The Salton Sea Region, California

Total Page:16

File Type:pdf, Size:1020Kb

The Salton Sea Region, California DEPARTMENT OF THE INTERIOR HUBERT WORK, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 497 THE SALTON SEA REGION, CALIFORNIA A GEOGEAPHIC, GEOLOGIC, AND HTDEOLOGIC EECONNAISSANCE WITH A GUIDE TO DESEET WATEEING PLACES BY JOHN S. BROWN Prepared in cooperation with the DEPARTMENT OF ENGINEERING OF THE STATE OF CALIFORNIA WASHINGTON GOVERNMENT PRINTING OFFICE 1923 ADDITIONAL COPIES Or THIS PUBLICATION MAT BE PBOCUBED FROM THE SUPERINTENDENT OV DOCUMENTS GOVEBNMENT PEINTINO OFFICE WASHINQTON, D. C. AT 60 CENTS PER COPY PUECHASEE AQEEES NOT TO EESELL OB DISTRIBUTE THIS COPT FOB PBOFTT. PUB. EES. 57, APPBOVED MAT 11, 1922 n CONTENTS. Fact. Preface, by 0. E. Meinzer................................................ xi Introduction......................... .................................... 1 Methods and scope of work............................................. 1 Acknowledgments.......................................... .......... 2 Oeneral features of the region............................................. 2 Location............................................................. 2 Name................................................................ 2 History.............................................................. 3 Early Spanish exploration and development........................ 3 Later explorations................................................ 4 Gold seekers..................................................... 5 Pacifier Railroad explorations..................................... 5 Colorado River exploration........................................ 6 Old stage roods................................................... 6 Southern Pacific Railroad......................................... 7 Mining................i.......................................... 7 Agriculture..v........................... ............ ............ 7 Imperial Valley.................................................. 9 Early schemes for reclamation................................. 9 Irrigation developments....................................... 10 Engineering problems......................................... 10 Flood dangers of 1905-1907 ................................... 11 Prospects forthe valley....................................... 12 Climate.............................................................. 12 Flora................................................................ 16 Nature of desert flora...............................:............. 16 Vegetation of valleys that contain ground water.................... 17 Vegetation of the detrital ; slopes................................... 18 Mountain vegetation..................................I........... 19 Seasonal changes in vegetation.................................... 19 Fauna............................................. .................. 19 Physiography...................... .................................. 21 Divisions of the region...... ...................................... 21 Peninsular Mountains............................................. 22 Desert basins and ranges.......................................... 23 Salton Basin..................................................... 26 Location and general character................................ 26 Badlands...... .............................................. 26 Sand dunes................................................... 27 Shore lines................................................... 32 Colorado River valley................. .......................... 33 General features.............................................. 33 Causes of stream terraces...................................... 35 Suggested hypothesis for formation of Colorado River terraces.... 36 Drainage............................................................. 40 in IV CONTENTS. General features of the region Continued. Page. Geology............................................................... 41 General rock section.............................................. 42 Pre-Tertiary rocks................................................ 42 Tertiary sedimentary deposits..................................... 44 Tertiary and Quaternary volcanic rocks............................ 47 Quaternary deposits............................................... 47 Structure......................................................... 49 Faulting..................................................... 49 Formation of Salton Basin................................. 49 Faults northeast of Salton Basin........................... 50 San Andreas rift...................................... 50 Indio fault........................................... 50 Faults southwest of Salton Basin........................... 51 Valleys formed by faulting................................ 52 Faults in the desert basins and ranges...................... 53 Typeandageof faulting.................................. 54 Folding and metamorphism................................... 54 Folding and metamorphism in pre-Tertiary rocks, t......... 54 Folding in Tertiary rocks................................. 54 Carrizo Creek and adjacent areas...................... 55 Indio and Mecca hills................................ 55 Volcanic rocks of eastern Imperial County............. 56 Folding in Quaternary beds............................... 56 Igneous structure............................................. 56 Geologic history.................................................. 57 Pre-Quaternary events........................................ 57 Quaternary events............................................ 58 Mineral resources..................................................... 