Owens Lake and the Los Angeles Aqueduct
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Instructionally Related Activities Report
Instructionally Related Activities Report Linda O’Hirok, ESRM ESRM 463 Water Resources Management Owens Valley Field Trip, March 4-6, 2016 th And 5 Annual Water Symposium, April 25, 2016 DESCRIPTION OF THE ACTIVITY; The students in ESRM 463 Water Resources Management participated in a three-day field trip (March 4-6, 2016) to the Owens Valley to explore the environmental and social impacts of the City of Los Angeles (LA DWP) extraction and transportation of water via the LA Aqueduct to that city. The trip included visiting Owens Lake, the Owens Valley Visitor Center, Lower Owens Restoration Project (LORP), LA DWP Owens River Diversion, Alabama Gates, Southern California Edison Rush Creek Power Plant, Mono Lake and Visitor Center, June Mountain, Rush Creek Restoration, and the Bishop Paiute Reservation Restoration Ponds and Visitor Center. In preparation for the field trip, students received lectures, read their textbook, and watched the film Cadillac Desert about the history of the City of Los Angeles, its explosive population growth in the late 1800’s, and need to secure reliable sources of water. The class also received a summary of the history of water exploitation in the Owens Valley and Field Guide. For example, in 1900, William Mulholland, Chief Engineer for the City of Los Angeles, identified the Owens River, which drains the Eastern Sierra Nevada Mountains, as a reliable source of water to support Los Angeles’ growing population. To secure the water rights, Los Angeles secretly purchased much of the land in the Owens Valley. In 1913, the City of Los Angeles completed the construction of the 223 mile, gravity-flow, Los Angeles Aqueduct that delivered Owens River water to Los Angeles. -
Eocene Origin of Owens Valley, California
geosciences Article Eocene Origin of Owens Valley, California Francis J. Sousa College of Earth, Oceans, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA; [email protected] Received: 22 March 2019; Accepted: 26 April 2019; Published: 28 April 2019 Abstract: Bedrock (U-Th)/He data reveal an Eocene exhumation difference greater than four kilometers athwart Owens Valley, California near the Alabama Hills. This difference is localized at the eastern fault-bound edge of the valley between the Owens Valley Fault and the Inyo-White Mountains Fault. Time-temperature modeling of published data reveal a major phase of tectonic activity from 55 to 50 Ma that was of a magnitude equivalent to the total modern bedrock relief of Owens Valley. Exhumation was likely accommodated by one or both of the Owens Valley and Inyo-White Mountains faults, requiring an Eocene structural origin of Owens Valley 30 to 40 million years earlier than previously estimated. This analysis highlights the importance of constraining the initial and boundary conditions of geologic models and exemplifies that this task becomes increasingly difficult deeper in geologic time. Keywords: low-temperature thermochronology; western US tectonics; quantitative thermochronologic modeling 1. Introduction The accuracy of initial and boundary conditions is critical to the development of realistic models of geologic systems. These conditions are often controlled by pre-existing features such as geologic structures and elements of topographic relief. Features can develop under one tectono-climatic regime and persist on geologic time scales, often controlling later geologic evolution by imposing initial and boundary conditions through mechanisms such as the structural reactivation of faults and geomorphic inheritance of landscapes (e.g., [1,2]). -
Reditabs Viagra
Bishop Paiute Tribal Council Update The Bishop Indian Tribal Council wishes all of the community a Happy New Year 2018. In reflection of last years efforts to improve the livelihood of our Tribal Members through the growth of Tribal services, we anticipate a successful 2018 ahead. Contin- ue to stay updated with the good things happening in our community by continuing to read our monthly newsletter articles and attend tribal meetings. A new way to com- municate concerns and give feedback on programs directly to the Tribal Council will be to attend our new Monthly CIM (Community Input Meetings), starting with the first one on January 16, 2018 @ 6pm in the Tribal Chambers. Our monthly CIM’s will be an open discussion with the BITC talking about current efforts and concerns the commu- nity may have. As always, If you have any suggestions or comments to assist us in these efforts, please contact Brian Poncho @ 760-873-3584 Ext.1220. Law Enforcement - The Tribal Police Department has began efforts to identify Non-Indians in our community who are participating in drug activity on the Reservation. Once identified the Council will begin efforts of removal off of Tribal Lands. These efforts have been a result of continuous concerns from our tribal community. If you have any concerns about persons Tribal/Non-Tribal on the reservation who may be involved in drug activi- ty please contact our Tribal Police Department. Tribal Police Chief Hernandez can be contacted @ (760) 920-2759 New Gas Station- Plans for a new gas station on the corner of See Vee Ln and Line St have been developed throughout the year 2016-2017 and will begin by Spring 2018. -
