DOCSLIB.ORG

±305 AC Harper Lake, CA

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
±305 AC Harper Lake, CA Solar Energy Development Potential ±305 AC Harper Lake, CA Luz Solar Power Plant Harper Lake Abengoa Mojave Solar Power Plant 305 AC SITE Potential Uses: Garlock Mars • RENEWABLE ENERGY Randsburg Copper City • Industrial Storage Mojave Base • Manufacturing • Warehousing 395 • Distribution Center Harper Highlights: Aerial Acres Lake • 230 kV “Kramer/Coolwater” Transmission Lockhart 58 Boron Line Adjacent 58 Hinkley 15 • Flat Ready to Build Kramer Hills Yermo Barstow • Highways 58/ 395 – I -15 and I - 40 Close Daggett 58 • Assessor’s Parcel Number 0490-121-26 395 • San Bernardino Thomas Guide Page 349 A7 15 247 Helendale Offering Price Below Market: Call Broker For more information: No warranty, express or implied, is made as to the accuracy of the information contained herein. This information is submitted subject to errors, omissions, change of price, rental or other conditions, withdrawal without notice, and is subject to any special Scott Lisk, Senior Vice President listing conditions imposed by our principals. Cooperating brokers, buyers, tenants and other parties who receive this document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the 951.346.0805 • [email protected] information contained herein through a due diligence review of the books, records, files and documents that constitute reliable sources of the information described herein. Logos are for identification purposes only and may be trademarks of their respective Cal BRE #00574287 companies. NAI Capital, Inc. CA BRE Lic. #01990696. Solar Energy Development Potential ±305 AC Harper Lake, CA Property Summary This site is located approximately nine miles northwest of the town of Hinkley in unincorporated San Bernardino County, approximately halfway between the city of Barstow and the community of Kramer Junction (Highway 395 / Highway 58 junction). The property has frontage on the south side of Lockhart Ranch Road +/- 1 mile west of Harper Lake Road approximately twenty miles west of Barstow, approximately six miles north of the intersection of Harper Lake Road at Highway 58. The Southern California Edison Company’s Kramer-Cool Water 230-kV transmission line “POWER LINE ROAD” is located adjacent to the southern border of the site. A potential use for this site would be a solar energy production plant like the existing Solar Electric Generating Stations (SEGS) VIII and IX facilities, owned by NextEra™ Energy Resources just north the property. The adjoining property owner, ABENGOA MOJAVE SOLAR has built one of the worlds largest solar parabolic trough technology electric generating facilities on their property. This site could also be used for many different types of uses including Materials Production Plants connected with the Solar Industry. The county wants the area to develop and will support almost any type of proposed Industrial Development plan. They will consider many other uses including Industrial Uses, Farming, Mining, Distribution Facilities, etc. The owners understand the current economic conditions and will respond to all offers. Items such as price, due diligence/ feasibility period, escrow periods are all negotiable. Offering price "REDUCED" to ±$2,500.00/Acre. For more information: No warranty, express or implied, is made as to the accuracy of the information contained herein. This information is submitted subject to errors, omissions, change of price, rental or other conditions, withdrawal without notice, and is subject to any special Scott Lisk, Senior Vice President listing conditions imposed by our principals. Cooperating brokers, buyers, tenants and other parties who receive this document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the 951.346.0805 • [email protected] information contained herein through a due diligence review of the books, records, files and documents that constitute reliable sources of the information described herein. Logos are for identification purposes only and may be trademarks of their respective Cal BRE #00574287 companies. NAI Capital, Inc. CA BRE Lic. #01990696. Solar Energy Development Potential ±305 AC Harper Lake, CA Location Map Inyokern 178 Ridgecrest Valjean Renoville 14 395 Garlock Mars Randsburg Copper City Cantil Mojave Base Fort Irwin Baker 15 Zzyzx California City Harper Aerial Acres Lake 58 Lockhart Afton Crucero Boron 15 Manix 58 Hinkley Edwards AFB Kramer Hills Yermo Barstow Daggett Newberry 395 Springs 58 15 Pisgah Helendale Lavic Ludlow Lancaster 247 Ragtown Lake Los Angeles Victorville Littlerock 18 Apply Valley 138 Lucerne Johnson Phelan Hesperia Valley Valley Wrightwood 247 Angeles National Forest 138 Landers 15 Big Bear Lake 18 Desert Heights 215 210 Pioneertown 62 210 San Bernardino Yucca Valley Ontario For more information: No warranty, express or