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Page 2 1% <br /> Jim Monroe <br /> Patterson Pass Business Park <br /> The Patterson Run drainage bisects the site, flowing from under the California Aqueduct <br /> northeast to the Delta Mendota Canal. Drainage A flows northeast from the California <br /> Aqueduct, and is an existing State of California Drainage Easement. Drainage B also flows <br /> northeast from the California Aqueduct to a pond. Area C is located to the nest of Patterson <br /> Run. All potential jurisdictional wetlands and waters are indicated on the four U.S. Army <br /> Corps of Engineers Potential Jurisdictional Wetlands and Waters of the.U.S maps. <br /> METHODS <br /> Wetlands were delineated using the "Corps of Engineers Wetlands Delineation Manual" <br /> (Environmental Latx-)ratory 1987 with updates). A total of twenty data points were utilized to <br /> dete-m,ine the extent and location of the upland/wctland boundaries. At each data point, <br /> information was collected about vegetation, soils and hydrology. The dominant and sub- <br /> domirant plant species were identified and their relative percentage cover was determined. <br /> Soil pits -,vere excavated at each data point to an average depth of twelve inches to <br /> characterize the potential extent of hydric soils and presence of wetland hydrology at each <br /> location. <br /> Wetland hydrology criterion is usually satisfied if the soil was saturated or inundated within a <br /> major portion ofthe root zone for more than 5% (18 or more days) of the growing season. In <br /> this case, the growing season would be the frost free period, which at this location is year <br /> round. Field indicators used to identify hydrology include wetland topography, drainage <br /> patterns, drift lines, sediment .deposits on plants and other objects, water marks, visual <br /> observation of soil saturation or inundation, oxidized rhizospheres, and other indicators. <br /> Wetland soil criterion are satisfied if soils have low chroma, exhibit gleyed colors, or have <br /> concretions or mottles. According to the San Joaquin County soil classification map, the <br /> study area consists of one soil type: Cm-Rn-Capay-Rossi Waukena D, characterized as clay <br /> soils with low infiltration rates, permanent water table, soils with a claypan or clay laver at or <br /> near the surface, and shallow soils over nearly impervious material. <br /> Wetland vegetation criterion is satisfied if the plants identified at the data point location are <br /> classified as Obligate (OBL), Facultative-Wetland (FACW), or Facultative (FAC) wetland <br /> plant species as listed in the National List of Plant Species that Occur in Wetlands: California <br /> (Region O)U.S. Fish and Wildlife Service. <br /> A. section of Patterson Run was delineated on November 21, 1997. A total of eighteen data <br /> points were utilized to determine the extent and location of the upland/wetland boundary. <br /> This area was delineated separately to characterize the extent of the low-lying "flood plain" <br /> area south of Patterson Run, at the northeast end of the drainage. At this location the <br /> boundaries of the wetland drainage and adjacent upland area is not clearly.defined. <br /> RMI <br /> R LCOL ACL NJAc 4 1.1 NL %T <br /> I\ ILA.1 A T 10 Al • I \C. <br />