Appendix L, Bureau of Land Management Worksheets
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Wilderness Visitors and Recreation Impacts: Baseline Data Available for Twentieth Century Conditions
United States Department of Agriculture Wilderness Visitors and Forest Service Recreation Impacts: Baseline Rocky Mountain Research Station Data Available for Twentieth General Technical Report RMRS-GTR-117 Century Conditions September 2003 David N. Cole Vita Wright Abstract __________________________________________ Cole, David N.; Wright, Vita. 2003. Wilderness visitors and recreation impacts: baseline data available for twentieth century conditions. Gen. Tech. Rep. RMRS-GTR-117. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 52 p. This report provides an assessment and compilation of recreation-related monitoring data sources across the National Wilderness Preservation System (NWPS). Telephone interviews with managers of all units of the NWPS and a literature search were conducted to locate studies that provide campsite impact data, trail impact data, and information about visitor characteristics. Of the 628 wildernesses that comprised the NWPS in January 2000, 51 percent had baseline campsite data, 9 percent had trail condition data and 24 percent had data on visitor characteristics. Wildernesses managed by the Forest Service and National Park Service were much more likely to have data than wildernesses managed by the Bureau of Land Management and Fish and Wildlife Service. Both unpublished data collected by the management agencies and data published in reports are included. Extensive appendices provide detailed information about available data for every study that we located. These have been organized by wilderness so that it is easy to locate all the information available for each wilderness in the NWPS. Keywords: campsite condition, monitoring, National Wilderness Preservation System, trail condition, visitor characteristics The Authors _______________________________________ David N. -
Iron Mountains Endangered Desert Legacy
Iron Mountains Endangered Desert Legacy Location: The Iron Mountains area is located in the Mojave Desert, in both San Bernardino and Riverside Counties, south of the town of Cadiz. The area is located north of Highway 62, northeast of Joshua Tree National Park, south of the Cadiz Dunes Wilderness and southwest of the Old Woman Mountains Wilderness. The area abuts the eastern side of the Cadiz Valley. Management Agency: Bureau of Land Management, Needles Field Office Description: The terrain includes rugged mountains, playas, sand dunes, bajadas, washes and dozens of other geologic features. The area also contains a portion of Danby Lake (dry). Elevations range from about 600 feet to about 3,200 feet. Wildlife and Plants: The Iron Mountains area is habitat for the endangered desert tortoise, the protected desert bighorn sheep (photo above), and several species on the state watch-list, including the Mojave fringe-toed lizard, hepatic tanager, and prairie falcon. Emory's crucifixion-thorn and Harwood's eriastrum can also be found here. In 1999, a Gila monster was also seen in the area. The California Department of Fish and Wildlife recognizes this area as a wildlife migration corridor, which is an area connecting wildlife populations that have been separated due to human activities. Corridors help avoid inbreeding and may help to re-establish populations that have been reduced or eliminated due to random events such as fire or disease. Desert bighorn sheep have also been found to migrate between the Iron Mountains and the Old Woman Mountains, which can be an important factor in trying to ensure that the species does not die out. -
Pamphlet SIM 3411: Geologic Map of the Castle Rock 7.5' Quadrangle
Geologic Map of the Castle Rock 7.5’ Quadrangle, Arizona and California By P. Kyle House, Barbara E. John, Daniel V. Malmon, Debra Block, L. Sue Beard, Tracey J. Felger, Ryan S. Crow, Jonathan E. Schwing, and Colleen E. Cassidy Pamphlet to accompany Scientific Investigations Map 3411 Kayaker's view of Castle Rock (unit Tac) looking north-northeast from Castle Rock Bay, Arizona. The northern Mohave Mountains are visible in left background, and sediments of the Chemehuevi Formation (unit Qch) are seen along right edge of photo. Photograph taken August 27, 2014, by Kyle House, USGS. 2018 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2018 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. To order USGS information products, visit https://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: House, P.K., John, B.E., Malmon, D.V., Block, Debra, Beard, L.S., Felger, T.J., Crow, R.S., Schwing, J.E., and Cassidy, C.E., 2018, Geologic map of the Castle Rock 7.5’ quadrangle: U.S. -