implied, is made as to the accuracy of the information contained herein. This information is submitted subject to errors, omissions, change of price, rental or other conditions, withdrawal without notice, and is subject to any special Scott Lisk, Senior Vice President listing conditions imposed by our principals. Cooperating brokers, buyers, tenants and other parties who receive this document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the 951.346.0805 • [email protected] information contained herein through a due diligence review of the books, records, files and documents that constitute reliable sources of the information described herein. Logos are for identification purposes only and may be trademarks of their respective Cal BRE #00574287 companies. NAI Capital, Inc. CA BRE Lic. #01990696. Solar Energy Development Potential ±305 AC Harper Lake, CA Solar Energy Development Potential Existing Energy CorridorsApprox. 305 Acres Near Barstow, CA EXISTING ENERGY CORRIDORS 305 ac Scott Lisk 2280 Market St. For more information: Senior Vice President Suite 150 No warranty,951 346 express 0800 or implied, is made as to the accuracyRiverside, of the information CA contained 92501 herein. This information is submitted subject to errors, omissions, change of price, rental or other conditions, withdrawal without notice, and is subject to any special Scott Lisk, Senior Vice President [email protected] conditions imposed by our principals. Cooperating Faxbrokers, 951 buyers, 346 tenants 0801 and other parties who receive this document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the 951.346.0805 • [email protected] informationDRE containedLic. #00574287 herein through a due diligence reviewwww.naicapital.com of the books, records, files and documents that constitute reliable sources of the information described herein. Logos are for identification purposes only and may be trademarks of their respective No warranty, express or implied, isCal made asBRE to the accuracy #00574287 of the information contained herein. This information is submitted subject to errors, omissions, changecompanies. of price, rental NAI or Capital, other conditions, Inc. CA BRE withdrawal Lic. #01990696. without notice, and is subject to any special listing conditions imposed by our principals. Cooperating brokers, buyers, tenants and other parties who receive this document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the information contained herein through a due diligence review of the books, records, files and documents that constitute reliable sources of the information described herein. Solar Energy Development Potential Solar Energy Development±305 AC Harper Potential Lake, CA Approx. 305 Acres Near Barstow, CA ASSESORS’Assesor’s PARCEL Parcel MAP Map Scott Lisk 2280 Market St. For more information: Senior Vice President Suite 150 No warranty, express or implied, is951 made as346 to the 0800 accuracy of the information contained herein.Riverside, This information CA is submitted 92501 subject to errors, omissions, change of price, rental or other conditions, withdrawal without notice, and is subject to any special Scott Lisk, Senior Vice President listing conditions imposed by our [email protected] Cooperating brokers, buyers, tenants and other Faxparties who951 receive 346 this 0801document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the 951.346.0805 • [email protected] information contained herein through a due diligence review of the books, records, files andwww.naicapital.com documents that constitute reliable sources of the information describedDRE herein. Lic.Logos are#00574287 for identification purposes only and may be trademarks of their respective Cal BRE #00574287 companies. NAI Capital, Inc. CA BRE Lic. #01990696. No warranty, express or implied, is made as to the accuracy of the information contained herein. This information is submitted subject to errors, omissions, change of price, rental or other conditions, withdrawal without notice, and is subject to any special listing conditions imposed by our principals. Cooperating brokers, buyers, tenants and other parties who receive this document should not rely on it, but should use it as a starting point of analysis, and should independently confirm the accuracy of the information contained herein through a due diligence
Load more

Recommended publications
  • Harper Valley Groundwater Basin Bulletin 118
