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CO0052918
Environmental Health - Public
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CO0052918
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Entry Properties
Last modified
7/14/2022 10:51:25 AM
Creation date
3/5/2021 10:16:14 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
RECORD_ID
CO0052918
PE
2900
STREET_NUMBER
0
STREET_NAME
WALNUT GROVE
City
WALNUT GROVE
ENTERED_DATE
11/4/2020 12:00:00 AM
SITE_LOCATION
WALNUT GROVE & OTHERS
RECEIVED_DATE
11/4/2020 12:00:00 AM
P_LOCATION
99
QC Status
Approved
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<br />Soil Investigations for Data Collection in the Delta <br />Initial Study/Proposed Mitigated Negative Declaration 90 <br />HYD-1 and MM HAZ-1 through 4 would reduce potential impacts to Sacramento <br />Splittail to: Less than Significant with Mitigation Incorporated. <br />Longfin Smelt (Spirinchus thaleichthys) <br />The Bay-Delta population of Longfin Smelt is designated as a candidate for <br />listing under the FESA (USFWS 2012) and, since June 26, 2009, the Longfin <br />Smelt is listed as threatened under the CESA. <br />Longfin Smelt are anadromous and semelparous, moving from saline to brackish <br />or freshwater for spawning from November to May (Moyle 2002; Rosenfield and <br />Baxter 2007) Longfin Smelt usually live for 2 years, spawn, and then die <br />(Rosenfield 2010). Peak spawning takes place in January and February of most <br />years and appears to be centered in brackish water (1–8 ppt); their habitat <br />typically extends from San Pablo Bay to the confluence of the Sacramento River <br />and San Joaquin River. Newly hatched Longfin Smelt larvae are planktonic and <br />probably do not control their position in the water column before they develop an <br />air bladder. Once their air bladder is developed (~12 mm standard length) they <br />are capable of controlling their position in the water column by undergoing <br />reverse diel vertical migrations, which allows them to maintain position on the <br />axis of the estuary (Bennett et al. 2002). <br />The geographic distribution of larval and early juvenile life stages of Longfin <br />Smelt may be influenced by freshwater inflows to the Delta during late winter and <br />spring, although the mechanisms are complicated and not fully understood (Hieb <br />and Baxter 1993; Baxter 1999; Dege and Brown 2004). Juvenile Longfin smelt <br />move seaward, mostly west of Carquinez Bridge, by late summer and fall. <br />Rosenfield and Baxter (2007) suggest that juvenile Longfin Smelt seek cooler <br />and deeper water in the summer months. <br />Overall, designated in-water work windows would reduce exposure of sensitive <br />fish species, including Longfin smelt and life stages to in-water work activities. <br />The activities of the Proposed Project would be minor in scope and would not <br />result in degradation of aquatic habitat or water quality conditions and any <br />potential effects related to potential increase in suspended sediment <br />concentrations and contaminants due to disturbance of the river bed would be <br />negligible. Implementation of Mitigation Measures MM BIO-14, along with MM <br />HYD-1 and MM HAZ-1 through 4 would reduce potential impacts to Longfin <br />Smelt to: Less than Significant with Mitigation Incorporated. <br />Western Red Bat (Lasiurus blossevillii) <br />Western red bat is identified as a CDFW Species of Special Concern. It is a <br />medium bat with mottled reddish grayish pelage but can range from bright <br />orange to yellow-brown, and short rounded ears. This species is locally common <br />in some areas of California, occurring from Shasta County to the Mexico border, <br />west of the Sierra Nevada/Cascade crest and deserts. Their winter range <br />includes western lowlands and coastal regions south of San Francisco Bay.
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