Distribution and Seasonal Movements of Bendire's Thrasher in California
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RIT Projects in Need of Funding (491KB PDF)
3 October 2019 DESERT TORTOISE RECOVERY IMPLEMENTATION STATUS SUMMARY TABLE OF CONTENTS Desert Tortoise Management Oversight Group Recovery Priorities 1 RIT Projects in Need of Funding 1 RIT Project Summaries 7 Top 10 Fencing Recommendations 134 Funded RIT Projects 16 DESERT TORTOISE MANAGEMENT OVERSIGHT GROUP RECOVERY PRIORITIES ● Restore habitat (incl. route restoration) ● Reduce predator subsidies ● Targeted predator control ● Install and maintain tortoise barrier fencing ● Fire management planning and implementation ● Education (lower priority than on-the-ground actions) RIT PROJECTS IN NEED OF FUNDING Project Priority Title Budget # Rangewide RW02 Seed Increases for Desert Tortoise Habitat Restoration in Southern Nevada $140,000 California RIT - Rangewide Mojave Raven Watch - a desert tortoise rangewide human education CA09 $126,500 program Removal of free-roaming burros on BLM managed land in excess of CA41 $2,465,000 authorized population level. California RIT - Northeast Mojave Workgroup Ivanpah Critical Habitat Unit (see also CA41) -7.4%/year Increase law enforcement patrols for desert tortoise protection in Mojave CA19 $259,000 National Preserve. CA26 Evaluation of raven food subsidy sites near the Mojave National Preserve $82,133 Fenner Critical Habitat Unit (see also CA19, CA26, and CA41) -7.3%/year CA25. Piosphere Restoration on the Fenner/Piute Valley Critical Habitat Unit in $209,250 v2 Mojave National Preserve CA30 Desert Tortoise Barrier Fencing: Interstate 40 near Kelbaker Road $543,500 Rd 5 Rd7 Fence US 95 Nevada border -
Mammals of the California Desert
MAMMALS OF THE CALIFORNIA DESERT William F. Laudenslayer, Jr. Karen Boyer Buckingham Theodore A. Rado INTRODUCTION I ,+! The desert lands of southern California (Figure 1) support a rich variety of wildlife, of which mammals comprise an important element. Of the 19 living orders of mammals known in the world i- *- loday, nine are represented in the California desert15. Ninety-seven mammal species are known to t ':i he in this area. The southwestern United States has a larger number of mammal subspecies than my other continental area of comparable size (Hall 1981). This high degree of subspeciation, which f I;, ; leads to the development of new species, seems to be due to the great variation in topography, , , elevation, temperature, soils, and isolation caused by natural barriers. The order Rodentia may be k., 2:' , considered the most successful of the mammalian taxa in the desert; it is represented by 48 species Lc - occupying a wide variety of habitats. Bats comprise the second largest contingent of species. Of the 97 mammal species, 48 are found throughout the desert; the remaining 49 occur peripherally, with many restricted to the bordering mountain ranges or the Colorado River Valley. Four of the 97 I ?$ are non-native, having been introduced into the California desert. These are the Virginia opossum, ' >% Rocky Mountain mule deer, horse, and burro. Table 1 lists the desert mammals and their range 1 ;>?-axurrence as well as their current status of endangerment as determined by the U.S. fish and $' Wildlife Service (USWS 1989, 1990) and the California Department of Fish and Game (Calif. -
Recruitment of Desert Tortoises (Gopherus Agassizii and G
Herpetological Conservation and Biology 10(2):583–591. Submitted: 29 September 2014; Accepted: 7 April 2015; Published: 31 August 2015. RECRUITMENT OF DESERT TORTOISES (GOPHERUS AGASSIZII AND G. MORAFKAI): A SYNTHESIS OF REPRODUCTION AND FIRST-YEAR SURVIVAL STEVEN P. CAMPBELL1,2,3, ROBERT J. STEIDL1, AND ERIN R. ZYLSTRA1 1School of Natural Resources and the Environment, University of Arizona, Tucson, Arizona 85721, USA 2Albany Pine Bush Preserve Commission, Albany, New York 12205, USA 3Corresponding author, email: [email protected] Abstract.