The History of Valentine Camp by Mary Farrell
History of Valentine Camp Mary M. Farrell Trans-Sierran Archaeological Research P.O. Box 840 Lone Pine, CA 93545 November 7, 2015 Prepared for Valentine Eastern Sierra Reserve University of California, Santa Barbara, Natural Reserve System Sierra Nevada Aquatic Research Laboratory 1016 Mt. Morrison Road Mammoth Lakes, CA 93546 Abstract Located in Mammoth Lakes, California, Valentine Camp and the nearby Sierra Nevada Aquatic Research Laboratory form the Valentine Eastern Sierra Reserve, a field research station in the University of California's Natural Reserve System. The University’s tenure at Valentine Camp began over 40 years ago, but the area’s history goes back thousands of years. Before the arrival of Euroamericans in the nineteenth century, the region was home to Paiutes and other Native American tribes. Land just east of Valentine Camp was surveyed under contract with the United States government in 1856, and mineral deposits in the mountains just west of Valentine Camp brought hundreds of miners to the vicinity in the last decades of the nineteenth century. Even as mining in the region waned, grazing increased. The land that became Valentine Camp was patented in 1897 by Thomas Williams, a rancher and capitalist who lived in Owens Valley. It was Williams’s son, also Thomas, who sold the 160 acres to Valentine Camp’s founders. Those founders were very wealthy, very influential men in southern California who could have, and did, vacation wherever they wanted. Anyone familiar with the natural beauty of Mammoth Lakes would not be surprised that they chose to spend time at Valentine Camp. Valentine Camp was donated to the University of California Natural Land and Water Reserve System (now the Natural Reserve System) in 1972 to ensure the land’s continued protection. -
Chapter 8 Manzanar
CHAPTER 8 MANZANAR Introduction The Manzanar Relocation Center, initially referred to as the “Owens Valley Reception Center”, was located at about 36oo44' N latitude and 118 09'W longitude, and at about 3,900 feet elevation in east-central California’s Inyo County (Figure 8.1). Independence lay about six miles north and Lone Pine approximately ten miles south along U.S. highway 395. Los Angeles is about 225 miles to the south and Las Vegas approximately 230 miles to the southeast. The relocation center was named after Manzanar, a turn-of-the-century fruit town at the site that disappeared after the City of Los Angeles purchased its land and water. The Los Angeles Aqueduct lies about a mile to the east. The Works Progress Administration (1939, p. 517-518), on the eve of World War II, described this area as: This section of US 395 penetrates a land of contrasts–cool crests and burning lowlands, fertile agricultural regions and untamed deserts. It is a land where Indians made a last stand against the invading white man, where bandits sought refuge from early vigilante retribution; a land of fortunes–past and present–in gold, silver, tungsten, marble, soda, and borax; and a land esteemed by sportsmen because of scores of lakes and streams abounding with trout and forests alive with game. The highway follows the irregular base of the towering Sierra Nevada, past the highest peak in any of the States–Mount Whitney–at the western approach to Death Valley, the Nation’s lowest, and hottest, area. The following pages address: 1) the physical and human setting in which Manzanar was located; 2) why east central California was selected for a relocation center; 3) the structural layout of Manzanar; 4) the origins of Manzanar’s evacuees; 5) how Manzanar’s evacuees interacted with the physical and human environments of east central California; 6) relocation patterns of Manzanar’s evacuees; 7) the fate of Manzanar after closing; and 8) the impact of Manzanar on east central California some 60 years after closing. -
Boyhood Days in the Owens Valley 1890-1908
Boyhood Days in the Owens Valley 1890-1908 Beyond the High Sierra and near the Nevada line lies Inyo County, California—big, wild, beautiful, and lonely. In its center stretches the Owens River Valley, surrounded by the granite walls of the Sierra Nevada to the west and the White Mountains to the east. Here the remote town of Bishop hugs the slopes of towering Mount Tom, 13,652 feet high, and here I was born on January 6, 1890. When I went to college, I discovered that most Californians did not know where Bishop was, and I had to draw them a map. My birthplace should have been Candelaria, Nevada, for that was where my parents were living in 1890. My father was an engineer in the Northern Belle silver mine. I was often asked, "Then how come you were born in Bishop?" and I replied, "Because my mother was there." The truth was that after losing a child at birth the year before, she felt Candelaria's medical care was not to be trusted. The decline in the price of silver, the subsequent depression, and the playing out of the mines in Candelaria forced the Albright family to move to Bishop permanently. We had a good life in Bishop. I loved it, was inspired by its aura, and always drew strength and serenity from it. I have no recollection of ever having any bad times. There weren't many special things to do, but what- ever we did, it was on horseback or afoot. Long hours were spent in school. -
