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06 16 20 PWA_02_02 Exh2 - IS-MND
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75B - FAIRVIEW BRIDGE PROJECT CD
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06 16 20 PWA_02_02 Exh2 - IS-MND
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INITIAL STUDY/MITIGATED NEGATIVE DECLARATION FAIRVIEw BRIDGE REPLACEMENT AND STREET IMPROVEMENTS w <br />MAY 2020 (9TH STREET TO 16TH STREET) PROJECT <br />J" <br />SANTA ANA. CALIFORNIA <br />streams. These deposits accumulated along river and stream channels as floods and debris flows <br />carried sediment down from higher elevations. The size, color, and types of clasts in these deposits <br />are dependent on the local bedrock from which they were derived, with boulder -size clasts more <br />common closer to the mountains and in areas prone to flash floods. These deposits are mapped <br />along the Santa Ana River channel in the Project area. Although Holocene deposits can contain <br />remains of plants and animals, only those from the middle to early Holocene (4,200 to 11,700 years <br />ago) are considered scientifically important. Older deposits that may contain scientifically important <br />fossils may be encountered at undetermined depths below these late Holocene deposits. Therefore, <br />the Very Young Wash Deposits are considered to have low paleontological sensitivity. <br />Young Alluvial Fan Deposits, which are Holocene to late Pleistocene in age (less than 126,000 years <br />ago), consist of unconsolidated gravel, sand, and silt with occasional cobbles and boulders near <br />mountain fronts. These sediments were deposited by flooding streams and debris flows coming <br />down from higher elevations and generally form a fan or lobe shape at the base of hills and <br />mountains. As noted above, only fossils from the middle to early Holocene (4,200 to 11,700 years <br />ago) are considered scientifically important. These Holocene deposits overlie older Pleistocene <br />deposits, which have produced scientifically important fossils elsewhere in the region. These older <br />deposits span the end of the Rancholabrean North American Land Mammal Age (NALMA), which <br />dates from 11,000 to 240,000 years ago and was named for the Rancho La Brea fossil site in central <br />Los Angeles. The presence of Bison defines the beginning of the Rancholabrean NALMA, but fossils <br />from this time also include other large and small mammals, reptiles, fish, invertebrates, and plants. <br />There is a potential to find these types of fossils in the older sediments of this geologic unit, which <br />may be encountered below a depth of approximately 10 ft. Therefore, these deposits are assigned <br />low paleontological sensitivity from the surface to a depth of 10 ft and high sensitivity below that <br />mark. <br />According to the locality search conducted by the LACM, there are no known fossil localities within <br />the boundaries of the proposed Project. The LACM reports that the Project area is underlain by <br />deposits of younger Quaternary alluvium overlying older Quaternary alluvium (i.e., Young Alluvial <br />Fan Deposits). The museum notes that these deposits typically do not contain scientifically <br />significant fossils in the uppermost layers however; they may produce important fossils at depth. <br />The closest vertebrate locality in these older Quaternary deposits is LACM 1339, south-southwest of <br />the Project area near the top of the bluffs along Adams Avenue in Costa Mesa. This locality <br />produced a specimen of horse (Equus) at a depth of 43 feet below the street. The next closest <br />locality is LACM 2032, northeast of the Project area near the intersection of Mission Road and Daly <br />Street. That locality yielded specimens of mammoth (Mammuthus) and camel (Camelidae) at a <br />depth of 15 ft below the top of the bluff. Locality LACM 4943, which is located northeast of the <br />Project area near the intersection of Glassell Street and Fletcher Avenue in Orange, produced a <br />specimen of horse (Equus) at a depth of 8 to 10 ft below the surface. <br />The LACM believes that shallow excavations in the Young Alluvial Fan Deposits in the Project area <br />are unlikely to encounter any scientifically important vertebrate fossils. However, the museum notes <br />that deeper excavations into these deposits may encounter scientifically significant vertebrate <br />remains and should be monitored to recover those remains. A copy of the letter describing the <br />locality search results from the LACM is provided in Appendix A. <br />R:\WKE1702\ISMND\Final ISMND\Fairview Street Bridge Final ISMND.docx (05/26/20) 3-39 <br />
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