—Recruitment is integral to population persistence, therefore characterizing this process is essential for evaluating recovery actions for species in decline. We gathered all data available and used Bayesian analyses to quantify annual recruitment of Mojave Desert (Gopherus agassizii) and Sonoran Desert (G. morafkai) tortoises as the product of four components: proportion of females that reproduced, number of eggs produced per reproducing female, hatching success, and hatchling survival. For Mojave Desert Tortoises, the estimated proportion of females that reproduced (0.81 [95% Credible Interval: 0.52–0.99]) and number of eggs produced per year (6.90 [5.51–8.16]) were higher than for Sonoran Desert Tortoises (0.52 [0.07–0.94] and 5.17 [3.05–7.60], respectively). For Mojave Desert Tortoises, hatching success averaged 0.61 (0.25–0.90). Data on hatching success for Sonoran Desert Tortoises and hatchling survival for both species were sparse, therefore we represented these components with a range of plausible values. When we combined components, average recruitment for Mojave Desert Tortoises ranged from 0.51 females/female/y assuming that hatchling survival was 0.30 to 1.18 females/female/y with hatchling survival assumed to be 0.70. -
28 September 2020 Desert Tortoise Management Oversight Group
28 September 2020 DESERT TORTOISE RECOVERY IMPLEMENTATION STATUS SUMMARY TABLE OF CONTENTS Desert Tortoise Management Oversight Group Recovery Priorities 1 RIT Projects in Need of Funding 1 RIT Project Summaries 6 Top Fencing Recommendations 14 Funded RIT Projects 16 DESERT TORTOISE MANAGEMENT OVERSIGHT GROUP RECOVERY PRIORITIES ● Restore habitat (incl. route restoration) ● Reduce predator subsidies ● Targeted predator control ● Install and maintain tortoise barrier fencing ● Fire management planning and implementation ● Education (lower priority than on-the-ground actions) RIT PROJECTS IN NEED OF FUNDING Desert tortoise population trends through 2014 are indicated for geographic areas covered by the range-wide monitoring program Project Priority Title Budget # Rangewide RW02 Seed Increases for Desert Tortoise Habitat Restoration in Southern Nevada $140,000 California RIT - Rangewide Mojave Raven Watch - a desert tortoise rangewide human education CA09 $126,500 program Removal of free-roaming burros on BLM managed land in excess of CA41 $2,465,000 authorized population level. Identification of existing culverts and underpasses needing maintenance or CA42 modification to facilitate desert tortoise movement under highways and $48,000 roads. Rd8 Fence I-40 north of Black Ridge, CA, both sides, 5.0 miles TBD Rd11 Fence I-40 near Old Dad Mountains, both sides, 9.4 miles TBD Rd13 Fence I-40 near Kalbaker Rd, 8.1 miles TBD California RIT - Northeast Mojave Workgroup Ivanpah Critical Habitat Unit (see also CA41) -7.4%/year Increase law enforcement patrols for desert tortoise protection in Mojave CA19 $259,000 National Preserve. CA26 Evaluation of raven food subsidy sites near the Mojave National Preserve $82,133 Fenner Critical Habitat Unit (see also CA19, CA26, and CA41) -7.3%/year CA25. -
The Imperial Valley Is Located About 150 Miles Southeast of Los Angeles
The Imperial Valley is located about 150 miles southeast of Los Angeles. It is a section of a much larger geologic structure -- the Salton Trough -- which is about 1,000 miles in length. The structure extends from San Gorgonio Pass southeast to the Mexican border, including the Gulf of California and beyond the tip of the Baja California Peninsula. The surrounding mountains are largely faulted blocks of the Southern California batholith of Mesozoic age, overlain by fragments of an earlier metamorphic complex. The valley basin consists of a sedimentary fill of sands and gravels ranging up to 15,000 feet in thickness. The layers slope gently down-valley, and contain several important aquifers. The valley is laced with major members of the San Andreas Fault system. Minor to moderate earthquake events are common, but severe shocks have not been experienced in recorded history. The entire trough, including the Gulf is an extension of the East Pacific Rise, a zone of separation in Earth's crust. Deep sea submergence instruments have observed many phenomena of crustal formation. The axis of the Rise, hence of the Salton Valley as well, is a great transform fault that is having the effect of separating an enormous slab of North America, consisting of the Baja Peninsula and coastal California away from the mainland, with movement to the northwest and out to sea as a terranne. Table of Contents Chapter 1 The San Jacinto and Santa Rosa Mountains Chapter 2 The Eastern Mountains Chapter 3 San Gorgonio Pass Chapter 4 The Hills Chapter 5 Desert Sand -
