round of wolverat ledisi? (Thre Courant the appearance of the dejoin with Which Liad of mass wasting must bely left this deposit, Op of Now or a bpe of sick? Who evidence shown on the map and Mereogram upports your answerfollin: Note the path taken by the miserial on its way downslope.) Steep, Sloping contours forming Plat grade.La foot it to indicate it's convotiofanon Salimenter EXERCISE 38 PROBLEMS-PART II following questions are based on Map T-26a, a section of the USGS "Spring Hill, Idaho," wrangle (scale 1:24,000; contour interval 20 feet), You are going to calculate the approximate of the mass wasting deposit shown at the foot of the Pahsimeroi Mountains. How thick is the deposit at the end (the "toe") of the deposits (Take the 6800' contour to be the top of the deposit). w 20 Although the deposit is somewhat irregular, assume that it is square or rectangular shape. Estimate the length of the two sides of the deposit that are in contact with fountain front (the northwest [NW] side and the southwest side [SWI), then calculate face area. 0299 feet x 4724 1 29 7564/76 (SW side length) (socal surface seca) square feet uming that your answer to problem I represents the uniform thickness of the dep uplistic assumption), calculate the total volume of the deposit. G feet x 4721 * thickness) square feet (total surface arca) (approx. total volume) cubic feet LXWXT 265