Benchmark 4: Conceptual Plans and Cost Estimates Volume 1: Water Import and Export Options May 2016
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Section 3.3 Geology Jan 09 02 ER Rev4
3.3 Geology and Soils 3.3.1 Introduction and Summary Table 3.3-1 summarizes the geology and soils impacts for the Proposed Project and alternatives. TABLE 3.3-1 Summary of Geology and Soils Impacts1 Alternative 2: 130 KAFY Proposed Project: On-farm Irrigation Alternative 3: 300 KAFY System 230 KAFY Alternative 4: All Conservation Alternative 1: Improvements All Conservation 300 KAFY Measures No Project Only Measures Fallowing Only LOWER COLORADO RIVER No impacts. Continuation of No impacts. No impacts. No impacts. existing conditions. IID WATER SERVICE AREA AND AAC GS-1: Soil erosion Continuation of A2-GS-1: Soil A3-GS-1: Soil A4-GS-1: Soil from construction existing conditions. erosion from erosion from erosion from of conservation construction of construction of fallowing: Less measures: Less conservation conservation than significant than significant measures: Less measures: Less impact with impact. than significant than significant mitigation. impact. impact. GS-2: Soil erosion Continuation of No impact. A3-GS-2: Soil No impact. from operation of existing conditions. erosion from conservation operation of measures: Less conservation than significant measures: Less impact. than significant impact. GS-3: Reduction Continuation of A2-GS-2: A3-GS-3: No impact. of soil erosion existing conditions. Reduction of soil Reduction of soil from reduction in erosion from erosion from irrigation: reduction in reduction in Beneficial impact. irrigation: irrigation: Beneficial impact. Beneficial impact. GS-4: Ground Continuation of A2-GS-3: Ground A3-GS-4: Ground No impact. acceleration and existing conditions. acceleration and acceleration and shaking: Less than shaking: Less than shaking: Less than significant impact. -
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. -
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. -
The Future of the Salton Sea with No Restoration Project
HAZARD The Future of the Salton Sea With No Restoration Project MAY 2006 © Copyright 2006, All Rights Reserved ISBN No. 1-893790-12-6 ISBN-13: 978-1-893790-12-4 Pacific Institute 654 13th Street, Preservation Park Oakland, CA 94612 Telephone (510) 251-1600 Facsimile (510) 251-2203 [email protected] www.pacinst.org HAZARD The Future of the Salton Sea With No Restoration Project Michael J. Cohen and Karen H. Hyun A report of the MAY 2006 Prepared with the support of The Salton Sea Coalition & Imperial Visions The U.S. Geological Survey Salton Sea Science Office and the Compton Foundation About the Authors Michael Cohen is a Senior Associate at the Pacific Institute. He is the lead author of the Institute’s 1999 report entitled Haven or Hazard: The Ecology and Future of the Salton Sea, and of the 2001 report entitled Missing Water: The Uses and Flows of Water in the Colorado River Delta Region. He is also the co-author of several journal articles on water and the environment in the border region. He is a member of the California Resources Agency’s Salton Sea Advisory Committee. Karen Hyun is a Ph.D. candidate in the Marine Affairs Program at the University of Rhode Island. Her research interests include ecosystem-based management and governance, especially in the Colorado River Delta. She also has interests in transboundary water issues, authoring Solutions Lie Between the Extremes: The Evolution of International Watercourse Law on the Colorado River. In addition, she has examined watershed to coast issues in Transboundary Solutions to Environmental Problems in the Gulf of California Large Marine Ecosystem. -
Field Trip Log Gulf of California Rift System: Laguna Salda-Valles Chico-San Feli- Pe, Baja California, México