60 Production...................................................... 60 Riverside County ........... ................................ 60 Imperial County............................................. 61 San Diego County............................................ 61 Undeveloped resources........................................... 61 Gold........................................................ 61 Copper ...................................................... 61 Silver and lead............................................... 61 Manganese. .........................................I........ 61 Iron......................................................... 62 Gems........................................................ 62 Salt......................................................... 62 Gypsum..................................................... 62 Strontium ................................................... 62 Clay and stone ............................................... 62 Pumice...................................................... 63 Petroleum. ...................................... ........... 63 Other minerals............................................... 63 Hydrology............................................................... 63 Importance of water supply........................................... 63 Sources of water...................................................... 63 Precipitation..................................................... 63 Colorado River................................................... 64 Ocean water. ............^....................................... 65 CONTENTS. V Hydrology Continued. Page. Occurrence and quality of water....................................... 65 Surface water.................................................... 65 Streams ..................................................... 65 Lakes. ...................................................... 68 Ground water.................................................... 69 General conditions. .......................................... 69 Salton Basin................................................. 73. Coachella Valley......................................... 73 Imperial Valley.......................................... 78 Sand Hills area.......................................... 84 Area northeast of Salton Sea.............................. 85 San Felipe area.......................................... 87 - Coyote Wells area........................................ 90 Western mountain valleys .................................. 91 San Felipe Valley............................!........... 91 Mason Valley............................................ 93 Vallecito Valley.......................................... 94 Carrizo Valley........................................... 95 Borego Valley............................................ 96 Clark Valley............................................. 98 Pleasant Valley.............................................. 98 Pinto Basin.................................................. 99 Blythe Junction Basin........................................ 99 Chuckwalla Valley........................................... 101 Palo Verde Mesa............................................. 108 Arroyo Seco valley and adjacent areas......................... 106 Colorado River valley ........................................ 108 Palo Verde Valley........................................ 108 Yuma Valley............................................. 110 Kinds of desert watering places........................................ 110 Springs and streams............................................... 110 Wells............................................................ Ill Natural tanks .................................................... Ill Artificial reservoirs................................................ Ill Surface indications of water..........................................
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.
    [Show full text]
  • Eagle Crest Energy Gen-Tie and Water Pipeline Environmental
    Eagle Crest Energy Gen-Tie and Water Pipeline Environmental Assessment and Proposed California Desert Conservation Area Plan Amendment BLM Case File No. CACA-054096 BLM-DOI-CA-D060-2016-0017-EA BUREAU OF LAND MANAGEMENT California Desert District 22835 Calle San Juan De Los Lagos Moreno Valley, CA 92553 April 2017 USDOI Bureau of Land Management April 2017Page 2 Eagle Crest Energy Gen-Tie and Water Pipeline EA and Proposed CDCA Plan Amendment United States Department of the Interior BUREAU OF LAND MANAGEMENT California Desert District 22835 Calle San Juan De Los Lagos Moreno Valley, CA 92553 April XX, 2017 Dear Reader: The U.S. Department of the Interior, Bureau of Land Management (BLM) has finalized the Environmental Assessment (EA) for the proposed right-of-way (ROW) and associated California Desert Conservation Area Plan (CDCA) Plan Amendment (PA) for the Eagle Crest Energy Gen- Tie and Water Supply Pipeline (Proposed Action), located in eastern Riverside County, California. The Proposed Action is part of a larger project, the Eagle Mountain Pumped Storage Project (FERC Project), licensed by the Federal Energy Regulatory Commission (FERC) in 2014. The BLM is issuing a Finding of No Significant Impact (FONSI) on the Proposed Action. The FERC Project would be located on approximately 1,150 acres of BLM-managed land and approximately 1,377 acres of private land. Of the 1,150 acres of BLM-managed land, 507 acres are in the 16-mile gen-tie line alignment; 154 acres are in the water supply pipeline alignment and other Proposed Action facilities outside the Central Project Area; and approximately 489 acres are lands within the Central Project Area of the hydropower project.