Chemehuevi Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Chemehuevi Valley Groundwater Basin Bulletin 118 Chemehuevi Valley Groundwater Basin • Groundwater Basin Number: 7-43 • County: San Bernardino • Surface Area: 273,000 acres (427 square miles) Basin Boundaries and Hydrology This basin underlies Chemehuevi Valley in eastern San Bernardino County. The basin is bounded by Havasu Lake on the east and by nonwater-bearing rocks of the Sacramento Mountains on the north, of the Chemehuevi Mountains on the northeast, of the Whipple Mountains on the southeast, of the Turtle Mountains on the west and south (Bishop 1963). The valley is drained by Chemehuevi Wash to Havasu Lake. Annual average precipitation ranges from about 4 to 6 inches. Hydrogeologic Information Water Bearing Formations Groundwater in the basin is found in alluvium and the Bouse Formation. Alluvium. Holocene age younger alluvium, which is found in washes and the floodplain of the Colorado River, is composed of sand, silt and gravel (Metzger and Loeltz 1973). Older alluvium consists of unconsolidated, fine- to coarse-grained sand, pebbles, and boulders with variable amounts of silt and clay. Bouse Formation. The Pliocene age Bouse Formation is composed of a basal limestone bed overlain by interbedded clay, silt, and sand. Thickness of the formation reaches 254 feet (Metzger and Loeltz 1973). The formation is underlain by locally derived fanglomerate and overlain by alluviums of the Colorado River and its tributaries. Restrictive Structures An unnamed fault crosses a portion of the southern side of the basin (Bishop 1963), but it is not known whether or not this fault impedes groundwater flow in the basin. -
Forwards DOI Request for LLNL Tritium Tests at Ward Valley
- _ . - . - - . .. -_. - .. - - - * . March 19, 1996 NOTE T0: X. Stablein J. Austin ; C. Paperiello M. Bell ' J. Greeves J. Holonich M. Federline B. Reamer M. Weber C. Cameron P. Lohaus J. Kennedy P. Sobel FROM: Nelson,[[[ SUBJECT: DOE STAFF POSITION ON DOI REQUEST FOR LLNL TRITIUM TESTS AT WARD ! VALLEY ! The attached staff position paper was provided to us by Terry Plummer, ! DOE, last week and is forwarded FYI. ; Attachment: As stated | | l, i l ! ! 1 ! t l' 970 g;g,60pe, - 1 - , - - . - - - - - - 4 , ' . I 1 * , . i. > !. 4 DEPARTMENT OF THE INTERIOR REQUEST FOR LAWRENCE LIVERMORE NATIONAL LABORA'IORY i 70 i PERFORM TRTITUM TF.STS AT WARD VALLEY, CALIFORNIA | f FACTS / BACKGROUND , i - On February 23,1996, John Garamendi, Deputy Secretary of the Depiu unent of the Interior, requested the participation of the De,partment of Energy in contracting with the Lawrence i Livermore National Laboratory to perform tntium tests at the State licensed low-level radioactive waste (LLW) disposal facility in Ward Valley, Califomia. * On Demhn 15,1995, Secretary O' leary denied a similar request dated June 8,1995, : from Senator Boxer, (D-CA). 'Ihe Secretary stated that,"We believe the State of California, in its ! licensing role as authorized by the Nuclear Regulatory Commission, should determine how to implement the National Academy of Sciences' recommendations. If the State Mermines that further testing is needed based on analytical services unique to the Departmw of Energy, we will consider such a request." l ! + In response to an earlier request of Senator Boxer, Secretary Babbitt asked the National ! Academy of Sciences (NAS) to examine several key safety related issues of the site. -
Rice Valley Groundwater Basin Bulletin 118