    South Lahontan Hydrologic Region California’s Groundwater Harper Valley Groundwater Basin Bulletin 118 Harper Valley Groundwater Basin • Groundwater Basin Number: 6-47 • County: Kern, San Bernardino • Surface Area: 410,000 acres (640 square miles) Basin Boundaries and Hydrology This groundwater basin underlies Harper Valley in western San Bernardino and eastern Kern Counties of the central Mojave Desert. This basin is bounded on the east by nonwater-bearing rocks of Fremont Peak, Black Mountain, the Gravel Hills, and the Mud Hills. The basin is bounded on the west by a combination of surface drainage divides, portions of the Harper, Kramer Hills and Lockhart faults, and nonwater-bearing rocks of the Kramer Hills and other low-lying basement hills. The basin is bounded on the south by nonwater-bearing rocks of Mount General, Iron Mountain, and the Waterman Hills, and by subsurface drainage patterns. The basin is bounded on the north by nonwater-bearing rocks of the Rand Mountains (DWR 1964; Jennings and others 1962; Rogers 1967) Harper Valley is drained by numerous ephemeral streams towards Harper (dry) Lake (Jennings and others 1962; Rogers 1967). Floodwater from Grass Valley occasionally flows into Harper Valley via Black Canyon on the eastern side of the valley (DWR 1964). Average annual precipitation is about 5 inches and ranges from about 3 to 7 inches. Hydrogeologic Information Water Bearing Formations Quaternary lacustrine and alluvial deposits, including unconsolidated younger alluvial fan material and unconsolidated to semi-consolidated older alluvium, can be water-bearing within the basin. The younger alluvium generally lies above the groundwater surface; whereas, the older alluvium extends beneath the groundwater table (DWR 1971).
    [Show full text]
  • Jay Von Werlhof Imperial Valley College Desert Museum El Centro, California
    DISTRIBUTION AS A FUNCTIONAL FACTOR OF ROCK ALIGNMENTS IN THE MOJAVE DESERT Jay Von Werlhof Imperial Valley College Desert Museum El Centro, California ABSTRACT This paper suggests that the distribution, setting, content, and form of early rock alignments in the Mojave Desert are directly related to the function of these features. Each of these factors will be described and discussed in turn, leading to an interpretive synthesis. Why a reliable model cannot be developed for locating rock alignment sites is also suggested. I am pleased to have been invited to present a paper in this noted also that a few isolated sites are uniquely present, which session honoring Dee Simpson. I have admired her life-long is another concern of research. Such sites, for example, might devotion to archaeology and the tenacity with which she works have been in the process of being developed into larger and toward goal completions. I am also indebted to her, along more complex sites but were never completed, as possibly that with Arda Haenzel, her co-worker at the San Bernardino at Lavic Lake (MacDonald 1993). Also, in complex sites con­ County Museum, for interesting me in earthen art back in taining numerous designs it is not clear whether the diverse el­ 1975 when few others thought that path worth treading. Since ements are even temporally related, or if each design exists as then, I have worked to advance the study of geogylphs and rock an entity from a different era. However, this type of earthen art alignments, and the paper I am presenting today is drawn appears to have been the earliest, and its association with the around a small sector of that study: distribution as a functional Lake Hill Pleistocene site (Davis 1978) focuses the Panamint factor of rock alignments in the Mojave Desert.
    [Show full text]
  • Harper Family on the Shore for Was Living in Warmth
    TThhee LLoouuiissvvii llllee HHiissttoorriiaann A Publication of the Louisville Historical Museum, Issue #105 Louisville History Foundation, and Louisville Historical Commission Winter 2015 The Harpers and Harper Lake: How One Family Left Its Mark on Louisville, Colorado By Bridget Bacon, Museum Coordinator arper Lake, located at what is today called the what is now Harper Lake, before the town of Louisville H Leon A. Wurl Wildlife Sanctuary, has long been a was established in 1878 and even before Colorado place for recreation in Louisville. People now in their became a state in 1876. seventies, eighties, and nineties who were born between around 1915 and 1940 well remember trekking as young John H. Harper, who was born in Scotland in 1825 and people from their homes in downtown Louisville all the died in Colorado in 1874, served as mayor of Denver for way up to Harper Lake for ice skating and hockey games a term in 1871-1872, and his purchase of land in our area in the winter and swimming in the summer. They for farming and potentially coal mining by the early remember that the lake, which was smaller and 1870s is one of several examples of Colorado’s “movers shallower then, would stay frozen all winter. and shakers” of the late 1800s casting their eyes to eastern Boulder The only equipment County for the that a boy needed investment back then for a game opportunities that of hockey was a pair they saw. of ice skates, since the hockey sticks John H. Harper came were typically to the United States fashioned from tree at the age of eight branches and the with his family.
