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indicated possible boundaries of a large block slide. The overlay was <br />prepared by Bissell & Karn and shows the boundaries running through lots <br />3, 4, 5, 6 and 7 and going out of the proposed project. He stated borings <br />were done by Gribaldo et al. He then showed this in his overlay for the <br />Commission to see. The Moore and Tabor report indicated that should there <br />be any movement it would be on the boundary lines. He stated borings <br />shown on the overlay are not necessarily to scale but placed in an area <br />where homes are currently built. He stated that the site specific reports <br />have already been done (by somebody) -- He doesn't see any reason to do <br />more prior to filing a tentative map. Mr. Maines said he asked for soils <br />reports from the staff and individual property owners for lots 4, 5, 6, 7, <br />8 and 9. He said he received reports for lots 6 and 8 from the City and <br />for lot 7 from Mr. McGovern, the owner of that lot. He said the sites <br />are buildable according to all reports. He stated that on lot 6, there <br />were three borings done by Dunnam. & Associates. He stated this ties <br />into the Moore and Tabor geological report. He then read from the report. <br />He stated on lot 7 the borings done encountered shale - 50-1". This indi- <br />cated firm bedrock. Mr. Maines stated William Widdington, president of <br />Engio Geologists and Don Bissell, of Bissell and Karn are present to <br />answer any questions. <br />Pat Jennings, a Longview Drive resident, inquired as to who owns lot 6? <br />Dr. Long responded that Bruce Sasak owned the property. <br />Mr. Widdington then addressed the Planning Commission stating he is a <br />certified geologist and is prepared to answer any questions concerning the <br />ridge. Commissioner Leppert asked Mr. Widdington to describe a block slide. <br />He responded by saying it is something which moves in one piece. He <br />stated that Burkland maintains this slide to be 5 miles long and several <br />thousand feet wide. Commissioner Geppert asked Mr. Widdington how thick <br />this slide would be. Mr. Widdington responded it would be 100-200 feet. <br />Commissioner Geppert then asked if there was a movement, would the soil <br />break up? Mr. Widdington responded it would move as one piece unless you <br />address a 500 ft. movement. He then cited the Alaska movement of one-half <br />mile. Commissioner Geppert asked if it is the nature of a landslide to <br />move at a rapid rate? Mr. Widdington then explained the slide in Alaska <br />as moving one-half mile in distance and these slides moved in blocks. He <br />stated that if there was a slide in 100-200 ft. in solid bedrock he would <br />not expect it to break up. <br />Mr. Widdington stated that from 1769 to the present time he couldn't find <br />any record of movement on the Pleasanton Ridge. He stated the U.C. <br />Berkeley maps of 1906 didn't show any changes in the contours. 1861 <br />records show ground movement doesn't exist. At the time of the Calaveras <br />quake, 1769, there was no movement. <br />Mr. Widdington stated this situation is similar to the Vallecitos situation <br />with regard to extensive trenching and various geologists not arriving at <br />any conclusions. He stated he doesn't feel that the geologists have taken <br />conflicting positions when it comes to building this property. He stated <br />that Moore and Tabor are cautious but no one has said it is unbuildable. <br />Commissioner Wilson read from the Moore and Tabor Report and said he <br />doesn't understand what it means -- "no known methods to evaluate the <br />ancient slides." Mr. Widdington stated there are known methods, but <br />it would take 10 years. <br />-8- <br />