Chemehuevi Valley Special Recreation Management Area (SRMA)
Chemehuevi Valley Special Recreation Management Area (SRMA) The Chemehuevi Valley Viewshed with the Turtle Mountains National Natural Landmark is directly west of the communities of Havasu Landing, California and Lake Havasu City, Arizona. The Turtle Mountains Natural Landmark is an excellent illustration of volcanic phenomena with superimposed sculpturing of mountain landforms. In combination, the eastern and western sections present some of the finest geological formations in the Mohave Desert. The site is of scenic value and interest; it also contains excellent examples of Mohave Desert flora and fauna. From October to April each year hundreds of travelers “snowbirds” from the northeastern United States, Canada and Europe journey to the area to enjoy the mild winter climate seeking new experiences, enjoying vast landscape which have not existed in European Nations for hundreds of years. Visitors participate in backcountry touring adventure and the discovery of new hiking trails, rock hounding sites and camping opportunities. The Chemehuevi Reservation Havasu Landing Resort depends on the naturalness of the Chemehuevi Valley to support the recreation pursuits of their visitors. The Needles Field Office has developed a system of designated trails entitled the Mojave Adventure Routes in regards to the 2002 Northern and Eastern Colorado Desert Coordinated Management Plan item 3.8.7. These routes are an outstanding network of 4x4 vehicle backcountry touring routes for motorized recreation. These routes were developed for the purpose of traveling to areas not often seen by many people. This network is a shared-use trail system providing recreation opportunities for all persons, including those who use street-legal and non-street legal (Green Sticker) vehicles, hikers, bicyclists, and equestrians. -
Elmer C. Aldrich
PLANNING MILESTONES FOR THE PARK UNITS AND MAJOR PROPERTIES ASSOCIATED WITH THE CALIFORNIA STATE PARKS SYSTEM July 1, 2010 Planning Division California State Parks P. O. Box 942896 Sacramento, CA 94296-0001 PLANNING MILESTONES FOR THE PARK UNITS AND MAJOR PROPERTIES ASSOCIATED WITH THE CALIFORNIA STATE PARK SYSTEM July 1, 2010 OVERVIEW This document is a compendium providing selected information on the classified units and major unclassified properties which currently are or have in the past been associated with the California State Park System. The main purposes of this compendium are to provide, in a single source: 1. a record of the major milestones and achievements in unit-level land use and management planning which have been accomplished through the years by the Department, with the major accomplishments of the last year summarized in Chapter II; 2. a variety of other information useful to understanding the past history or current status of these units and properties, and of the evolution of unit-level land use and resource management planning in the Department; and 3. The definitive number and the specific identity of those basic classified units and major unclassified properties which constitute the official State Park System as of the date of this report’s publication. As of July 1, 2010, the California State Park System consists of 278 basic classified units and major unclassified properties. These are identified on Lists 1 and 2 in Chapter III. To have data current to July 1, 2010, this total will be the Department’s official figure until the next edition of this report. -
Propagation of Native Plants for Restoration Projects in the SW U.S
Propagation of Native Plants for Restoration Projects in the Southwestern U.S. - Preliminary Investigations 1 David R. Dreesen2 and John T. Harrington3 Abstract-Seed treatments to enhance germination capacity of a variety of native tree. shrub. forb. and grass species are reported. Scarification methods including hot water immersion (HW). mechanical scarification (MS). tumble scarification (TS), proximal end cuts (PEC), and sodium hypochlorite (SH) have been tested: Psorothamnus fremontii (HW. TS). Ceanothus integerrimus (HW). Ceanothus sanguineus (HW). Rhus g/abra (HW). Pte/ea trifoliata (PEG of seed separated by size and color). Rubus strigosus (SH), Oryzopsis hymenoides (TS), Co/eogyne ramosissima (TS). and a variety of native woody and herbaceous perennial legume species (HW. TS. MS). Gibberellic acid treatments were examined to overcome endo-dormancy of A/nus tenuifo/ia. A. ob/ongifolia, Rubus strigosus, and Oryzopsis hymenoides. Vegetative propagation methods investigated include mound layering of Platanus wrightii, root propagation of