    [Show full text]
  • California Vegetation Map in Support of the DRECP
    CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California
    [Show full text]
  • The Uranium Deposits of Northeastern Arizona William L
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/24 The uranium deposits of northeastern Arizona William L. Chenoweth and Roger C. Malan, 1973, pp. 139-149 in: Monument Valley (Arizona, Utah and New Mexico), James, H. L.; [ed.], New Mexico Geological Society 24th Annual Fall Field Conference Guidebook, 232 p. This is one of many related papers that were included in the 1973 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • A Window Into Paleocene to Early Eocene Depositional History in Egypt Basedoncoccolithstratigraphy
    The Dababiya Core: A window into Paleocene to Early Eocene depositional history in Egypt basedoncoccolithstratigraphy Marie-Pierre Aubry1 and Rehab Salem1,2 1Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, NJ 08854-8066, USA email: [email protected] 2Geology Department, Faculty of Science, Tanta University, 31527, Tanta, Egypt [email protected] ABSTRACT: The composite Paleocene-lower Eocene Dababiya section recovered in the Dababiya Quarry core and accessible in out- crop in the Dababiya Quarry exhibits an unexpected contrast in thickness between the Lower Eocene succession (~Esna Shales) and the Paleocene one (~Dakhla Shales and Tarawan Chalk). We investigate the significance of this contrast by reviewing calcareous nannofossil stratigraphic studies performed on sections throughout Egypt. We show that a regional pattern occurs, and distinguish six areas—Nile Valley, Eastern Desert and western Sinai, Central and eastern Sinai, northern Egypt and Western Desert. Based on patterns related to thicknesses of selected lithobiostratigraphic intervals and distribution of main stratigraphic gaps, we propose that the differences in the stratigraphic architecture between these regions result from differential latest Paleocene and Early Eocene subsidence following intense Middle to Late Paleocene tectonic activity in the Syrian Arc folds as a result of the closure of the Neo-Tethys. INTRODUCTION view of coccolithophore studies in Egypt since their inception During the Late Cretaceous and Early Paleogene Egypt was (1968). Coccolith-bearing sedimentary rocks as old as part of a vast epicontinental shelf at the edge of the southern Cenomanian outcrop in central Sinai (Thamed area; Bauer et al. Tethys (text-fig. 1). Bounded by the Arabian-Nubian craton to 2001; Faris and Abu Shama 2003).
    [Show full text]
  • Demography of Desert Mule Deer in Southeastern California
    CALIFORNIA FISH AND GAME California Fish and Game 92(2):55-66 2006 DEMOGRAPHY OF DESERT MULE DEER IN SOUTHEASTERN CALIFORNIA JASON P. MARSHAL School of Natural Resources University of Arizona Tucson, AZ 85721 [email protected] LEON M. LESICKA Desert Wildlife Unlimited 4780 Highway 111 Brawley, CA 92227 VERNON C. BLEICH Sierra Nevada Bighorn Sheep Recovery Program California Department of Fish and Game 407 West Line Street Bishop, CA 93514 PAUL R. KRAUSMAN School of Natural Resources University of Arizona Tucson, AZ 85721 GERALD P. MULCAHY California Department of Fish and Game P. O. Box 2160 Blythe, CA 92226 NANCY G. ANDREW California Department of Fish and Game 78-078 Country Club Drive, Suite 109 Bermuda Dunes, CA 92201 Desert mule deer, Odocoileus hemionus eremicus, occur at low densities in the Sonoran Desert of southeastern California and consequently are difficult to monitor using standard wildlife techniques. We used radiocollared deer, remote photography at wildlife water developments (i.e., catchments), and mark-recapture techniques to estimate population abundance and sex and age ratios. Abundance estimates for 1999-2004 ranged from 40 to 106 deer, resulting in density estimates of 0.05-0.13 deer/km2. Ranges in herd composition were 41-74% (females), 6-31% (males), and 6-34% (young). There was a positive correlation (R = 0.73, P = 0.051) between abundance estimates and number of deer photographed/ catchment-day, and that relationship may be useful as an index of abundance in the absence of marked deer for mark-recapture methods. Because of the variable nature of desert wildlife populations, implementing 55 56 CALIFORNIA FISH AND GAME strategies that recognize that variability and conserving the habitat that allow populations to fluctuate naturally will be necessary for long-term conservation.
    [Show full text]
  • B.C.D. 15-23 Employer Status Determination Baja California Railroad, Inc. (BJRR) September 17,2015 This Is the Decision of the R
    B.C.D. 15-23 September 17,2015 Employer Status Determination Baja California Railroad, Inc. (BJRR) BA # 5751 This is the decision of the Railroad Retirement Board regarding the status of Baja California Railroad Inc. (BJRR) as an employer under the Railroad Retirement and Railroad Unemployment Insurance Acts, collectively known as the Acts. The status of this company has not previously been considered. Information regarding BJRR was submitted by the company’s controller—first Ana Laura Tufo and then Manuel Hernandez. Alejandro de la Torre Martinez is the Chief Executive Officer and owns the company along with Fernando Beltran and Fernando Cano. There are no affiliated companies. BJRR has offices in San Diego, California and Tijuana, Mexico. It is a short line operator located in the international border region of San Diego, California and Baja California, Mexico. The BJRR stretches 71 kilometers from the San Ysidro, Califomia-Tijuana, Mexico port of entry to the city of Tecate, Mexico. BJRR interchanges at the San Ysidro rail yard with the San Diego and Imperial Valley Railroad, a covered employer under the Acts (BA No. 3758). BJRR interchanges solely with the San Diego and Imperial Valley Railroad. BJRR runs approximately lA mile in the United States and then goes southbound through customs and into Mexico providing rail freight services to customers from various industries such as gas, construction, food, and manufacturing. All deliveries are made in Mexico. The annual volume is approximately 4,500 carloads of exports to Mexico. Section 1(a)(1) of the Railroad Retirement Act (RRA) (45 U.S.C.
