The Future of the Salton Sea with No Restoration Project
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Overview of Management and Restoration Activities in the Salton Sea Name Redacted Specialist in Natural Resources Policy
Overview of Management and Restoration Activities in the Salton Sea name redacted Specialist in Natural Resources Policy May 26, 2004 Congressional Research Service 7-.... www.crs.gov RL31820 CRS Report for Congress Prepared for Members and Committees of Congress Overview of Management and Restoration Activities in the Salton Sea Summary The Salton Basin in southern California has supported many lakes and water bodies throughout its geological history. The most recent inland water body in the Basin is the Salton Sea, which was created from a levee break in 1905. The Salton Sea is the largest inland water body in California. In the past several decades the salinity of the Sea has been increasing, and is now considered a significant threat to the health of the current Salton Sea ecosystem. Ecosystem changes in the Sea were exemplified by several large die-offs of fish and birds that inhabit the Sea. Some of these events included endangered species such as the brown pelican. The Sea receives most of its water from agricultural drainage originating in the Imperial and Coachella Valleys in California. When water transfers from agricultural lands in these valleys to municipal water districts in San Diego were proposed to reduce California’s reliance on water from the Colorado River, concerns about the environmental impacts of these transfers on the Sea surfaced. The proposed water transfers would have resulted in less water flowing into the Salton Sea, which according to some scientists would increase the rate of evaporation in the Sea so that salinity levels would be lethal to most fish and wildlife in less than 10 years. -
The Colorado River Aqueduct
Fact Sheet: Our Water Lifeline__ The Colorado River Aqueduct. Photo: Aerial photo of CRA Investment in Reliability The Colorado River Aqueduct is considered one of the nation’s Many innovations came from this period in time, including the top civil engineering marvels. It was originally conceived by creation of a medical system for contract workers that would William Mulholland and designed by Metropolitan’s first Chief become the forerunner for the prepaid healthcare plan offered Engineer Frank Weymouth after consideration of more than by Kaiser Permanente. 50 routes. The 242-mile CRA carries water from Lake Havasu to the system’s terminal reservoir at Lake Mathews in Riverside. This reservoir’s location was selected because it is situated at the upper end of Metropolitan’s service area and its elevation of nearly 1,400 feet allows water to flow by gravity to the majority of our service area The CRA was the largest public works project built in Southern California during the Great Depression. Overwhelming voter approval in 1929 for a $220 million bond – equivalent to a $3.75 billion investment today – brought jobs to 35,000 people. Miners, engineers, surveyors, cooks and more came to build Colorado River the aqueduct, living in the harshest of desert conditions and Aqueduct ultimately constructing 150 miles of canals, siphons, conduits and pipelines. They added five pumping plants to lift water over mountains so deliveries could then flow west by gravity. And they blasted 90-plus miles of tunnels, including a waterway under Mount San Jacinto. THE METROPOLITAN WATER DISTRICT OF SOUTHERN CALIFORNIA // // JULY 2021 FACT SHEET: THE COLORADO RIVER AQUEDUCT // // OUR WATER LIFELINE The Vision Despite the city of Los Angeles’ investment in its aqueduct, by the early 1920s, Southern Californians understood the region did not have enough local supplies to meet growing demands. -
A History of Water — and the Salton Sea — in Imperial
Imperial Valley Press Saturday, March 21, 2015 A7 Land of Extremes QUESTIONS? Contact Local Content Editor Richard Montenegro Brown at [email protected] or 760-337-3453. UNCERTAIN FUTURE A history of water — and the Salton Sea — in Imperial BY NEAL V. HITCH Special to this Newspaper/Imperial Valley here is a cur- rent debate Sediments from the Grand Canyon among geol- and Colorado Pla- T ogists as to teau fill in the Gulf when the Grand Can- yon formed. In 2011, new evidence suggest- ed the Colorado River began carving into the Colorado Plateau 17 million years ago. This is different than the ABOVE: About 3.5 million years ago silt from the Colorado River fi lled the Gulf of California leaving a large salt lake in traditional theories what would become the Imperial Valley. PHOTOS COURTESY OF IMPE- dating to 6 million RIAL VALLEY DESERT MUSEUM years ago. What is clear, however, is what happened to the ma- terial after it left the ABOVE: Design of the Topographical Water Interactive by Wel- don Exhibit. RIGHT: Lake Cahuilla was created when the Col- Grand Canyon. orado River changed its course and fi lled the Imperial Valley. When it reached 39 feet above sea level, the water would open An interactive a breech and spill back into the Gulf of California. the Colorado River drained take advantages of the abun- topographical map into the Gulf until it was dance of resources the lake closed off. offered. The lake was com- This week at the museum A body of salt water re- pletely dry by 1700. -
