USGS Open-File Report 2010-1333 and CGS SR
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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. -
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. -
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. -
GEOPHYSICAL STUDY of the SALTON TROUGH of Soutllern CALIFORNIA
GEOPHYSICAL STUDY OF THE SALTON TROUGH OF SOUTllERN CALIFORNIA Thesis by Shawn Biehler In Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy California Institute of Technology Pasadena. California 1964 (Su bm i t t ed Ma Y 7, l 964) PLEASE NOTE: Figures are not original copy. 11 These pages tend to "curl • Very small print on several. Filmed in the best possible way. UNIVERSITY MICROFILMS, INC. i i ACKNOWLEDGMENTS The author gratefully acknowledges Frank Press and Clarence R. Allen for their advice and suggestions through out this entire study. Robert L. Kovach kindly made avail able all of this Qravity and seismic data in the Colorado Delta region. G. P. Woo11ard supplied regional gravity maps of southern California and Arizona. Martin F. Kane made available his terrain correction program. c. w. Jenn ings released prel imlnary field maps of the San Bernardino ct11u Ni::eule::> quad1-angles. c. E. Co1-bato supplied information on the gravimeter calibration loop. The oil companies of California supplied helpful infor mation on thelr wells and released somA QAnphysical data. The Standard Oil Company of California supplied a grant-In- a l d for the s e i sm i c f i e l d work • I am i ndebt e d to Drs Luc i en La Coste of La Coste and Romberg for supplying the underwater gravimeter, and to Aerial Control, Inc. and Paclf ic Air Industries for the use of their Tellurometers. A.Ibrahim and L. Teng assisted with the seismic field program. am especially indebted to Elaine E. -
Coachella Valley Water Management Plan 2010 Update
COACHELLA VALLEY WATER MANAGEMENT PLAN 2010 UPDATE Final Report January 2012 Prepared for: Coachella Valley Water District Steve Robbins General Manager-Chief Engineer Patti Reyes Planning and Special Program Manager Prepared by: MWH 618 Michillinda Ave., Suite 200 Arcadia, CA 91007 Water Consult 535 North Garfield Avenue Loveland, CO 80537 Table of Contents Section Name Page Number Executive Summary ................................................................................................................ ES-1 ES-1 The Coachella Valley ...............................................................................................ES-1 ES-2 Water Management in the Coachella Valley ...........................................................ES-3 ES-3 Current Condition of Coachella Valley Groundwater Basin ...................................ES-4 ES-4 The 2002 Water Management Plan..........................................................................ES-5 ES-4.1 Goals and Objectives ......................................................................................ES-5 ES-4.2 Accomplishments Since 2002 .........................................................................ES-6 ES-5 2010 WMP Update ................................................................................................ES-13 ES-5.1 Population and Water Demand .....................................................................ES-13 ES-5.2 Future Water Supply Needs ..........................................................................ES-16 ES-5.3 What -
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 -
Imperial Irrigation District Final EIS/EIR
Final Environmental Impact Report/ Environmental Impact Statement Imperial Irrigation District Water Conservation and Transfer Project VOLUME 2 of 6 (Section 3.3—Section 9.23) See Volume 1 for Table of Contents Prepared for Bureau of Reclamation Imperial Irrigation District October 2002 155 Grand Avenue Suite 1000 Oakland, CA 94612 SECTION 3.3 Geology and Soils 3.3 GEOLOGY AND SOILS 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. -
Sedimentation and Deformation in a Pliocene–Pleistocene Transtensional Supradetachment Basin, Laguna Salada, North-West Mexico R
Basin Research (1999) 11, 205–221 Sedimentation and deformation in a Pliocene–Pleistocene transtensional supradetachment basin, Laguna Salada, north-west Mexico R. Dorsey* and A. Martı´n-Barajas† Department of Geological Sciences, 1272 University of Oregon, Eugene, OR 97403–1272, USA †Departamento de Geologı´a, Centro de Investigacio´ n Cientı´fica y de Educacio´ n Superior de Ensenada, Baja California, Mexico ABSTRACT This study examines a thick section of Pliocene–Pleistocene sedimentary rocks exposed in the footwall of an active normal fault (Can˜on Rojo fault) near its intersection with the dextral- normal Laguna Salada fault in north-western Mexico. These rocks are situated in the upper plate of an inactive strand of the Can˜ada David detachment fault, which is cut on the north- east by the Laguna Salada fault. The stratigraphy is divided into three unconformity-bounded sequences: (1) marine mudstone of the Pliocene Imperial Formation; (2) nonmarine Pliocene– Pleistocene redbeds, consisting of sedimentary breccia, conglomerate, conglomeratic sandstone (all un-named) and fine-grained sandstone and mudstone of the Palm Spring Formation; and (3) uncemented Pleistocene boulder gravel. Coarse deposits of the redbeds sequence were deposited in fault-bounded, high- and low-gradient alluvial fans that passed laterally into a low-energy fluvial plain of the ancestral Colorado River (Palm Spring Formation) which occupied the present-day Laguna Salada. Detailed mapping reveals convergence and lap-out of bedding surfaces in the redbeds sequence onto the west limb of a large anticline cored by Imperial Formation. These geometries, combined with fanning dips and thickening of stratigraphy into the flanking syncline, indicate that the anticline grew during deposition of the redbeds. -
Imperial County Multi-Jurisdiction Hazard Mitigation Plan Update April
