Laserfiche WebLink
Page 3 <br />1696-16 <br />Our review of historic aerial photographs (1949 black-and-white, USDA series GS -JL aerial <br />photographs 2-57, 2-58, 2-74, 2-75) confirms the presence of a landslide complex. Although a <br />Terraseach, Inc. California Certified Engineering Geologist examined two stereo pairs of aerial <br />photographs to evaluate the presence or absence of landsliding on the subject property (page 8), the <br />photos used in the examination are not provided. Information on the vintage and scale of the aerial <br />photographs exanuned also is not presented in the report. It is customary, standard of practice, to <br />provide this information with the cited references. More importantly, the location of the landslide <br />mapped by Nilsen should be shown on the site geologic map and positive evidence for the presence or <br />absence of landsliding should be presented. <br />Our field examination of the site identified a broad swale along the southeastern margin of the <br />property, roughly coincident with the margin of the larger landslide mapped by Nilsen. A stock pond <br />is located at the head of the swale, upslope of the proposed limit of grading for Lot 6. The source of <br />the water for the stock pond is not apparent and may be a spring. Because uncontrolled water seepage <br />or flow is one of the major causes of soil movement, it is important that the source of the water be <br />identified. No information is provided in the report on what will be done with the stock pond and <br />possible water seepage uphill of Lot 6. The presence or absence of a landslide margin, colluvial- <br />related slope creep, and/or seepage from a spring in the vicinity of Lot 6 should be addressed. We <br />recommend that the source of the water in the stock pond be identified, any seepage controlled by <br />adequate drainage, and the colluvial swale be cleaned to a firm soil or rock base prior to placement of <br />fill. <br />Subsurface exploration studies on the adjacent Heinz property indicates the large landslide feature is <br />likely much smaller than the outline shown by Nilsen. However, Terrasearch should confum that this <br />feature does not exist on the Sarich parcel by supplemental subsurface exploration. In addition, the <br />smaller landslide feature should also be evaluated unless it is concluded it is an active feature. <br />Appropriate, specific mitigation measures should be recommended for identified concerns, including <br />seepage in the vicinity of proposed Lot 6. <br />2. Estate lot cut slope -Proposed grading for the hilltop estate lot consists of a significant cut up to 40 <br />feet high. As stated on page 17 of the report, "the subsurface material that will form the SO foot cut <br />slope planned for the estate lot is not known, but is anticipated to be Livermore Gravel bedrock <br />material and the cut slope is expected to be preliminarily stable at an inclination of 2.75:1. This will <br />be confirmed during grading or prior to grading when access for a drill rig is available" (emphasis <br />added). Elsewhere grading is described as consisting of "cuts to 40 feet at the estate lot" (page 6) and, <br />based on our examination of the preliminary grading plans, we believe that the proposed cut slope <br />will be about 40 feet high. However, we believe that more information is necessary on the height and <br />possible stability of the proposed cut slope. In particular, we are concerned about the absence of <br />information on the dip of bedding in the vicinity of the proposed estate development. Our concern is <br />that the Livermore gravels are mapped (Barlock, 1988; Majmundar, 1991) with a gentle (2-28 <br />degrees) northeasterly dip, roughly slope parallel. No subsurface information is provided for the <br />proposed estate lot although an additional boring is proposed at a later time. <br />More subsurface information is required for adequate characterization of the estate lot and the height <br />and possible stability of the proposed cut slope. We recommend that the bedding orientation within <br />the Livermore Gravel (assuming that bedrock at the estate site is Livermore Gravel) be more fully <br />characterized and that a boring be completed at the site to a depth greater than the proposed cut prior <br />to final grading design. <br />sa t_ ~~ y ~< ~ ~ ~ ~ <br />x .,.~~,~~,.,~ Wis. ,~~;c. <br />