Colorado River Hydrologic Region California’s Groundwater Rice Valley Groundwater Basin Bulletin 118 Rice Valley Groundwater Basin • Groundwater Basin Number: 7-4 • County: Riverside, San Bernardino • Surface Area: 189,000 acres (295 square miles) Basin Boundaries and Hydrology This groundwater basin underlies Rice Valley in northeast Riverside and southeast San Bernardino Counties. Elevation of the valley floor ranges from about 675 feet above sea level near the center of the valley to about 1,000 feet along the outer margins. The basin is bounded by nonwater- bearing rocks of the Turtle Mountains on the north, the Little Maria and Big Maria Mountains on the south, the Arica Mountains on the west, and by the West Riverside and Riverside Mountains on the east. Low-lying alluvial drainage divides form a portion of the basin boundaries on the northwest and northeast, and the Colorado River bounds a portion of the basin on the east. Maximum elevations of the surrounding mountains range to about 2,000 feet in the Arica Mountains, about 3,000 feet in the Big Maria Mountains, and 5,866 feet at Horn Peak in the Turtle Mountains (Bishop 1963; Jennings 1967; USGS 1971a, 1971b, 1983a, 1983b, 1983c). Annual average precipitation ranges from about 3 to 5 inches. Surface runoff from the mountains drains towards the center of the valley, except in the eastern part of the valley, where Big Wash drains to the Colorado River (USGS 1971a, 1971b, 1983a, 1983b, 1983c). Hydrogeologic Information Water Bearing Formations Alluvium is the water-bearing material that forms the basin and includes unconsolidated Holocene age deposits and underlying unconsolidated to semi-consolidated Pleistocene deposits (DWR 1954, 1963). -
San Bernardino & Inyo Counties, California
BLM-California Old Spanish National Historic Trail Recreation & Development Strategy San Bernardino & Inyo Counties, California—September, 2015 14 Old Spanish National Historic Trail Recreation & Development Strategy Department of the Interior Bureau of Land Management Utah State Office Prepared For: The Bureau of Land Management, Barstow Field Office The Old Spanish Trail Association Prepared By: Michael Knight, BLM, ACE Landscape Architect Intern Graydon Bascom, BLM, ACE Historic Trails Intern September, 2015 Contents Note to the Reader 1 Participants 2 Explanation of Document Sections 3 Project Overview Old Spanish Trail Map 7 Recreation Route Map 9 Typical Trail Elements 11 Trail Zone Details Cajon Junction to Barstow (Zone 1) 15 Barstow to Harvard Rd (Zone 2) 19 Harvard Rd to Salt Creek (Zone 3) 27 Zzyzx to Piute Gorge (Zone 4) 31 Salt Creek to California State Line (Zone 5) 37 Summary 41 Above: Old Spanish Trail Marker at Emigrant Pass Cover Page: Top photo: Salt Creek ACEC, Bottom Photo: Mouth of Spanish Canyon looking southwest Note To The Reader National Historic Trails are trails that have a historical significance to the nation, and can only be designated by an act of Congress. There are currently 19 National Historic Trails in the United States. In 1968, the National Trails System Act, which is intended to provide for the outdoor recreation needs of the public, opened the door to federal involvement in all types of trails. Today, the Bureau of Land Management, along with the National Park Service and National Forest Service, are responsible for the administration and management of National Historic Trails. -
Lanfair Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Lanfair Valley Groundwater Basin Bulletin 118 Lanfair Valley Groundwater Basin • Groundwater Basin Number: 7-1 • County: San Bernardino • Surface Area: 157,000 acres (245 square miles) Basin Boundaries and Hydrology This basin underlies Lanfair Valley in eastern San Bernardino County. The valley slopes southeasterly with valley floor elevations ranging from 3,500 to 5,000 feet above sea level. The basin is bounded by impermeable rocks of the New York and Castle Mountains on the north, of the Piute Range on the east, of the Hackberry Mountain on the south, and of the Providence Mountains and Mid Hills on the west. Caruthers Creek flows intermittently southeastward during periods of heavy precipitation. Piute Spring discharges groundwater from Lanfair Valley to an adjacent valley and other smaller springs are found throughout the valley. Average annual precipitation ranges from 7 to 10 inches. Hydrogeologic Description Water Bearing Formations The primary water-bearing formations are Quaternary and Tertiary age unconsolidated