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Intracorp E-3592-520 <br />_ September 23, 1998 Page 2 <br />SITE CONDITIONS <br />Surface <br />The subject lot is located immediately south of Merrill Creek Parkway in an undeveloped <br />portion of Seaway Tract 1, Lot 5. The site is bordered to the east and west by asphalt paved <br />access roads that extend to existing commercial buildings, to the north by Merrill Creek <br />Parkway, and to the south by south and east facing slopes. <br />The proposed building area is essentially flat, with a maximum elevation change of <br />approximately five feet. The existing site grades were cut at least five feet to attain existing <br />grade. Along the eastern and southern perimeter of the site is a thirty (30) to seventy (70) <br />foot high descending slope. The slopes range from 2H:1 V(Horizontal:Vertical) to 1.5H:1 V. <br />The 2H:1 V slopes were cut during gravel mining operations. The 1.5H:1 V slopes were also <br />cut during mass grading of the Seaway project in 1996. At the toe of the s{ope is an asphalt <br />paved access road. <br />The site is vegetated with grass and brush. <br />Subsurface <br />Subsurface conditions were evaluated by excavating four test pits at the approximate <br />locations shown on Plate 2. Please refer to the Test Pit Logs, Plates A2 through A5, for a <br />more detailed description of the conditions encountered at each test pit location. A <br />description of the field exploration methods is included in Appendix A. The following is a <br />generalized description of the subsurface conditions encountered. <br />At our test pit locations, we typically encountered a one to two foot thick layer of inedium <br />dense to dense fill comprised of silty sand with gravel. The observed fill appears to have been <br />derived from on-site materials or from material removed from earlier phases of the Seaway <br />development. The fill was similar to the underlying native soil, but appeared to be disturbed. <br />It was most likely placed after the major excavation of the site took place. <br />The underlying native soils were comprised of inedium dense to dense, interbedded sequences <br />of poorly graded gravel with silt and sand, poorly graded sand with sift and gravel, poorly <br />graded sand with gravel, silty gravel and silty sand (Unified Soil Classifications GP-GM, <br />SP-SM, SP, GM and SM, respectively). The observed soils typically consisted of gradational <br />sequences from coarse grained material at the top of the excavation to finer grained soils <br />toward the bottom. <br />Earth Consultents, Inc. <br />