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Geologic Map of the Long Valley Caldera, Mono-Inyo Craters
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-1933 US. GEOLOGICAL SURVEY GEOLOGIC MAP OF LONG VALLEY CALDERA, MONO-INYO CRATERS VOLCANIC CHAIN, AND VICINITY, EASTERN CALIFORNIA By Roy A. Bailey GEOLOGIC SETTING VOLCANISM Long Valley caldera and the Mono-Inyo Craters Long Valley caldera volcanic chain compose a late Tertiary to Quaternary Volcanism in the Long Valley area (Bailey and others, volcanic complex on the west edge of the Basin and 1976; Bailey, 1982b) began about 3.6 Ma with Range Province at the base of the Sierra Nevada frontal widespread eruption of trachybasaltic-trachyandesitic fault escarpment. The caldera, an east-west-elongate, lavas on a moderately well dissected upland surface oval depression 17 by 32 km, is located just northwest (Huber, 1981).Erosional remnants of these mafic lavas of the northern end of the Owens Valley rift and forms are scattered over a 4,000-km2 area extending from the a reentrant or offset in the Sierran escarpment, Adobe Hills (5-10 km notheast of the map area), commonly referred to as the "Mammoth embayment.'? around the periphery of Long Valley caldera, and The Mono-Inyo Craters volcanic chain forms a north- southwestward into the High Sierra. Although these trending zone of volcanic vents extending 45 km from lavas never formed a continuous cover over this region, the west moat of the caldera to Mono Lake. The their wide distribution suggests an extensive mantle prevolcanic basement in the area is mainly Mesozoic source for these initial mafic eruptions. Between 3.0 granitic rock of the Sierra Nevada batholith and and 2.5 Ma quartz-latite domes and flows erupted near Paleozoic metasedimentary and Mesozoic metavolcanic the north and northwest rims of the present caldera, at rocks of the Mount Morrisen, Gull Lake, and Ritter and near Bald Mountain and on San Joaquin Ridge Range roof pendants (map A). -
Santa Ana Sucker Habitat, Santa Ana River
Santa Ana succker (Catostomus santaanae) 5-Year Review: Summary and Evaluation Santa Ana sucker habitat, Santa Ana River. Photo credit Christine Medak (USFWS). U.S. Fish and Wildliffee Service Carlsbad Fish and Wildlife Office Carlsbad, CA March 10, 2011 2011 5-Year Review for Santa Ana sucker 5-YEAR REVIEW Santa Ana sucker (Catostomus santaanae) I. GENERAL INFORMATION Purpose of 5-Year Reviews: The U.S. Fish and Wildlife Service (Service) is required by section 4(c)(2) of the Endangered Species Act (Act) to conduct a status review of each listed species at least once every 5 years. The purpose of a 5-year review is to evaluate whether or not the species’ status has changed since it was listed. Based on the 5-year review, we recommend whether the species should be removed from the list of endangered and threatened species, be changed in status from endangered to threatened, or be changed in status from threatened to endangered. Our original listing of a species as endangered or threatened is based on the existence of threats attributable to one or more of the five threat factors described in section 4(a)(1) of the Act, and we must consider these same five factors in any subsequent consideration of reclassification or delisting of a species. In the 5-year review, we consider the best available scientific and commercial data on the species, and focus on new information available since the species was listed or last reviewed. If we recommend a change in listing status based on the results of the 5-year review, we must propose to do so through a separate rule-making process defined in the Act that includes public review and comment. -
Bailey-1976.Pdf
VOL. 81, NO. 5 JOURNAL OF GEOPHYSICAL RESEARCH FEBRUARY 10, 1976 Volcanism, Structure,and Geochronologyof Long Valley Caldera, Mono County, California RoY A. BAILEY U.S. GeologicalSurvey, Reston, Virginia 22092 G. BRENT DALRYMPLE AND MARVIN A. LANPHERE U.S. GeologicalSurvey, Menlo Park, California 94025 Long Valley caldera, a 17- by 32-km elliptical depressionon the east front of the Sierra Nevada, formed 0.7 m.y. ago during eruption of the Bishoptuff. Subsequentintracaldera volcanism included eruption of (1) aphyric rhyolite 0.68-0.64 m.y. ago during resurgentdoming of the caldera floor, (2) porphyritic hornblende-biotiterhyolite from centersperipheral to the resurgentdome at 0.5, 