Chapter 1: Introduction
1. Introduction 1.1 Introduction and Background The Sonny Bono Salton Sea National Wildlife Refuge Complex (Complex or NWRC) consists of the Sonny Bono Salton Sea National Wildlife Refuge (NWR) and Coachella Valley NWR. Although both Refuges are located within the 8,000-square-mile Salton Basin of the Colorado Desert (Figure 1-1), the purposes of these two Refuges are as different as the habitats and species they protect. The Sonny Bono Salton Sea NWR, which consists of 37,660 acres, is situated at the south end of the Salton Sea, about 20 miles north of El Centro in Imperial County, California (Figure 1-2). The purpose of this Refuge is to protect and manage habitat to support migratory birds, particularly waterfowl, and other wildlife. Thousands of shorebirds, seabirds, and waterfowl stop-over or winter at the Salton Sea (Mark Stewart/USFWS) About 75 miles to the northwest is the 3,577-acre Coachella Valley NWR, located 10 miles east of Palm Springs in Riverside County, California (Figure 1-3). The purpose of this Refuge is to protect and contribute to the long-term survival of the federally threatened Coachella Valley fringe-toed lizard (Uma inornata) and federally endangered Coachella Valley milk-vetch (Astragalus lentiginosus var. coachellae), both endemic to the active sand habitats in the Coachella Valley. The U.S. Fish and Wildlife Service (Service) prepared this Comprehensive Conservation Plan (CCP) for the Sonny Bono Salton Sea NWR and Coachella Valley NWR to guide the management of these Refuges over the next 15 years. The CCP describes future Refuge conditions and provides long-range management direction for achieving the purposes for which each Refuge was established. -
Salton Sea Hydrological Modeling and Results
TECHNICAL REPORT Salton Sea Hydrological Modeling and Results Prepared for Imperial Irrigation District October 2018 CH2M HILL 402 W. Broadway, Suite 1450 San Diego, CA 92101 Contents Section Page 1 Introduction ....................................................................................................................... 1-1 2 Description of Study Area .................................................................................................... 2-1 2.1 Background ...................................................................................................................... 2-1 2.2 Salton Sea Watershed ...................................................................................................... 2-2 3 SALSA2 Model Description .................................................................................................. 3-1 3.1.1 Time Step ............................................................................................................ 3-2 3.2 Air Quality Mitigation and Habitat Components Incorporated into SALSA2 ................... 3-2 3.3 Simulations of Water and Salt Balance ............................................................................ 3-4 3.3.1 Inflows ................................................................................................................. 3-4 3.3.2 Consumptive Use Demands and Deliveries ........................................................ 3-4 3.3.3 Salton Sea Evaporation ...................................................................................... -
Law of the River the Colorado River Compact
Colorado River Water Users Association: Law of the River . The Colorado River Compact . As the 20th century dawned, the The Colorado River Compact vast domain of the Colorado River lay almost entirely Boulder Canyon Project Act untouched. Though there had been a few early filings for Treaty with Mexico diversion and a "grand ditch" conveying water some 16 miles across the Continental Divide Upper Colorado River Basin into eastern Colorado in the late Compact of 1948 1800s, California's Imperial Valley was among the first areas to tap the river's true potential. In early 1901, the 60 mile long Alamo Canal, Colorado River Storage Project developed by private concerns, was completed to deliver Colorado Act River water for irrigation, and a wasteland was transformed. But the Imperial Valley did not move ahead without problems. About 50 miles Grand Canyon Protection Act of the canal coursed through Mexico, leaving the valley farmers at the mercy of a foreign government. And in 1905, the river, raging with Arizona vs. California floods, eroded the opening to the canal, roared through and created the Salton Sea before the river was pushed back into its normal channel. Future of Western Water With the constant threat of flood looming along the lower Colorado, demands grew for some sort of permanent flood control work -a storage reservoir and dam on the river. And Imperial Valley farmers called for a canal totally within the United States, free of Mexican interference. By 1919, Imperial Irrigation District had won the support of the federal Bureau of Reclamation. A bureau engineering board recommended favorably on the canal and added the government "should undertake the early construction of a storage reservoir on the drainage basin of the Colorado." While this report was greeted with enthusiasm by people along the river's lower stretches, it was viewed with alarm by those in upper reaches. -