    [Show full text]
  • BLM Worksheets
    10 18 " 13 4 47 ! ! ! 47 " " 11 Piute Valley and Sacramento Mountains 54 " ! ! 87 12 ! 81 " 4 55 61 22 " ! " Pinto Lucerne Valley and Eastern Slopes ! 63 33 " 56 " " " 36 25 Colorado Desert " 20 ! " " 59 37 ! 2 ! 19 " ! 16 19 ! 56 21 " ! ! 15 27 ! 38 Arizona Lake Cahuilla 72 Lake Cahuilla 48 57 " ! ! 57 ! " 34 35 84 ! " 42 76 ! 26 41 ! " 0 5 10 14 58I Miles 28 " " 43 ! ! ! ! 8!9 Existing " Proposed DRECPSubareas 66 62 Colorado Desert Desert Renewable Energy Conservation Plan (DRECP) ACECs within the Colorado Desert Subarea # Proposed ACECs 12 Cadiz Valley Chuckwalla Central 19 (covered in Chuckwalla, see below)) Chuckwalla Extension 20 (covered in Chuckwalla, see below) Chuckwalla Mountains Central 21 (covered in Corn Springs, see below) 22 Chuckwalla to Chemehuevi Tortoise Linkage Joshua Tree to Palen Corridor 33 (covered in Chuckwalla to Chemehuevi Tortoise Linkage) 36 McCoy Valley 37 McCoy Wash 38 Mule McCoy 44 Palen Ford Playa Dunes 48 Picacho Turtle Mountains Corridor 55 (covered in Chuckwalla to Chemehuevi Tortoise Linkage) 56 Upper McCoy # Existing ACECs (within DRECP boundary) 2 Alligator Rock 15 Chuckwalla 16 Chuckwalla Valley Dune Thicket 19 Corn Springs 25 Desert Lily Preserve 56 Mule Mountains 59 Palen Dry Lake 61 Patton's Iron Mountain Divisional Camp 81 Turtle Mountains Cadiz Valley Description/Location: North of Hwy 62, south of Hwy 40 between the Sheep Hole mountains to the west and the Chemehuevi ACEC to the east. Nationally Significant Values: Ecological: The Cadiz Valley contains an enormous variation of Mojave vegetation, from Ajo Lilies to Mojave Yucca. Bighorn, deer and mountain lion easily migrate between basin and range mountains of the Sheephole, Calumet Mountains, Iron Mountains, Kilbeck Hills and Old Woman Mountains with little or no human infrastructure limits.
    [Show full text]
  • Inland Habitat Associations of Marbled Murrelets in British Columbia
    Chapter 16 Inland Habitat Associations of Marbled Murrelets in British Columbia Alan E. Burger1 Abstract: Most Marbled Murrelets (Brachyramphus marmoratus) the greatest threat (Rodway 1990, Rodway and others in British Columbia nest in the Coastal Western Hemlock 1992). The listing stimulated several inland studies, biogeoclimatic zone. In this zone, detection frequencies were highest including reconnaissance surveys in many watersheds of in the moister ecosections and in low elevation forests. Nests and the Queen Charlotte Islands (Rodway and others 1991, moderately high levels of activity were also found in some forest 1993a) and Vancouver Island (Savard and Lemon in press) patches in the subalpine Mountain Hemlock zone. There was no evidence of nesting in subalpine scrub forest, lowland bog forest, and intensive surveys at several sites. or alpine tundra. Studies on the Queen Charlotte Islands and Identification and mapping of potential nesting habitats Vancouver Island reported consistently higher detection frequen- was identified as a high priority for research in the National cies in old-growth than second growth forests (20-120 years old). Recovery Plan for the Marbled Murrelet, prepared by the Detections in second-growth were usually associated with nearby Canadian Marbled Murrelet Recovery Team (Kaiser and patches of old-growth. Within low elevation old-growth, detection others 1994). Detailed 1:50,000 maps of coastal old-growth frequencies were sometimes positively correlated with mean tree forests are being prepared (Derocher, pers. comm.). There diameter, but showed weak or no associations with tree species are still very few data available for either landscape- or composition and minor variations in forest structure.