0.3, and 0.1 m.y. ago, and (3) porphyritic hornblende-biotiterhyodacite from outer ring fractures0.2 m.y. ago to 50,000 yr ago, a sequencethat apparently records progressivecrystallization of a subjacentchemically zoned magma chamber. Holocene rhyolitic and phreatic eruptions suggestthat residual magma was present in the chamber as recentlyas 450 yr ago. Intracaldera hydrothermalactivity beganat least0.3 m.y. ago and was widespreadin the caldera moat; it has sincedeclined due to self-sealingof near-surfacecaldera sediments by zeolitization, argillization, and silicificationand has becomelocalized on recentlyreactivated north- west-trendingSierra Nevada frontal faults that tap hot water at depth. INTRODUCTION concentrates were treated with a dilute HF solution to remove small bits of attached glassand fragments of other mineral In the westernUnited States,only three calderasare known grains. Obsidian used for dating was totally unhydrated and to be large enoughand young enoughto possiblystill contain not devitrified. Small blocks sawed from many of the hand residual magma in their chambers:the Vailes caldera (•1.1 specimenswere used for dating. -
Target Species Mapping for the Green Visions Plan
Target Species Habitat Mapping California Quail and Mountain Quail (Callipepla californica and Oreortyx pictus) Family: Phasianidae Order: Galliformes Class: Aves WHR #: B140 and B141 Distribution: California quail are found in southern Oregon, northern Nevada, California, and Baja California, and have been introduced in other states such as Hawaii, Washington, Idaho, Colorado, and Utah (Peterson 1961). In California, they are widespread but absent from the higher elevations of the Sierra Nevada, the Cascades, the White Mountains, and the Warner Mountains, and are replaced by the related Gambel’s quail (C. gambelii) in some desert regions (Peterson 1961, Small 1994). In southern California, they are found from the Coast Range south to the Mexican border, and occur as far east as the western fringes of the Mojave and Sonoran deserts, such as in the Antelope Valley (Garrett and Dunn 1981, Small 1994). California quail range from sea level to about 5000 ft (1524 meters; Stephenson and Calcarone 1999) Mountain quail are resident from northern Washington and northern Idaho, south through parts of Oregon, northwestern Nevada, California, and northern Baja California (Peterson 1961). In southern California, mountain quail are found in nearly all of the mountain ranges west of the deserts, including the southern Coast Ranges, from the Santa Lucia Mountains south through Santa Barbara and Ventura counties, and the Peninsular Ranges south to the Mexican border (Garrot and Dunn 1981, Small 1994). In the Transverse Ranges, a small population occurs in the western Santa Monica Mountains, and larger populations occur in the San Gabriel and San Bernardino Mountains (Small 1994). Mountain quail are found at elevations from below 2000 ft (610 meters) to over 9000 ft (2743 meters; Stephenson and Calcarone 1999). -
Doing Zooarchaeology As If It Mattered: Use of Faunal Data To
In, Zooarchaeoloqy and Conseryation Biology 2004, R. Lee Lyman and Kenneth P. Cannon,-eds. pp. 25-44, The University of Utah Press, Salt Lake City. 2 Doing Zooarchaeologyas if It Mattered: Use of Faunal Data to AddressCurrent Issuesin Fish ConservationBiology in OwensValley, California VIRGINIA L. BUTLERAND MICHAEL G. DELACORTE "V cologists are increasingly incorporating conceptssuch as "legacy" into l::Jtheir explanations of current ecosystems(Harding et al. 1:998). This approach acknowledges that understanding the structure and function of extant ecosystems(or predicting future responsesto climate change)re- quires knowledge of historical forces that have beenoperating for decades, centuries, or longer (Foster 2.000;Moorhead et al. 1:999).Indeed, recog- nition of the needfor such long-term historical records is demonstratedby the level of National ScienceFoundation funding for the Long-Term Eco- logical Research(LTER) network (Kaiser 2.oo1:b;LTER Network 2.001:). Over 1:,1:00researcqers funded by the LTER carry out researchon 2..4des- ignated sites that have been studied;from a few years to several decades (Kaiser 2.O01:b).These studies cover a range of topics with the overall goal of "investigating ecological processesover long temporal and broad spa- tial scales" (LTER Network 2.001:).This goal is precisely that of zoo- archaeology.Yet, to our knowledge, zooarchaeologicalexpertise and data have not been incorporated into the LTER network. Our point is simply I that ecological sciencesseeking to understand the long-term properties of ecosystemshave direct accessto such information through zooarchaeology. Zooarchaeology needsto tollaborate with wildlife sciencesbecause of the increasing speedwith which habitats and biotas are being lost in the face of human population growth and habitat destruction (Minckley and Deacon 1:991:;Vitousek et al. -