    [Show full text]
  • Draft DRECP and EIR/EIS – Appendix L, Bureau of Land Management Worksheets
    Harper Dry Lake Description/Location: Harper Dry Lake is a year‐round marsh and wetland utilized by a variety of resident and migratory bird species, as well as a watchable wildlife area for viewing these species. It is located within and along the southwestern border of Harper Lake playa in San Bernardino County, approximately twenty miles northwest of Barstow off of Harper Lake Road. Nationally Significant Values: Ecological: Harper Dry Lake is recognized as a Key Raptor Area by the BLM, which designated 223 areas nationwide. Key Raptor Areas are places known to be significant habitats for selected species of birds of prey, and Harper Dry Lake is 1 of 7 Key Raptor Areas in the California desert. The species known to utilize the habitat at Harper Dry Lake are northern harrier, short‐eared owl, ferruginous hawk, and long‐eared owl. Special Designations/Management Plan/Date: This ACEC was designated in the CDCA Plan of 1980, and the management plan was approved in June of 1982, and later in 2006, additional management provisions were incorporated in the plan. Relevance and Importance Criteria: Relevant biological resources. Before early settlement and adjacent agricultural activities, this playa possessed a shallow water table feeding a productive meadowland habitat. At that time, surface water flowed in the Mojave River throughout the year in much of the West Mojave and spring flows were frequent. With the advent of ranching and later agriculture, much of the Harper Lake meadowland was degraded, and with additional populations and dams, Mojave River flow has been substantially reduced and flows down river of the Victor Valley area are infrequent.
    [Show full text]
  • Appendix D Mojave River Exhibit
    APPENDIX D MOJAVE RIVER EXHIBIT Floor Unit The floor unit will be a free-standing, three dimensional representation of the Mojave River and adjacent lands. Pleistocene lakes and present day features will be labeled. See Figure 1. Four horizontal panels will be attached to the floor unit. Two large vertical panels will be adjacent to the floor unit. One will be the modified existing panel on Afton Canyon and Pleistocene Lake Manix. Figure 1. Map For Floor Unit (after Automobile Club of Southern California, 2002; Reheis, et al, 2015). D-1 Panels Adjacent to Floor Unit The four panels mounted on the sides of the floor unit will contain addition information about subjects related to the Mojave Desert, both during the Pleistocene and Holocene. The four panels going clockwise from the top of the exhibit will discuss thermoregulation by the shasta ground sloth (Nothrotheriops shastensis), eolian activity, the flood plain aquifer, and gold processing. Each panel will contain text and diagrams. Free Standing Panels The existing panel with information on Afton Canyon and Lake Manix is shown in figure 2. The heading will be changed to "The Mojave: the River that Grew in Your Own Backyard". Otherwise, it will be unchanged. The text of the existing panel is difficult to read in Figure 2; its text is given below: Afton Canyon: During the later part of the Pleistocene Epoch, Lake Manix extended eastwards as far as Cave Mountain and the Cady Mountains, just west of Soda Lake. After approximately 21,000 years ago, as the last glacial pulse of the Ice Ages was waning, Lake Manix overtopped its eastern threshold and catastrophically drained to the east, forming a new lake - Pleistocene Lake Mojave.
