7825 EVERGREEN WAY 2018-01-01 MF Import

Embar Equities Corporation E-2773 Plovember �4, 1985 Page 2 BasE:d on our discussions with you, we underatand that it is planned to construct two, single-story retail structuretz having 15,000 and 11,000 square feet. A 2100 aquare foot cirive-in restaurant £acility is being considered for the northeast coiner• If any of the above design cri.*.eria change, we should be conaulted to review the recortonendations contained in this rePo:^t. In any case, it is recommended that Farth Consultants, Inc. provide a gecieral review o¢ the final design. SITE COAiD7CTSON& Surface The subject site is located in the southeast corner of the intersection formed by Evergr.een Way and Campus Parkway. The site comprises 2.85 acres with four hundred fifteen (415) feet fronting Evergreen Way and three hundred (�00) feet along Campus Parkway. Undevelo��ed land bounds the site to the south and Cascade High School Flayfield property bounds the site to the east. Presently, no development has uccurred on the parcel le3ving it in a natural state with a moderately dense alder tree cover, ecattered small diameter cedar trees and isolated large diameter fir trees. Associated with the tree cover i.e an undergrowth of native bushes. The site topography has a relatively gentle slope to the east. The total elevation differenti.al across the site is approximately sixteen (16) feet from the southwest to northeast property corners. Subsurface The site was explored by excavating nine test pits at the locations shown on Plate 2. Please re.Eer to the test. pit logs, Plates 4 thXough 8, for a detailed iiescription of the conditions encountered at-each location explored. A de�cription of the field exploration methods and laboratory testing pr.ogram is included in this report following the Discussion ancl Recomnendations section. The test pits disclosed a uniform subsurface profile across the site. Generally four (4) to twelve (12) inches of organic topsoil was found covering the site over loose silty sand with gravel. The silty oand becomes dense to very dense at two to tnree feet below the surface. The soil ie qlacially deposited and coneolidated with the upper loose zone being the weathered horizon. EaAh Consuhants, Inc.