    [Show full text]
  • Origin of the Sinai-Negev Erg, Egypt and Israel: Mineralogical and Geochemical Evidence for the Importance of the Nile and Sea Level History Daniel R
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- ubP lished Research US Geological Survey 2013 Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R. Muhs U.S. Geological Survey, [email protected] Joel Roskin Ben-Gurion University of the Negev Haim Tsoar Ben-Gurion University of the Negev Gary Skipp U.S. Geological Survey, [email protected] James Budahn U.S. Geological Survey See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Geology Commons, Oceanography and Atmospheric Sciences and Meteorology Commons, Other Earth Sciences Commons, and the Other Environmental Sciences Commons Muhs, Daniel R.; Roskin, Joel; Tsoar, Haim; Skipp, Gary; Budahn, James; Sneh, Amihai; Porat, Naomi; Stanley, Jean-Daniel; Katra, Itzhak; and Blumberg, Dan G., "Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history" (2013). USGS Staff -- Published Research. 931. https://digitalcommons.unl.edu/usgsstaffpub/931 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- ubP lished Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Daniel R. Muhs, Joel Roskin, Haim Tsoar, Gary Skipp, James Budahn, Amihai Sneh, Naomi Porat, Jean-Daniel Stanley, Itzhak Katra, and Dan G. Blumberg This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/usgsstaffpub/931 Quaternary Science Reviews 69 (2013) 28e48 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Origin of the SinaieNegev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history Daniel R.
    [Show full text]
  • Terrestrial Mammal Species of Special Concern in California, Bolster, B.C., Ed., 1998 27
    Terrestrial Mammal Species of Special Concern in California, Bolster, B.C., Ed., 1998 27 California leaf-nosed bat, Macrotus californicus Elizabeth D. Pierson & William E. Rainey Description: Macrotus californicus is one of two phyllostomid species that occur in California. It is a medium sized bat (forearm = 46-52 mm, weight = 12-22 g), with grey pelage and long (>25 mm) ears. It can be distinguished from all other long-eared bats by the presence of a distinct nose leaf, which is erect and lanceolate (Hoffmeister 1986). The only other California species with a leaf-shaped nose projection, Choeronycteris mexicana, has very short ears. Corynorhinus townsendii, the other long-eared species with which M. californicus could most readily be confused, can be distinguished by the presence of bilateral nose lumps as opposed to a single nose leaf. Antrozous pallidus has long ears and a scroll pattern around the nostrils instead of a nose leaf. M. californicus has a tail which extends beyond the edge of the tail membrane by 5-10 mm. Taxonomic Remarks: M. californicus, a member of the Family Phyllostomidae, has sometimes been considered a subspecies of Macrotus waterhousii (Anderson and Nelson 1965), but more recently, based primarily on chromosomal characters, has been treated as a separate species (Davis and Baker 1974, Greenbaum and Baker 1976, Baker 1979, Straney et al. 1979). The form now recognized as M. californicus was first described from a specimen collected at Old Fort Yuma, Imperial County (Baird 1859). There are currently two species recognized in the genus Macrotus (Koopman 1993). Only M. californicus occurs in the United States.
    [Show full text]
  • Imperial County Agriculture Imperial County Overview
    Imperial County Agriculture Fresh market carrots Thinning cantaloupes Field harvesting broccoli Harvesting Wheat Cattle Feedlot Colorado water delivery Field packing 'Sweet Imperial' Field packing of Alfalfa hay bale onions honeydew melons Imperial County Overview The Weather Winters are mild and dry with daily maximum temperatures in the 65 to 75ºF (18-24ºC). Summers are extremely hot with daily maximum temperatures of 104 to 115ºF (40-46ºC). The annual rainfall is just over 3 inches (7.5 cm) with most of it coming in late summer or midwinter. Location & Early History Imperial County is located near the Mexican and Arizona borders in Southern California. In the early 1900's the region was a barren desert. Early developers saw that Colorado River could be diverted to supply irrigation water. By 1915, three hundred thousand acres were under cultivation producing vegetables, agronomic crops and livestock to feed the nation. In 2009, Imperial Valley had 572,286 harvested acres worth $1,045,092,000. Leading crops in the area in 2007 are vegetables (114,099 acres -value $690.3 million, agronomic crops (368,517 acres -value $257 million), livestock (Value $343.2 million) fruit & nuts (5,745 acres -value $47.765 million), seed & nursery (62,237 - value $65.577 million, and apiary products ($3.562 million). The Vegetables Imperial Valley has a well-known reputation for midwinter salad vegetables. Shipments of crisp head lettuce, leaf lettuce, cauliflower, broccoli, and cabbage start in December and continue until March. Asparagus is in- season January, February and March. Carrots are harvested January to June. Spring production of warm-season vegetables starts in late April with the harvest of Sweet Imperial onions, sweet corn, bell pepper, chili peppers, cantaloupes, mixed melons and watermelons.
    [Show full text]