    [Show full text]
  • Land Subsidence in the Southwestern Mojave Desert, California, 1992–2009 in Cooperation with the Mojave Water Agency (MWA), the U.S
    Land Subsidence in the Southwestern Mojave Desert, California, 1992–2009 In cooperation with the Mojave Water Agency (MWA), the U.S. Geological Survey (USGS) has been monitoring land subsidence in the southwestern Mojave Desert of California using satellite Interferometric Synthetic Aperture Radar (InSAR) combined with ground-based techniques. Maps of land subsidence constructed from the InSAR data have proven to be an economical means to evaluate subsidence—with the goal of identifying small problems before they become large ones. The maps of subsidence over the considerably large (nearly 5,000 square miles [mi2]) MWA management area (fig. 1) enabled researchers to detect small magnitude, localized areas of subsidence near five lakebeds. Introduction and Background integrated with results from other USGS/ MWA cooperative groundwater studies into the broader scoped USGS Mojave Groundwater has been the primary source of domestic, Groundwater Resources Web site (http://ca.water.usgs.gov/ agricultural, and municipal water supplies in the southwestern mojave/). This fact sheet combines the detailed analyses from the Mojave Desert, California, since the early 1900s. Increased three subsidence reports, distills them into a longer-term context, demands on water supplies have caused groundwater-level and provides an assessment of options for future monitoring. declines of more than 100 feet (ft) in some areas of this desert (fig. 2 inset) between the 1950s and the 1990s (Stamos and others, 2001; Sneed and others, 2003). These water-level InSAR Reveals Localized Subsidence near Dry Lakebeds declines have caused the aquifer system to compact, resulting InSAR data and field observations reveal land subsidence in land subsidence.
    [Show full text]
  • Data and Water-Table Map of the Mojave River Ground-Water Basin
    U.S. Department of the Interior Prepared in cooperation with the Water-Resources Investigations Report 95-4148 Stamos, C.L. and Predmore S.K., 1995, Data and U.S. Geological Survey MOJAVE WATER AGENCY Water-Table map of the Mojave River Ground-Water basin, San Bernardino County, California, November 1992 Introduction Water-table Map R 8 W R 7 W R 6 W R 5 W R 4 W R 3 W R 2 W R 1 W R 1 E R 2 E R 3 E R 4 E R 5 E Table 1. Water-level measurements, 1990-94, in the Mojave River ground-water basin. [State well No.: See "Well-Numbering System" section; some numbers subject to change upon verification. USGS identification Number. consists of latitude, longitude, and sequence number. Altitude of The Mojave River Basin is located about 80 mi northeast of Los Angeles, California. The proxim- The water-table map was constructed using U.S. Geological Survey water-level measurements 15 7D1 water level and altitude of surface in feet above sea level. Water level (depth) in feet below land surface. State well No.: Asterisk (*) indicates multiple-well completion site drilled as part of this study. ity of the Mojave River Basin to the highly urbanized Los Angeles region has led to a rapid from approximately 300 wells and additional water-level measurements reported by local water Measurement method: S, steel tape; R, reported by other agencies; V, calibrated electric tape. --, no data. Site status: F, flowing; R, recently pumped; S nearby pumping; T, nearby recent pumping] 1,980 CoyoteCoyote Lake Dry growth in population and, consequently, an increase in the demand for water.
    [Show full text]
  • Surficial Geologic Map and Geodatabase of the Cuddeback Lake 30' X 60' Quadrangle, San Bernardino and Kern Counties, California
    Surficial Geologic Map and Geodatabase of the Cuddeback Lake 30' x 60' Quadrangle, San Bernardino and Kern Counties, California By Lee Amoroso and David M Miller Pamphlet to accompany Open-file Report 2006-1276 2006 U.S. Department of the Interior U.S. Geological Survey 2 Surficial geologic map and geodatabase of the Cuddeback Lake 30’ x 60’ quadrangle, California Abstract A USGS surficial geologic mapping project, focused on the arid Southwest USA, conducted mapping and process studies to investigate landscape development and tectonic evolution. This project included the Cuddeback Lake 1:100,000-scale quadrangle located in the western Mojave Desert north-northeast of Los Angeles, between the southern Sierra Nevada and San Bernardino Mountains, in Kern and San Bernardino Counties, California. Geomorphic features include high-relief mountains, small hills, volcanic domes, pediments, broad alluvial valleys, and dry lakes. The mapped area includes pre-Tertiary plutonic, metavolcanic, metasedimentary, and other metamorphic rocks; Tertiary sedimentary and volcanic rocks; and Quaternary sediments and basalts. Included in the area are the El Paso, Lockhart, Blackwater, and Muroc faults as well as the central segment of the Garlock fault zone. The tectonically active western Mojave Desert and the variety of surficial materials have resulted in distinctive geomorphic features and terrains. Geologic mapping has shown that active faults are widespread and have influenced drainage patterns. The tectonically active area near the Garlock fault zone and the nearby El Paso fault influenced development of drainage networks; base level is controlled by fault offset. There is evidence of a late Tertiary drainage network preserved in remnants of alluvial fans and paleo-drainage deposits north of the El Paso Mountains, west of the Lava Mountains, and south and west of the Rand Mountains.