Ju IMPERIAL COUNTY M ULTI-JURISDICTION AZARD ITIGATION H M PLAN UPDATE APRIL 2014 Imperial County Multi-Jurisdictional Hazard Mitigation Plan Update April 2014 Adoption by Local Governing Body: §201.6(c)(5) County of Imperial RESOLUTION OF THE COUTY OF IMPERIAL BOARD OF SUPERVISORS ADOPTING THE IMPERIAL COUNTY MULTI-JURISDICTION HAZARD MITIGATION PLAN UPDATE RESOLUTION NO. __________ WHEREAS, the Disaster Mitigation Act of 2000 requires all jurisdictions to be covered by a Pre- Disaster All Hazards Mitigation Plan to be eligible for Federal Emergency Management Agency pre- and post-disaster mitigation funds; and WHEREAS, the County of Imperial recognizes that no community is immune from natural, technological or domestic security hazards, whether it be earthquake, flood, severe winter weather, drought, heat wave, wildfire or dam failure related; and recognizes the importance of enhancing its ability to withstand hazards as well as the importance of reducing human suffering, property damage, interruption of public services and economic losses caused by those hazards; and WHEREAS, the Federal Emergency Management Agency and California Office of Emergency Services have developed a hazards mitigation program that assists communities in their efforts to become Disaster-Resistant Communities that focus, not just on disaster response and recovery, but also on preparedness and hazard mitigation, which enhances economic sustainability, environmental stability and social well-being; and WHEREAS, Imperial County fully participated in the Federal -
How to Save the Salton Sea: Proposal to Import Seawater Across California Desert Is Biggest Since Hoover Dam California's Salton Sea Has Been Drying up for Years
How to save the Salton Sea: Proposal to import seawater across California desert is biggest since Hoover Dam California's Salton Sea has been drying up for years. Can the proposed infrastructure projects help save it? 4:14 pm UTC Jun. 11, 2021 Time is running out to come up with a plan to save the Salton Sea. Water levels in California's largest lake continue to drop, subjecting nearby communities to harmful levels of toxic dust stirred up from the dry, exposed lakebed. For more than a century, the shallow lake has been a beneficiary of the Colorado River water that feeds the nearby Imperial Valley farm fields. As water was sold off and diverted, more than 15,000 acres of lakebed containing years of fertilizer and pesticide runoff were exposed to the air and desert winds. The dwindling water supply increases the lake's salinity, killing off fish, destroying once-lush migratory bird habitats and making children sick from the airborne toxins stirred up in the dust. Kaylee Pineda, a child living in Westmorland, Calif. speaks about her experiences with asthma Many of the players on Kaylee’s Little League team have asthma. The coach says he watches his asthmatic players and is prepared to respond if any of them start gasping for air. Zoë Meyers, Palm Springs Desert Sun The California Natural Resources Agency was tasked with coming up with a long-term fix by the end of 2022, and 11 plans on the table focus mainly on one big idea: pulling in water across the U.S.-Mexican border from the Sea of Cortez north to the Salton Sea. -
Response to Comments, Part 17
Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-277 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-278 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-279 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-280 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-281 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-282 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-283 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-284 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-285 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-286 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California 3-287 Final Programmatic Environmental Impact Report, Imperial County Renewable Energy and Transmission Element Update Imperial County, California Response to Comment Letter #22: Cal Energy Operating Corporation Comment 22-1: Thank you for your comments on the Imperial County General Plan Renewable Energy and Transmission Element Update, Implementation Ordinance, and Draft PEIR. We have provided responses to your specific comments on each of the documents below. -
Salinity and Fish Effects on Salton Sea Invertebrates
qqj SALINITY AND FISH EFFECTS ON SALTON SEA INVERTEBRATES : A MICROCOSM EXPERIMENT r A Thesis Presented to the Faculty of San Diego State University In Partial Fulfillment of the Requirements for the Degree Master of Science in Biology by Cheryl M . Hart Spring 1994 THE UNDERSIGNED FACULTY COMMITTEE APPROVES THE THESIS OF CHERYL M . HART Stuart H . Huribert SAN DIEGO STATE UNIVERSITY SPRING 1994 III TABLE OF CONTENTS PAGE LIST OF TABLES vi LIST OF FIGURES viii INTRODUCTION 1 METHODS 7 Experimental Design 7 Establishment Of Microcosms And Salinity Levels 7 Inoculation Of Tanks 12 Fish Introductions 13 Sampling Methods And Regimes 15 Sample Analysis And Data Analysis 16 RESULTS 19 Salinity And Temperature 19 Effects Of Salinity 19 Crustaceans 19 Trichocorixa 26 Rotifers 27 Protozoans 28 Nematodes 29 Polychaetes 29 Total Invertebrates 29 iv PAGE Taxonomic Composition 30 Effects Of Tilapia 30 Correlations Among Taxa 33 DISCUSSION 36 The Microcosm Foodweb 36 Gammanis And Salinity 39 Invertebrate Predator-Prey Interactions 40 Competitive Interactions 42 Fish And Community Structure 43 Ecological Change At The Salton Sea 44 CONCLUSIONS 46 ACKNOWLEDGEMENTS 47 LITERATURE CITED 48 APPENDICES 55 A. INOCULATION OF TANKS 56 B. FISH WEIGHTS/LENGTHS AND DATES OF PLACEMENT INTO THE TANKS 58 C. COUNT DATA FOR INDIVIDUAL TAXA AT FIVE SALINITIES 60 D. BIOVOLUME DATA FOR INDIVIDUAL TAXA AT FIVE SALINITIES 78 E. COUNT DATA AFTER FISH INTRODUCTIONS AT TWO SALINITIES 85 V PAGE F. BIOVOLUME DATA AFTER FISH INTRODUCTIONS AT TWO SALINITIES 96 ABSTRACT 100 vi LIST OF TABLES TABLE PAGE 1 . The Amounts Of Each Ion Added To The Diluted Salton Sea Water And The Total Salts Added In Order To Achieve An Increase Of 8 .84 g/L 10 VII LIST OF FIGURES FIGURE PAGE 1 .