deposits that include highly indurated sand, silt, clay and gravel. The maximum thickness of these deposits is not known; however, a boring log indicates a thickness of at least 550 feet locally. Wells in these deposits yield about 3 to 70 gpm (Friewald 1984). Restrictive Structures The Cedar Canyon fault crosses the northwest portion of the basin; however, it is unknown whether or not this fault is a barrier to groundwater. Recharge Areas The principal sources of recharge are likely percolation of runoff from surrounding mountains, percolation of precipitation to the valley floor, and subsurface inflow from adjacent basins. -
Regional Assessment for Desert Stateline
REGIONAL ASSESSMENT STATELINE SOLAR FARM PROJECT BLM CASE FILE NUMBER CACA-48669 Prepared for: Prepared by: Desert Stateline, LLC NatureServe 525 Market Street 4600 North Fairfax Drive 15th Floor 7th Floor San Francisco, California 94105 Arlington, Virginia 22203 Date: 27 July 2012 Cover photo credit: Geoffrey Hammerson NatureServe Project Team Mary Harkness Patrick Crist Conservation Planner/Project Manager Director, Conservation Planning and Ecosystem Management Ian Varley Jacquie Bow Conservation Planner GIS Analyst Jon Hak Geoffrey Hammerson Ecologist/Senior GIS Analyst Research Zoologist Suzanne Young Conservation Biologist and Data Analyst Suggested citation: NatureServe. 2012. Regional assessment: Stateline solar farm project. Technical report prepared for Desert Stateline, LLC. NatureServe, Arlington, VA. Regional Assessment: Stateline Solar Farm Project Page 2 of 94 1 Introduction .......................................................................................................................................... 8 1.1 Purpose and overview of assessment ........................................................................................... 8 1.2 Assessment approach ................................................................................................................... 8 1.3 Assessment areas and context ...................................................................................................... 8 1.3.1 Ivanpah Valley Watershed ................................................................................................... -
Mojave National Preserve Management Plan for Developed
Mojave National Preserve—Management Plan for Developed Water Resources CHAPTER 3: AFFECTED ENVIRONMENT Introduction This chapter describes the unique factors that influence water resource management in the Preserve and the resources that could be affected by the implementation of any of the alternatives described in Chapter 2: Alternatives. The resource descriptions provided in this chapter serve as a baseline to compare the potential effects of the management actions proposed in the alternatives. The following resource topics are described in this chapter: • Environmental Setting • Cultural Resources • Water Resources • Wilderness Character • Wildlife Environmental setting and water resources are important for context and are foundational for water resource management, but are not resources that are analyzed for effects. Resource issues that were considered and dismissed from further analysis are listed in Chapter 1: Purpose of and Need for Action and are not discussed further in this EA. A description of the effects of the proposed alternatives on wildlife, cultural resources, and wilderness character is presented in Chapter 4: Environmental Consequences. Environmental Setting The Preserve includes an ecologically diverse yet fragile desert ecosystem consisting of vegetative attributes that are unique to the Mojave Desert, as well as components of the Great Basin and Sonoran Deserts. Topography The topography of the Preserve is characteristic of the mountain and basin physiographic pattern, with tall mountain ranges separated by corresponding valleys filled with alluvial sediments. Primary mountain ranges in the Preserve, from west to east, include the Granite, Kelso, Providence, Clark, New York, and Piute Mountains. Major alluvial valleys include Soda Lake (dry lake bed), Shadow Valley, Ivanpah Valley, Lanfair Valley, and Fenner Valley.