    [Show full text]
  • Pluvial Lakes in the Great Basin of the Western United States-A View From
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/262806093 Pluvial lakes in the Great Basin of the western United States—a view from the outcrop Article in Quaternary Science Reviews · August 2014 DOI: 10.1016/j.quascirev.2014.04.012 CITATIONS READS 28 172 4 authors, including: Marith C. Reheis United States Geological Survey 119 PUBLICATIONS 3,485 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: fun in retirement! View project Tephrochronology Project View project All content following this page was uploaded by Marith C. Reheis on 26 April 2016. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Quaternary Science Reviews 97 (2014) 33e57 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Pluvial lakes in the Great Basin of the western United Statesda view from the outcrop Marith C. Reheis a,*, Kenneth D. Adams b, Charles G. Oviatt c, Steven N. Bacon b a U.S. Geological Survey, MS-980, Federal Center Box 25046, Denver, CO 80225, USA b Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512, USA c Department of Geology, Kansas State University, 108 Thompson Hall, Manhattan, KS 66506, USA article info abstract Article history: Paleo-lakes in the western United States provide geomorphic and hydrologic records of climate and Received 1 March 2013 drainage-basin change at multiple time scales extending back to the Miocene.
    [Show full text]
  • COMPLIANCE7-03-00, Mojave Solar Project 2019 Annual Compliance Report (09-AFC-5C) Part 1
    DOCKETED Docket Number: 09-AFC-05C Project Title: Abengoa Mojave Compliance TN #: 232295 COMPLIANCE7-03-00, Mojave Solar Project 2019 Annual Document Title: Compliance Report (09-AFC-5C) part 1 COMPLIANCE7-03-00, Mojave Solar Project 2019 Annual Description: Compliance Report (09-AFC-5C) part 1 Filer: Jose Manuel Bravo Romero Organization: Mojave Solar Project Submitter Role: Applicant Submission Date: 3/4/2020 7:46:58 AM Docketed Date: 3/4/2020 Mojave Solar LLC 42134 Harper Lake Road Phone: 760 308 0400 Hinkley, California 92347 SUBMITTED ELECTRONICALLY Subject: 09-AFC-5C Condition Number: Compliance 7 Description: Mojave Solar Project 2019 Annual Compliance Report Submittal Number: COMPLIANCE7-03-00 Distribution: Keith Winstead, CEC; Kara Harris, US DOE; Dr. Sharma Shankar CDFW; Ray Bransfield, USFWS; Thomas Dietsch, USFWS February 2, 2020 Keith Winstead Compliance Project Manager California Energy Commission 1516 Ninth Street, MS-2000 Sacramento, CA 95814 [email protected] Dear Mr. Winstead, The attached Mojave Solar Project 2019 Annual Compliance Report (09-AFC-5C) is submitted for your review as part of the ongoing reporting required by the California Energy Commission’s Conditions of Certification for the Mojave Solar Project. Sincerely, Jose Manuel Bravo Romero Manager Compliance, Permitting, Quality and Environment Department ASI Operations LLC Mojave Solar Project 42134 Harper Lake Rd Hinkley, CA 92347 (303) 378-7302 MPDQXHOEUDYR#DWODQWLFD\LHOGFRP Attachment: 09-AFC-5C Mojave Solar Project 2019 Annual Compliance Report. 09-AFC-5C Mojave Solar Project Annual Compliance Report 2019 reporting period Prepared by: AS Industrial Operations LLC . for Mojave Solar LLC 42134 Harper Lake Road Hinkley, California 92347 Mojave Solar LLC 42134 Harper Lake Road Phone: 760 308 0400 Hinkley, California 92347 Subject: 09-AFC-5C Condition Number: COMPLIANCE-7 Description: Annual Compliance Report – 2019.