Sonny Bono Salton Sea National Wildlife Refuge Complex
Appendix J Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex Appendix J: Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex The following sections describe the cultural setting in and around the two refuges that constitute the Sonny Bono Salton Sea National Wildlife Refuge Complex (NWRC) - Sonny Bono Salton Sea NWR and Coachella Valley NWR. The cultural resources associated with these Refuges may include archaeological and historic sites, buildings, structures, and/or objects. Both the Imperial Valley and the Coachella Valley contain rich archaeological records. Some portions of the Sonny Bono Salton Sea NWRC have previously been inventoried for cultural resources, while substantial additional areas have not yet been examined. Seventy-seven prehistoric and historic sites, features, or isolated finds have been documented on or within a 0.5- mile buffer of the Sonny Bono Salton Sea NWR and Coachella Valley NWR. Cultural History The outline of Colorado Desert culture history largely follows a summary by Jerry Schaefer (2006). It is founded on the pioneering work of Malcolm J. Rogers in many parts of the Colorado and Sonoran deserts (Rogers 1939, Rogers 1945, Rogers 1966). Since then, several overviews and syntheses have been prepared, with each succeeding effort drawing on the previous studies and adding new data and interpretations (Crabtree 1981, Schaefer 1994a, Schaefer and Laylander 2007, Wallace 1962, Warren 1984, Wilke 1976). The information presented here was compiled by ASM Affiliates in 2009 for the Service as part of Cultural Resources Review for the Sonny Bono Salton Sea NWRC. Four successive periods, each with distinctive cultural patterns, may be defined for the prehistoric Colorado Desert, extending back in time over a period of at least 12,000 years. -
Colorado River Slideshow Title TK
The Colorado River: Lifeline of the Southwest { The Headwaters The Colorado River begins in the Rocky Mountains at elevation 10,000 feet, about 60 miles northwest of Denver in Colorado. The Path Snow melts into water, flows into the river and moves downstream. In Utah, the river meets primary tributaries, the Green River and the San Juan River, before flowing into Lake Powell and beyond. Source: Bureau of Reclamation The Path In total, the Colorado River cuts through 1,450 miles of mountains, plains and deserts to Mexico and the Gulf of California. Source: George Eastman House It was almost 1,500 years ago when humans first tapped the river. Since then, the water has been claimed, reclaimed, divided and subdivided many times. The river is the life source for seven states – Arizona, California, Colorado, Nevada, New Mexico, Utah and Wyoming – as well as the Republic of Mexico. River Water Uses There are many demands for Colorado River water: • Agriculture and Livestock • Municipal and Industrial • Recreation • Fish/Wildlife and Habitat • Hydroelectricity • Tribes • Mexico Source: USGS Agriculture The Colorado River provides irrigation water to about 3.5 million acres of farmland – about 80 percent of its flows. Municipal Phoenix Denver About 15 percent of Colorado River flows provide drinking and household water to more than 30 million people. These cities include: Las Vegas and Phoenix, and cities outside the Basin – Denver, Albuquerque, Salt Lake City, Los Angeles, San Diego and Tijuana, Mexico. Recreation Source: Utah Office of Tourism Source: Emma Williams Recreation includes fishing, boating, waterskiing, camping and whitewater rafting in 22 National Wildlife Refuges, National Parks and National Recreation Areas along river. -
Southern Exposures
Searching for the Pliocene: Southern Exposures Robert E. Reynolds, editor California State University Desert Studies Center The 2012 Desert Research Symposium April 2012 Table of contents Searching for the Pliocene: Field trip guide to the southern exposures Field trip day 1 ���������������������������������������������������������������������������������������������������������������������������������������������� 5 Robert E. Reynolds, editor Field trip day 2 �������������������������������������������������������������������������������������������������������������������������������������������� 19 George T. Jefferson, David Lynch, L. K. Murray, and R. E. Reynolds Basin thickness variations at the junction of the Eastern California Shear Zone and the San Bernardino Mountains, California: how thick could the Pliocene section be? ��������������������������������������������������������������� 31 Victoria Langenheim, Tammy L. Surko, Phillip A. Armstrong, Jonathan C. Matti The morphology and anatomy of a Miocene long-runout landslide, Old Dad Mountain, California: implications for rock avalanche mechanics �������������������������������������������������������������������������������������������������� 38 Kim M. Bishop The discovery of the California Blue Mine ��������������������������������������������������������������������������������������������������� 44 Rick Kennedy Geomorphic evolution of the Morongo Valley, California ���������������������������������������������������������������������������� 45 Frank Jordan, Jr. New records -