Chapter 06 Fisheries & Aquatic Resources.Pdf
CHAPTER 6 Fisheries and Aquatic Resources CHAPTER 6 FISHERIES AND AQUATIC RESOURCES This chapter describes the existing fisheries and aquatic resources conditions, the applicable regulations, and potential impacts from implementation of the Proposed Project Alternative and other alternatives on the fisheries and aquatic resources in the Project Area. 6.1 ENVIRONMENTAL SETTING This section describes the environmental setting related to fisheries and aquatic resources that may be influenced by implementation of the Proposed Project Alternative or other alternatives in the Project Area including Lake Mary, Mammoth Creek extending from Lake Mary to its confluence with Hot Creek, and Hot Creek from its confluence with Mammoth Creek downstream to the USGS Hot Creek Flume Gage. 6.1.1 LAKE MARY Lake Mary is a cirque lake (a deep, steep-walled basin on a mountain) formed by the filling of remnant moraine depressions left by receding glaciers (USGS 1999). Lake Mary contains prominent granite features, and cold, clear water, making it a popular angling destination. A "fishing enhancement" program is implemented by both the Town of Mammoth Lakes and CDFG to maintain the lake’s appeal as a “trophy” trout destination. The recreational fishery in Lake Mary is maintained by both the Town of Mammoth Lakes and CDFG because of its economic importance to the Mammoth Lakes Basin (Mammoth City Concierge 2010). Lake Mary has been, and continues to be managed as a put-and-take recreational fishery. Hatchery rainbow trout have been regularly planted by CDFG beginning in the late spring and extending through the summer. The lake also is often planted with “Alpers trout.” The Alpers trout is a genetic hybrid of rainbow trout, Kamloops trout and steelhead, raised in the streams and ponds of Alpers Owens River Ranch. -
Development of a Groundwater Flow Model for the Bishop/Laws Area
DEVELOPMENT OF A GROUNDWATER FLOW MODEL FOR THE BISHOP/LAWS AREA FINAL REPORT FOR LOCAL GROUNDWATER ASSISTANCE GRANT AGREEMENT NO. 4600004129 Robert Harrington, PhD, R.G. INYO COUNTY WATER DEPARTMENT APRIL, 2007 TABLE OF CONTENTS EXECUTIVE SUMMARY ………………………………………. 3 INTRODUCTION ………………………………………………. 5 CONCEPTUAL MODEL ………………………………………… 8 SIMULATION MODEL …………………………………………. 5 PREDICTIVE SIMULATIONS …………………………………. 23 SUMMARY AND CONCLUSIONS ……………………………. 26 REFERENCES …………………………………………………… 28 APPENDIX 1 ……………………………………………………. 51 APPENDIX 2 ……………………………………………………. 54 LIST OF FIGURES Figure 1. Study area location……………………………………………… 30 Figure 2. Geology…………………………………………………………. 31 Figure 3. Hydraulic conductivity distribution…………………………….. 32 Figure 4. Aquifer test locations…………………………………………… 33 Figure 5. Well locations…………………………………………………... 34 Figure 6. Layer 1 hydraulic conductivity zones…………………………... 35 Figure 7. Layer 2 hydraulic conductivity zones………………………….. 36 Figure 8. Layer 3 hydraulic conductivity zones…………………………. 37 Figure 9. Layer 4 hydraulic conductivity zones…………………………. 38 Figure 10. Layer 5 hydraulic conductivity zones………………………… 39 Figure 11. Quaternary faults and horizontal flow barriers………………. 40 Figure 12. Recharge zones……………………………………………….. 41 Figure 13. Evapotranspiration zones……………………………………… 42 Figure 14. Boundary conditions………………………………………….. 43 Figure 15. Observed vs. residuals………………………………………… 44 Figure 16. Distribution of residuals………………………………………. 45 Figure 17. Spatial distribution of residuals………………………………. 46 Figure 18. Drawdown -
Microsoft Outlook