The Abandonment of the Cerro Gordo Silver Mining Claim 1869-1879: Abstracted to the Exchange of Energies Marley Mclaughlin Chapman University
Voces Novae Volume 6 Article 4 2018 The Abandonment of the Cerro Gordo Silver Mining Claim 1869-1879: Abstracted to the Exchange of Energies Marley McLaughlin Chapman University Follow this and additional works at: https://digitalcommons.chapman.edu/vocesnovae Recommended Citation McLaughlin, Marley (2018) "The Abandonment of the Cerro Gordo Silver Mining Claim 1869-1879: Abstracted to the Exchange of Energies," Voces Novae: Vol. 6 , Article 4. Available at: https://digitalcommons.chapman.edu/vocesnovae/vol6/iss1/4 This Article is brought to you for free and open access by Chapman University Digital Commons. It has been accepted for inclusion in Voces Novae by an authorized editor of Chapman University Digital Commons. For more information, please contact [email protected]. McLaughlin: The Abandonment of the Cerro Gordo Silver Mining Claim 1869-1879: The Abandonment of Cerro Gordo Voces Novae: Chapman University Historical Review, Vol 6, No 1 (2014) HOME ABOUT USER HOME SEARCH CURRENT ARCHIVES PHI ALPHA THETA Home > Vol 6, No 1 (2014) The Abandonment of the Cerro Gordo Silver Mining Claim 1869--1879: Abstracted to the Exchange of Energies Marley McLaughlin The mountain air of November echoed the screeching of brake pads from one lone stagecoach as it bumped down the Inyo mountain range's Yellow Grade Road in 1879. The 8,000--foot descent down the wagon road sent that last sound careening from the mine of Cerro Gordo as if the land was celebrating its own emptiness. After the fall of the mine's heyday years, all but the physical body of the town proved evanescent. Pioneers loaded the last wagon with only a couple bars of lead and one 420--pound ingot of pure silver despite the town's promise of wealth.[1]The metals, brick, and wood left scattered in the town were more enduring than men. -
Owens Valley Groundwater Basin Bulletin 118
South Lahontan Hydrologic Region California’s Groundwater Owens Valley Groundwater Basin Bulletin 118 Owens Valley Groundwater Basin • Groundwater Basin Number: 6-12 • County: Inyo & Mono • Surface Area: 661,000 acres (1,030 square miles) Basin Boundaries and Hydrology This groundwater basin underlies Benton, Hammil, and Chalfant Valleys in Mono County and Round and Owens Valleys in Inyo County. This basin is bounded by nonwater-bearing rocks of the Benton Range on the north, of the Coso Range on the south, of the Sierra Nevada on the west, and of the White and Inyo Mountians on the east (Jennings 1958; DWR 1964; Matthews and Burnett 1965; Strand 1967; Danskin 1998) This system of valleys is drained by several creeks to the Owens River, which flows southward into the Owens (dry) Lake, a closed drainage depression in the southern part of the Owens Valley. Average annual precipitation is 30 inches in the Sierra Nevada, 7 to 10 inches in the White and Inyo Mountains, and 4 to 6 inches on the Owens Valley floor (Groeneveld and others 1986a; 1986b; Duell 1990; Hollett and others 1991). Hydrogeologic Information Water Bearing Formations The water-bearing materials of this basin are sediments that fill the valley and reach at least 1,200 feet thick (DWR 1964). The primary productive unit is Quaternary in age and is separated into upper, lower and middle members (Danskin 1998). Upper Member. The upper member is composed of unconsolidated coarse alluvial fan material deposited along the margin of the basin, grading into layers of sand and silty clay of fluvial and lacustrine origin toward the axis of the basin. -
Proposal to Prepare Prepared
Proposal to Prepare GROUNDWATER SUSTAINABILITY PLAN OWENS VALLEY GROUNDWATER BASIN Prepared for County of Inyo Water Department Prepared by William R. Hutchison Independent Groundwater Consultant July 2018 Cover Letter July 30, 2018 Mr. Bob Harrington, Director Inyo County Water Department 135 S. Jackson Street Independence, California 93526 Subject: LSCE Team Proposal for Support Services to Develop a Groundwater Sustainability Plan for the Owens Valley Groundwater Basin Dear Mr. Harrington: Luhdorff & Scalmanini Consulting Engineers (LSCE), in association with TEAM Engineering and Management Inc., Dr. Bill Hutchison, Pacific Agroecology, Consensus and Collaboration Program (CCP), and ERA Economics (ERA) are pleased to submit this proposal in response to the June 20, 2018 Request for Qualifications (RFQ) to develop a single Groundwater Sustainability Plan (GSP) for the Owens Valley Groundwater Basin. To assist the Owens Valley Groundwater Authority (OVGA, exclusive GSA for the Basin) with the development of a GSP, we have assembled this team of highly experienced firms. LSCE will serve as the prime contractor; TEAM will provide local support for many tasks in the scope; Bill Hutchison will support tasks relating to water budget analyses and lead the task related to evaluation of existing groundwater flow models and recommendations; Pacific Agroecology (PAE) will support tasks related to outreach to beneficial users, particularly as related to groundwater dependent ecosystems and fish habitat and ecological considerations; the Consensus and Collaboration Program (CCP) group will lead the preparation of a public engagement plan and activities necessary to comply with SGMA requirements for public outreach and communication; and ERA will prepare a cost and rate study and provide a preliminary evaluation of the economic and financial feasibility of projects and potential management actions. -
