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3A Public Hearing 2006 1204
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3A Public Hearing 2006 1204
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5/10/2007 11:34:50 AM
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12/1/2006 10:50:58 AM
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CM City Clerk-City Council
CM City Clerk-City Council - Document Type
Staff Report
Document Date (6)
12/4/2006
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_CC Agenda 2006 1204
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Path:
\City Clerk\City Council\Agenda Packets\2006\Packet 2006 1204
MO 2006-044
(Reference)
Path:
\City Clerk\City Council\Minute Orders\2006
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<br />GEOTECNIA <br />Project Number: 060805 <br />2888 Darius Way, San Leandro <br />October 27,2006 <br /> <br />Page 5 <br /> <br />were encountered in the three borings drilled for this study. The potentials for landsliding, fault <br />rupture, and seismic shaking are discussed below. <br /> <br />Landsliding <br /> <br />As part of our study, we reviewed the soil and geologic investigation report for the subdivision <br />(Terrasearch, Inc., 1989) and published landslide maps of the site vicinity (Nilsen, 1975a and <br />1 975b ). These references do not show the presence of mapped landslides or colluvial soils at the <br />site. During our site reconnaissance, w9~id~ot observe evidence of deep-seated, active slo~ <br />instability at the site. Based on the above. discussion, it is our opinion that the potential for deep- <br />seated landsliding at the site is low provided the recommendations in this report are <br />implemented. <br /> <br />Fault Rupture <br /> <br />The subject property does not lie within the Alquist-Priolo Earthquake Fault Zone associated <br />with the Type-A Hayward Fault. No active faults are shown crossing the site on reviewed <br />published maps, nor did we observe evidence of fault rupture during our study. Therefore, we <br />conclude that the potential risk for damage to the planned improvements at the site due to surface <br />rupture from faults is low. <br /> <br />Seismic Shaking <br /> <br />Earthquake shaking results from the sudden release of seismic energy during displacement along <br />a fault. During an earthquake, the intensity of ground shaking at a particular location depends on <br />a number of factors including the earthquake magnitude, the distance to the zone of energy <br />release, and local geologic conditions. We expect that the site may be exposed to strong <br />earthquake shaking during the life of the improvements since the site is only about y,. mile from a <br />Type-A fault. Lateral loads should be estimated in accordance with the currently enforced <br />building code based on the seismic parameters recommended below. <br /> <br />RECOMMENDATIONS <br /> <br />General <br /> <br />As discussed above, we recommend that drilled-pier-and-grade-beam foundations be used for the <br />majority of the planned structures at the site (main house, carriage house, pool house, and <br />retaining walls), except that shallow footings may be used in excavated areas in the bedrock at <br />least 10 feet from slopes. Detailed recommendations are provided below for drilled piers and <br />shallow footings. <br /> <br />In addition, the recommendations contained in the latest adopted edition of the UBC should be <br />followed for reducing potential damage to the structures from earthquake shaking. <br />
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