Joey Steil From: Leslie Jordan <[email protected]> Sent: Tuesday, September 25, 2018 1:13 PM To: Angela Ruberto Subject: Potential Environmental Beneficial Users of Surface Water in Your GSA Attachments: Paso Basin - County of San Luis Obispo Groundwater Sustainabilit_detail.xls; Field_Descriptions.xlsx; Freshwater_Species_Data_Sources.xls; FW_Paper_PLOSONE.pdf; FW_Paper_PLOSONE_S1.pdf; FW_Paper_PLOSONE_S2.pdf; FW_Paper_PLOSONE_S3.pdf; FW_Paper_PLOSONE_S4.pdf CALIFORNIA WATER | GROUNDWATER To: GSAs We write to provide a starting point for addressing environmental beneficial users of surface water, as required under the Sustainable Groundwater Management Act (SGMA). SGMA seeks to achieve sustainability, which is defined as the absence of several undesirable results, including “depletions of interconnected surface water that have significant and unreasonable adverse impacts on beneficial users of surface water” (Water Code §10721). The Nature Conservancy (TNC) is a science-based, nonprofit organization with a mission to conserve the lands and waters on which all life depends. Like humans, plants and animals often rely on groundwater for survival, which is why TNC helped develop, and is now helping to implement, SGMA. Earlier this year, we launched the Groundwater Resource Hub, which is an online resource intended to help make it easier and cheaper to address environmental requirements under SGMA. As a first step in addressing when depletions might have an adverse impact, The Nature Conservancy recommends identifying the beneficial users of surface water, which include environmental users. This is a critical step, as it is impossible to define “significant and unreasonable adverse impacts” without knowing what is being impacted. To make this easy, we are providing this letter and the accompanying documents as the best available science on the freshwater species within the boundary of your groundwater sustainability agency (GSA). -
Owens Basin Wetland and Aquatic Species Recovery Plan Lnyo and Mono Counties,California OWENS BASIN WETLAND and AQUATIC SPECIES RECOVERY PLAN
Owens Basin Wetland and Aquatic Species Recovery Plan lnyo and Mono Counties,California OWENS BASIN WETLAND AND AQUATIC SPECIES RECOVERY PLAN INYG AND MONO COUNTIES, CALIFORNIA Owens pupfish, Owens tui chub, and Fish Slough milk-vetch and Selected Species of Concern Region I U.S. Fish and Wildlife Service Portland, Oregon Approved: U.S. ish and Wildlife Service Date: Cooperators r Concurred ~ .L~ ~zz:~~;WN ~ Director, California Department of Fish and Game Concurred K2) ~ C)\\Q~~~ \ CN ~N State Director, U.S. Bureau of Lana Management Concurred Regional ii DISCLAIMER Recovery plans delineate reasonable actions that are believed to be required to recover and/or protect listed species. Plans are published by the U.S. Fish and Wildlife Service (Service), and sometimes prepared with the assistance ofrecovery teams, contractors, State agencies, and others. Objectives will be attained and necessary funds made available subject to budgetary and other constraints affecting the parties involved, as well as the need to address other priorities. Recovery plans do not necessarily represent the views or the official positions or approval ofany individuals or agencies involved in the plan formulation, other than the U.S. Fish and Wildlife Service. They represent the official position of the U.S. Fish and Wildlife Service only after they have been signed by the Regional Director or Director as approved. Approved recovery plans are subject to modification as dictated by new findings, changes in species status, and the completion of recovery tasks. LITERATURE CITATIONS The literature citation for this recovery plan should read as follows: U.S. Fish and Wildlife Service. -
Chapter 3A. Environmental Setting, Impacts, and Mitigation Measures - Hydrology
Chapter 3A. Environmental Setting, Impacts, and Mitigation Measures - Hydrology INTRODUCTION As described in Chapter 2, alternative amendments to the City of Los Angeles appropriative water rights for diversion of four tributary streams in Mono Basin will have direct hydrologic effects on the four streams downstream of the diversions, the water balance and surface elevations of Mono Lake, and the amount of water exported to the Upper Owens River. The allowable exports from Mono Basin will also have indirect effects on Owens River flows, Lake Crowley reservoir storage, and exports from the Owens Valley to Los Angeles. The relationships between these variables were used to define a set of water rights alternatives using a monthly hydrologic model described in Chapter 2. Many of the hydrologic conditions in Mono Basin and the Owens River basin will