Lower Owens River Draft Recreation Use Plan
LOWER OWENS RIVER RECREATION USE PLAN JANUARY 2012 DRAFT MIG, Inc. 815 SW 2ND AVE. SUITE 200 PORTLAND, OR 97204 503.297.1005 www.migcom.com TABLE OF CONTENTS Executive Summary..............................................................................i I. Introduction ................................................................................1 II. Existing Conditions ....................................................................6 III. Recreation Preferences and Goals ...........................................11 IV. Recreation Use Plan Alternatives.............................................20 V. Next Steps.................................................................................37 Appendix A: Potential Impacts for Further Study ......................... A-1 Appendix B: Community Involvement Findings ............................ B-1 LOWER OWENS RIVER RECREATION USE PLAN TABLE OF CONTENTS Executive Summary..............................................................................i I. Introduction ................................................................................1 II. Existing Conditions ....................................................................6 III. Recreation Preferences and Goals ...........................................11 IV. Recreation Use Plan Alternatives.............................................20 V. Next Steps.................................................................................37 Appendix A: Potential Impacts for Further Study ......................... A-1 Appendix -
Distribution and Abundance of Tule Elk in the Owens Valley January 2020
Owens Valley Tule Elk Report 2020 Distribution and Abundance of Tule Elk in the Owens Valley January 2020 This final report fulfills the objectives that were outlined in the “Owens Valley Elk Movement” project proposal with a project start date of spring 2015 California Department of Fish and Wildlife Bishop, California Mike Morrison, Environmental Scientist Cody Massing, Environmental Scientist Dave German, Research Analyst Tom Stephenson, Wildlife Supervisor 1 Owens Valley Tule Elk Report 2020 EXECUTIVE SUMMARY In 2019, the minimum count for the Owens Valley population of tule elk (Cervus canadensis nannodes) was 343 elk with an annual recruitment rate of 0.37; the historic average annual population and recruitment rate were 335 and 0.30, respectively. The Owens Valley population of tule elk is distributed between lowland habitat, concentrated mainly around the Owens River and east of U.S. Highway 395, and upland habitat, which is located on the west side of Highway 395 along the base of the Sierra Nevada mountains. The lowland population is comprised of the Bishop, Tinemaha, Independence, and Lone Pine sub-herds with a current population of 196 tule elk. The upland population is comprised of the Tinemaha West, Tinemaha Mountain, Goodale, and Whitney sub-herds with a current population of 147 tule elk. There are no known cow elk occupying the Tinemaha Mountain sub-herd at present. In February 2019, 30 tule elk were translocated from the Central Valley to the Owens Valley. Eight bulls and twelve cows were translocated from the San Luis National Wildlife Refuge (SLNWR) in Los Banos on February 2 and one bull along with nine cows were translocated from the Tupman State Reserve in Buttonwillow (near Bakersfield) on February 3, 2019. -
Owens Lake Land Art Keeler, CA
Owens Lake Land Art Keeler, CA Owens Dry Lake is located in the Owens Valley on the eastern side of the Sierra Nevada Range in Inyo County, California. Unlike most dry lakes in North America’s Basin and Range Province which have been dry for thousands of years, Owens held significant water until 1913. To supply Southern California’s rapid population growth, the Owens River was diverted into the Los Angeles Aqueduct, causing Owens Lake to desiccate by 1926. The lake became the largest single source of dust pollution in the United States. Legislation passed in 1983 initiated the dust mitigation effort. Since then, significant reductions in dust production have been realized through the implementation of mitigation measures (shallow flood, gravel cover, and managed vegetation) over engineered parcels on the dry lake playa. Purpose of Project and Role of Landscape Architect Owens Lake Land Art project (located on a 700 acre parcel named T30) began with a mandate from California State Lands to the Los Angeles Department of Water and Power (LADWP) to meet the following goals: provide public access and hiking trails, create bird and mammal habitat, and preserve cultural resources while still meeting the dust emission controls. The landscape architect, adhering to the approved yet limited dust mitigation palette (shallow flood, gravel cover, and managed vegetation where soil conditions allow), designed a solution which evolved into a land art project named the ‘Whitecaps’. The project did not start out as an art commission yet the design developed into a spiritual composition of simple materials and forms inspired by the Owens Valley.