Geos, Vol. 28, No. 1, Septiembre, 2008 FIELD TRIP LOG GULF OF CALIFORNIA RIFT SYSTEM: LAGUNA SALDA-VALLES CHICO-SAN FELI- PE, BAJA CALIFORNIA, MÉXICO Francisco Suárez-Vidal Departamento de Geologia División de Ciencias de la Tierra CICESE Oblique rifts, in which rift margins are oblique to the direction of continental separation, are reasonably common in mo- dern record, e.g. the Red Sea and Gulf of Aden, the Tanganyika-Malawi-Rukwa rifts and the Gulf of California (McKenzie et al., 1970; Rosendhal et al., 1992; Stoke and Hodges, 1989; Manighetti et al., 1998; Nagy and Stock, 2000; Persaud, P., 2003; Persaud, et al., 2003). Although, how the oblique rift evolves is not well known. Oblique rifting remain poorly understand relative to those orthogonal rifts, where the rift margins are approximately perpendicular to the extension direction, and to strike-slip system (Axen and Fletcher, 1998). The Gulf of California is perhaps the best modern example of oblique continental rifting where we can study the pro- cesses of such rifting as they lead to the interplate transfer of a continental fragment. This area presents unique op- portunities for understanding key processes at transtensional plate margins, which is important for energy and mineral exploration, as well as for interpretation of tectonics ancient continental margins (Umhoefer and Dorsey, 1997). One of the main features along the length of the gulf is the fault system which connects active basins (incipient spreading centers) from south to north (Fig 1). Two main structural regions are defined. From the mouth of the gulf to the latitude of the Tiburon and Angel de La Guardia Islands several basins bathymetrically are well expressed, among them; the Pescaderos, Farallon, Carmen, Guaymas, San Pedro Martir and Salsipudes Basins. -
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 ...................................................................................... -
USGS Open-File Report 2010-1333 and CGS SR
Prepared in cooperation with the California Geological Survey; University of Oregon; University of Colorado; University of California, San Diego; and Jet Propulsion Laboratory, California Institute of Technology. Triggered Surface Slips in Southern California Associated with the 2010 El Mayor-Cucapah, Baja California, Mexico, Earthquake SALTON SEA Open-File Report 2010-1333 Jointly published as California Geological Survey Special Report 221 U.S. Department of Interior U.S. Geological Survey COVER Landsat satellite image (LE70390372003084EDC00) showing location of surface slip triggered along faults in the greater Salton Trough area. Red bars show the generalized location of 2010 surface slip along faults in the central Salton Trough and many additional faults in the southwestern section of the Salton Trough. Surface slip in the central Salton Trough shown only where verified in the field; slip in the southwestern section of the Salton Trough shown where verified in the field or inferred from UAVSAR images. Triggered Surface Slips in Southern California Associated with the 2010 El Mayor-Cucapah, Baja California, Mexico, Earthquake By Michael J. Rymer, Jerome A. Treiman, Katherine J. Kendrick, James J. Lienkaemper, Ray J. Weldon, Roger Bilham, Meng Wei, Eric J. Fielding, Janis L. Hernandez, Brian P. E. Olson, Pamela J. Irvine, Nichole Knepprath, Robert R. Sickler, Xiaopeng Tong, and Martin E. Siem Prepared in cooperation with the California Geological Survey; University of Oregon; University of Colorado; University of California, San Diego; and Jet Propulsion Laboratory, California Institute of Technology. Open-File Report 2010–1333 Jointly published as California Geological Survey Special Report 221 U.S. Department of Interior U.S. -
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 Delta in Mexico
Ongoing Restoration Efforts in the Colorado River Delta in Mexico Dr. Francisco Zamora-Arroyo Outline ¾ Conservation Priorities Areas ¾ Restoration Efforts: 9Colorado River 9Hardy River 9Other wetlands ¾ Conclusions CONSERVATION PRIORITIES IN THE - COLORADO RIVER D ELTA MEXICO AND TilE UNITED STATES these and many more organizations and funders are working in several ongoing efforts and initiatives to restore the Delta TCF CONAGUA Secretaria de Turismo David and Lucile Packard Foundation NWF SAGARPA UABC Club de Leones Cucapa Water Education Foundation DHS Rotary Club Results: Map of the Possible A network of 15 Conservation Priority Areas, totaling 850,000 acres that, with proper management, will ensure the long-term persistence of the Delta biodiversity Ongoing restoration efforts in Mexico Restoration = Riparian + Off-channel + Estuarine CATJFORNTA BAJA CALIFORNIA Restoration areas are those needing action to re-establish