not be altered by the proposed amendments to the city's water rights. The available runoff from the four Mono Lake tributary streams that are diverted by LADWP will not change. The other sources of water flowing into Mono Lake (e.g., rainfall, most groundwater, and other surface streamflow) will not change. The runoff and spring discharges in the Owens Valley will not be affected. As described in Chapter 2, the assumption has been made for this EIR that groundwater pumping in the Owens Valley will not change with amendment of Mono Basin water rights. The hydrologic records used to analyze the alternative water rights amendments for the four diverted Mono Lake tributaries are for 1940-1989. The LADWP diversions began in 1941 and continued until 1989. -
A List of Freshwater, Anadromous, and Euryhaline Fishes of California
CALIFORNIA FISH AND GAME California Fish and Game 86(4):244-258 2000 A LIST OF FRESHWATER, ANADROMOUS, AND EURYHALINE FISHES OF CALIFORNIA PETER B. MOYLE Department of Wildlife, Fish, and Conservation Biology University of California, Davis 1 Shields Avenue Davis, California 95616 e-mail: pbmoyle @ ucdavis.edu LIAM H. DAVIS California Department of Fish and Game 7329 Silverado Trail Yountville, California 94558 The freshwater fishes of California include 67 native resident or anadromous species, 53 non-native species, and 5 marine species that occur in fresh water, for a total of 125 species. Within these species, 100 taxa at lower levels (subspecies, Evolutionary Significant Units, runs of anadromous fish) are recognized. The number of freshwater fish species in California is increasing due to invasions of non-native fishes, which are becoming established at a rate of about 1 species every 3 years. Of the native fishes, 5 full species are extinct in California. Thus, the actual number of species maintaining populations in the state is 120. Of extant native species, 15 (22%) are threatened with extinction in the near future. Only 27 native species (40%) can be regarded as having secure populations. INTRODUCTION The fishes of California’s inland waters are a mixture of resident, anadromous, and euryhaline species, both native and non-native. The first attempt to compile a comprehensive list of these species was Evermann and Clark (1931), who listed 78 native species and 32 introduced species. Native species included an anomalous Pacific hagfish, Epatretus stouti, from the Eel River, 14 forms all now considered to be rainbow trout, and 18 other forms that are either no longer recognized as species or were mistakenly considered to be part of the California fish fauna. -
Long Valley Caldera Lake and Reincision of Owens River Gorge
Long Valley Caldera Lake and Reincision of Owens River Gorge Scientific Investigations Report 2016–5120 U.S. Department of the Interior U.S. Geological Survey COVER View southwestward across Long Valley Caldera and Sierra Nevada. Caldera depression, as wide as 30 km, formed during eruption of Bishop Tuff at 767 ka. Sierra consists of Mesozoic plutonic rocks, Mesozoic metavolcanic rocks, and Paleozoic marine metasedimentary strata. Patchy white exposures in caldera are lacustrine siltstones of middle Pleistocene age that are the top of a 700-m-thick accumulation of intracaldera lake sediment. Sedimentation in the deep closed depression took 600,000 years to raise lake level to its threshold for overflow around 150 ka. Outlet arm of Lake Crowley reservoir leads into Owens River Gorge, which extends 30 km southeast across a welded Bishop Tuff outflow sheet. Overflow and draining of the caldera lake reincised a 200-m-deep precaldera gorge (in Mesozoic granodiorite) that had been diverted by 3.3-Ma basalt and later blanketed by the Bishop Tuff. Round Valley Fault is 2-km-high east- facing scarp at left. At lower center of image, precaldera Glass Mountain rhyolite edifice was truncated by caldera collapse and draped by complexly incised apron of Bishop Tuff. Photo is a NaturalVue satellite image mosaic, which has been extracted from a global dataset of natural-color Landsat-7 multispectral images compiled by MDA Information Systems, Inc. Cover image produced and processed by Joel E. Robinson. Imagery copyright 2010, MDA Information Systems, USGS, NASA. Long Valley Caldera Lake and Reincision of Owens River Gorge By Wes Hildreth and Judy Fierstein Scientific Investigations Report 2016–5120 U.S.