    [Show full text]
  • Appendix a Subject-Specific Document Timelines for the Centro
    Appendix A Subject-Specific Document Timelines for the Centro and Baja Subareas Mojave River Hydrology and Upstream Dams Ungaged Local Mountain Runoff Harper Lake Area Riparian Vegetation and Water Demand Key Technical Reports of Mojave River Hydrology and Upstream Dams Year 1960 DWR, 1964, Determination of Underflow at the Cedar Springs Damsite, July. 1965 USACE, 1966, Design Memorandum No. 2, General Design for Mojave River Forks Reservoir, October. SBC Flood Control Dsitrict, 1968, The Mojave River and the Forks Dam, May. USGS, Hardt, 1969, Mojave River Basin Ground-Water Recharge-Floods of January and February 1969, Open-File Report. USACE, 1970, Information Pamphlet on Mojave River Forks Reservoir, June. 1970 Cedar Springs Dam and Mojave River Dam completed - Summer 1971 USGS, Hardt, 1971, Hydrologic Analysis of Mojave River Basin, CA, Using Electric Analog Model. Open-File Report, August. USGS, Durbin and Hardt, 1974, Hydrologic Analysis of the Mojave River, CA 1975 using a Mathematical Model, WRIR 17-74. Bookman Edmonston, 1978, Report on Analysis of Releases from Lake Silverwood in Satisfaction of Prior Downstream Rights, May 5. USGS, Buono and Lang, 1980, Aquifer Recharge from the 1969 and 1978 Floods 1980 in the Mojave River Basin, CA, WRIR 80-207. USACE, 1981, Preliminary Study, Modifications to Mojave Dam, Mojave River, July. MWA, 1983, Historic and Present Conditions, Helendale to Calico-Newberry Fault, December. 1985 1990 Hanson, J.C., 1993, Analysis of the Flow of the Mojave River at Afton, CA, February. Prepared for MWA. 1995 USGS, Lines, 1996, Ground-Water and Surface-Water Relations along the Mojave River, Southern California, WRIR 95-4189.
    [Show full text]
  • Changes in the Water Budget of the Mojave and the Drying out of the Southwest: New Constraints from the Study of Ancient Deposits
    Changes in the water budget of the Mojave and the drying out of the Southwest: New constraints from the study of ancient deposits John Mering, UCLA Department of Earth and Space Science During the next several centuries, anthropogenic global warming is expected to result in aridification in mid- latitude desert regions such as the Southwestern United States, further reducing hydrologic budgets (Wetherald and Manabe, 2002). In the Mojave region of Eastern California this is problematic, where surface and groundwater resources are already overdrawn to sustain population centers and agriculture. In order to accurately model potential aridification in the Mojave, a thorough understanding of regional climate history is essential. Specifically data on past variability in temperature and hydrology can be used to study regional climate processes and assess the accuracy of computer models. I propose to apply new geochemical methods to deposits from sites in the Mojave in order to study the regional climate history and establish the magnitude of change in summertime temperature, and in the source(s) of moisture in the region, to changing greenhouse gas forcing. Data from paleolakes (Fig. 1) have been used to develop climate reconstructions for the Pleistocene, including the Last Glacial Maximum (LGM) interval, 23,000 to 19,000 years before present (Lyle et al., 2012). Many workers have hypothesized a southward shift of the Polar Jet Stream during this time as major sources for precipitation feeding lakes in eastern and southern California at that time, with aridification being driven by the jet shifting northwards and a resultant decrease in winter storms (Oviatt, 1999; Reheis et al., 2012).
    [Show full text]