ecological Protection areas are thosA currAntly in good condition, as they provide critical habitat for spAciAs of Estimated water 2 - 4 m3/s needs 30 - 40 m3/s – 3 meses, 4 años < 2 ppm 3 1.2 - 2 m3/s 4 m /s < 3.5 ppm < 3 ppm 40 - 70 m3/s, 4 meses < 4 ppm Colorado River Corridor Overall goal: Develop a 80,000-acre functional ecological area Restoration Demonstration Project Sitios Demostrativos Poblados Ferrocarril D Sitios Carreteras Laguna Grande • Planted 2,400 native trees in 23 acres in 2006-07: – 1,300 mesquite – 1,100 CW and willow trees Fotos laguna grande Fotos Laguna grnade ESTA ZONA ES PARA QUE .t:t.. QIS Fr\UTE' CUIDALA NO INGRESES E!N VEHICULOS MOTOI\llJ.no, NO TIRES SA.SURA EVITA LA TALA DE AR.BOLES No PROVOQUES INCI:'NDIOS Developed a community vision for restoration Reached over 1,500 local community members and 60 government officials, 20 percent of which participated in restoration actions. -
A Groundwater Model to Assess Water Resource Impacts at the Imperial East Solar Energy Zone
This page intentionally left blank. CONTENTS Notation........................................................................................................................................... v Acknowledgments......................................................................................................................... vii 1 Introduction ................................................................................................................................ 1 1.1 The Bureau of Land Management’s Solar Energy Program ............................................... 2 1.2 The Imperial East Solar Energy Zone ................................................................................. 2 2 Hydrogeologic Setting ................................................................................................................ 5 2.1 Landscape and Aquifer Characteristics .............................................................................. 5 2.2 Water Budget ...................................................................................................................... 5 3 Model Development ................................................................................................................... 9 3.1 Modification of the Tompson et al. (2008) Model ............................................................. 9 3.2 Hydrogeologic Considerations .......................................................................................... 10 3.2.1 Specification of Hydraulic Conductivity ............................................................. -
Genesis of the Quaternary Terraces of the Eastern Sierra El Mayor, Northern Baja California, Mexico
GENESIS OF THE QUATERNARY TERRACES OF THE EASTERN SIERRA EL MAYOR, NORTHERN BAJA CALIFORNIA, MEXICO An Undergraduate Thesis Presented to The Faculty of California State University, Fullerton Department of Geological Sciences In Partial Fulfillment of the Requirements for the Degree Bachelor of Science in Geology By Rene Perez 2003 Phil Armstrong, Faculty Advisor Genesis of the Quaternary Terraces of the Eastern Sierra El Mayor, Northern Baja California, Mexico A Thesis Presented to the Faculty of California State University, Fullerton In Partial Fulfillment of the Requirements for the Degree of Bachelor of Science in Geology By: Rene Perez, Department of Geological Sciences, California State University, Fullerton Thesis Advisor: Dr. Phil Armstrong, Department of Geological Sciences, California State University, Fullerton TABLE OF CONTENTS ABSTRACT....................................................................................................................... 1 INTRODUCTION............................................................................................................... 2 TERRACES AS INDICATORS OF GEOLOGIC ACTIVITY ................................................... 6 REGIONAL GEOLOGY..................................................................................................... 9 Geology of the Sierra Cucapa and Sierra El Mayor ............................................................................9 Faults in the Sierra Cucapa and Sierra El Mayor..............................................................................12