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<br />whether soil meets the physical and chemical criteria for Prime rarmland or Farmland of Statewide <br />Importance. Fannlands arc further discussed under Agriculture and Grazing below. <br /> <br />Soil Types for Groundwater Recharre <br />'!1,e majority of groundwater recharge derives from stream recha'l~e through gravelly streambeds <br />across the valley floor. Zone 7 recharges groundwater by releasing water into streambeds with high <br />percolation rates and in Lake I of the Chain of L~ke with its gravelly western shore. <br /> <br />Soil Supports Stmctures <br />Buildings need stable soils for support. DurinI' seismic activity. some soil types are not as capable of <br />supporting stmctures as other soil types. <br /> <br />Ground motions during earthcluakes arc related mainly to local soil conditions. Local soil conditions <br /> <br />and subsurface geologic characteristics arc two of the six major components - including magnitude <br /> <br />and distance - related to structural damage from an earthquake. In addition. where loose granular <br /> <br />sands arc present. soils tend to compact resulting in soillicjuefaction and settlement. 9 <br /> <br />Landslides and soil erosion arc also related to surface and subsurface soil characteristics. Soil type is <br /> <br />just one of numerous factors that contribute to landslides including slope steepness. aspect'" rainfall. <br /> <br />rock type. land use. distance (roln fault. distance [tOOl water sources and vegetative cover. See the <br /> <br />Public Safety Element for a discussion of geologic hazards alonv with l'oals policies and programs <br /> <br />related to geologic safety. <br /> <br />Water Resources II Croundwatef <br /> <br />Pleasanton lies within the Alameda Creek watershed, a drainage basin encompassing about 675 s'luare <br /> <br />miles between Mount Hamilton and Mount Diablo. Alameda Creek, the principal stream, flows from <br /> <br /> <br />its origin on Mount IIamilton until it meets the Arroyo de la l.aguna near Sunol and then nllls west <br /> <br />through Niles Canyon to San rrancisco Bay. 'lbe Arroyo de la Laguna collects the surface water <br /> <br />mnoff from the ,\rn"tlor Li, ElI..ore Tt1 Valley and carries it south to Alameda Creek. 11,e General <br /> <br />Plan Map designates these creeks along with other areas as Public Health and Safety with a Wildlands <br /> <br /> <br />Overlay <br /> <br />Although all of the creeks feeding the Arroyo de la Laguna arc naturally seasonal, Zone 7 of the <br /> <br />Alameda County Flood Control and \Vater Conservation District releases controlled amountj of both <br /> <br />stored water from the Del Valle Reservoir and imported water from the South Bay Allueduct into <br /> <br />') Seed, H. Bolton, Department of Civil Engineering, University of California, Berkeley and I.M. ldriss, \Voouward-Clyde <br />Consultants, Ground Ala/iolls anti Soil Liquefacliol1 J)urin~~ Earthquakes, Earthquake Engineering Institute, Berkeley, <br />California, 1982. <br /> <br />In Aspect of a slope is exposure to a particular direction. <br />11 Zone 7 Water Agency, Stream Almlagemm/ Alaster Pkm, March 2006. <br /> <br />Con os Ekmcnl, CC 082906, redlinc <br /> <br />VII-9 <br />