Laserfiche WebLink
. <br />June 28,'l0G <br />David and Judy King <br />L&cA 1ob No. 6A076 <br />Page 3 <br />about thc southwest comcr of thc lot, tt�en tums casterly anJ exits the lot at ubout mid-length of <br />its cast boundary. <br />At the south cnd of the northem lot ure two sets of slopes and benches lhut descend norlhward. <br />The slopes arc cach roughly at about 25 to 30 percc,nt grade with 4 to S feet of vertical drop, mid <br />the benchcs are about 12 to 16 feet widc. Below lhesc slopes and benches, the ground in the <br />southeastem quarter of the northcrn lot continues to descend northcrly at about 52 to 58 perccnt <br />grade to the vallcy of the bowl, and the ground over the n;st of thc lot slopes c'.own easterly at <br />about 31 to G7 perccnt gradc towurds thc vallcy of thc bowl nnd lhe cast boundary of thc lot. Thc <br />southem slopes and tx:nchcs arc covercJ with !a�m grass. The mmaining nrea of thc lot is dottcJ <br />with mature anJ young deciduoss trecs with occ�vsional mature evergrecn trces mixed in, and <br />with the ground covcred hy thick �ndcrbnish. <br />GGOLOGIC SF,TTING <br />'►�he Preliminary Geolo�c M�� of Ihe Mukiltco and I:verc:lt Ouadraneles, Snohomish County, <br />Washineton, by Mackey Smith, publishcd by U. S. Gcological Survey in 1976, was referenced <br />for the gcologic anJ soil conJitions of thc northem I�t. According to this publication, the <br />surficial soil units at and in the vicinity of thc lot are mapped as Esperance Sand member (Qe) <br />undcrlain by Whidbcy formation (QH,). <br />'I hc gcology ot' the Puget Sound Lowland has been modified by the advance and retrcat of <br />scvcral glacicrs in thc past tuid sabscqucnt dc�sits und crosion. The latest glacier ndvnnced to <br />thc Pugct Sound Lowlnnd is refcrrcd to as thc Vashon Stade of thc Frnscr Glaciation, which has <br />oceurrcd during thc latcr stages of thc 1'Icistoccnc rpoch und retrented from the region somc <br />14,500 ycars ago. <br />LIU & AS�OCIATES, INC. <br />