Sunland-Tujunga, Lake View Terrace and Shadow Hills 07.14.2020 GREATER LOS ANGELES COUNTY INTEGRATED REGIONAL WATER MANAGEMENT REGION
Sunland-Tujunga, Lake View Terrace and Shadow Hills 07.14.2020 GREATER LOS ANGELES COUNTY INTEGRATED REGIONAL WATER MANAGEMENT REGION Sylmar Uninc. Sylmar San Fernando «¬118 Arleta - Pacoima Sunland-Tujunga-Lake View Terrace-Shadow Hills Mission Hills - Panorama City Sun Valley - ¨¦§210 - North Hills La Tuna Canyon La Canada Flintridge ¨¦§5 «¬170 Glendale Burbank North Hollywood - Valley Village City of LA Valley Glen - North 0 0.5 1 2 «¬2 Sherman Oaks ° City of LA Hollywood Miles Community Boundary Funded by California Department of Water Resources and Prop 1 It’s our water. TOOLKIT TABLE OF CONTENTS PROJECT BACKGROUND What is WaterTalks? IRWM Regions- How do we plan for water in California? Project Overview- How is WaterTalks funded? Funding- What sources of funding are available for water-related projects? WATER IN OUR ENVIRONMENT Surface Water and Groundwater- Where does my rainwater go? How do contaminants get into our water? Watershed- What is a watershed? Groundwater- Where does my groundwater come from? Flooding- Am I at risk of flooding? (optional) Access to Parks and Local Waterways- How clean are our lakes, streams, rivers, and beaches? Where can I find parks and local waterways? Existing Land Use- How does land use affect our water? Capturing and Storing Water- How can we catch and store rainwater? OUR TAP WATER Water Sources- Where does my tap water come from? Water Consumption- How much water does one person drink? How much water do we use at home? Tap Water Quality- How clean is my drinking water? Water Service Provider- -
Redalyc.Observations of Remotely Triggered Seismicity in Salton Sea
Geofísica Internacional ISSN: 0016-7169 [email protected] Universidad Nacional Autónoma de México México Castro, Raul R.; Clayton, Robert; Hauksson, Egill; Stock, Joann Observations of remotely triggered seismicity in Salton Sea and Coso geothermal regions, Southern California, USA, after big (MW>7.8) teleseismic earthquakes Geofísica Internacional, vol. 56, núm. 3, julio-septiembre, 2017, pp. 269-286 Universidad Nacional Autónoma de México Distrito Federal, México Available in: http://www.redalyc.org/articulo.oa?id=56851629004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative GEOFÍSICA INTERNACIONAL (2017) 56-3: 269-286 ORIGINAL PAPER Observations of remotely triggered seismicity in Salton Sea and Coso geothermal regions, Southern California, USA, after big (MW>7.8) teleseismic earthquakes Raul R. Castro*, Robert Clayton, Egill Hauksson and Joann Stock Received: September 27, 2016; accepted: January 08, 2017; published on line: July 01, 2017 Resumen incrementó en las dos regiones 9 días después de este mega-evento. La sismicidad después Se analizó un catálogo de sismos relocalizados del sismo de Chile del 2010 (Mw8.8) incrementó en las regiones cercanas a los campos en ambas regiones aproximadamente 14 días geotérmicos de Coso y Salton Sea, en el sur después de la ocurrencia de este telesimo. de California, USA, para investigar posibles La sismicidad en las regiones de Salton cambios en la tasa de sismicidad durante y Sea y de Coso incrementaron 17 y 14 días, después de telesismos grandes (Mw>7.8). -
Salton Sea Chronology a Salton Sea Chronology
RECLAMATION Managing Water in the West \ / U.S. Department of the Interior -- Bureau of Reclamation January 2016 Mission Statement The Bureau of Reclamation manages, develops, and protects water and related resources in an environmentally and economically sound manner in the interest of the American public. A Salton Sea Chronology A Salton Sea Chronology (Prehistory-2015) Year Events 10,000 BC First recorded human habitation in the Salton Basin. (Approx) 700 AD Lake Cahuilla is formed in the Salton Basin when the Colorado River silts (Flood!) up its outlet to the Gulf of California and swings northward. Lake Cahuilla is subject to multiple wet and dry cycles over intervening years. 1500 Large inflow of the Colorado River water fills Lake Cahuilla to create a waterbody 26 (Flood!) times the size of the current Salton Sea. (The calcareous water line remains visible on the northwest mountains in the present day). 1840-1891 Multiple flood events from the Colorado River are recorded in the Salton Basin forming ephemeral lakes up to 100,000 acres. 1876 Executive Order of May 15, 1876, establishes the Torres Martinez Desert Cahuilla Indian Reservation with a grant of 640 acres (Torres Martinez Compact, 2003). 1891 Executive Order of December 19, 1891, pursuant to the Mission Indian Relief Act of 1891, expands the Torres Martinez Desert Cahuilla Indian Reservation approximately 12,000 acres on the northern side of the Salton Basin. 1892 New Liverpool Salt Company mines salt from a salt marsh centered west of the railroad station named “Salton”. 1901 California Development Company is contracted by a private entity to build a canal (the Alamo Canal) to deliver water by gravity flow from the Colorado River to irrigate the Imperial Valley.