Populus tremu/oides. and pole plantings of riparian understory species (Amorpha fruticosa, Baccharis glutinosa, Forestiera neomexicana. and Chilopsis Iinearis). INTRODUCTION pounded by the scarcity of propagu\es (seed or vegeta tive material) of some species or ecotypes. Restoration ofdisturbed lands in the southwestern U.S. has become a primary mission of many federal and Seed propagation ofnative species often requires state land management agencies and a regulatory growers to rely on information from closely related requirement for extractive industries. Frequently, horticultural species for seed treatment requirements. containerized or bare-root plant materials are used for While this information is useful, many species are reclamation activities following severe disturbance or produced by the horticulture industry because oftheir for introduction ofwoody plant species formerly present ease ofpropagation as well as other horticulturally on poorly managed lands. -
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. -
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. -
Understanding the Source of Water for Selected Springs Within Mojave Trails National Monument, California
ENVIRONMENTAL FORENSICS, 2018 VOL. 19, NO. 2, 99–111 https://doi.org/10.1080/15275922.2018.1448909 Understanding the source of water for selected springs within Mojave Trails National Monument, California Andy Zdon, PG, CHg, CEGa, M. Lee Davisson, PGb and Adam H. Love, Ph.D.c aTechnical Director – Water Resources, PARTNER ENGINEERING AND SCIENCE, INC., Santa Ana, CA, Sacramento, CA; bML Davisson & Associates, Inc., Livermore, CA; cVice President/Principal Scientist, Roux Associates, Inc., Oakland, CA ABSTRACT KEYWORDS While water sources that sustain many of the springs in the Mojave Desert have been poorly Water resources; clipper understood, the desert ecosystem can be highly dependent on such resources. This evaluation mountains; bonanza spring; updates the water resource forensics of Bonanza Spring, the largest spring in the southeastern groundwater; forensics; Mojave Desert. The source of spring flow at Bonanza Spring was evaluated through an integration isotopes of published geologic maps, measured groundwater levels, water quality chemistry, and isotope data compiled from both published sources and new samples collected for water chemistry and isotopic composition. The results indicate that Bonanza Spring has a regional water source, in hydraulic communication with basin fill aquifer systems. Neighboring Lower Bonanza Spring appears to primarily be a downstream manifestation of surfacing water originally discharged from the Bonanza Spring source. Whereas other springs in the area, Hummingbird, Chuckwalla, and Teresa Springs, each appear to be locally sourced as “perched” springs. These conclusions have important implications for managing activities that have the potential to impact the desert ecosystem. Introduction above Bonanza Spring. Identification of future impacts General information and data regarding springs in the from water resource utilization becomes problematic if Mojave Desert are sparse, and many of these springs are initial baseline conditions are unknown or poorly under- not well understood. -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
Newberry/Dead Mountains Scenic Backcountry Drive the 10-Mile One-Way Drive Is on Bureau of Land Management Public Lands
Newberry/Dead Mountains Scenic Backcountry Drive The 10-mile one-way drive is on Bureau of Land Management public lands. However, it is better to take this as a loop trail (see directions) so you don’t have to backtrack and can see other attractions. Although the road is gravel, it is in good condition and can be navigated by 2-wheel drive sedan vehicles, although high clearance is preferable. This particular scenic drive offers a wide range of vistas. Looking north are the Newberry Mountains with the prominent and sacred Spirit Mountain looming above the horizon. Looking south are the Dead Moun- tains which are also sacred to the native Indian tribes in the area. To the west are the granitic crystal hills with interesting rock formations. To the east is the Colorado River Valley and the high peaks of the Hualapai Range in Arizona as backdrop. The green fields along the Colorado River in this area are part of the Fort Mojave Indian Reservation. The Fort Mojave Indian Reservation covers nearly 42,000 acres in the tri-state area of Arizona, California, and Nevada. The Mojave Indians are Pipa Aha Macav — “The People By The River.” Mojave culture traces the earthly origins of its people to Spirit Mountain. Newberry Mountains Newberry Mountains Prior to the arrival of white settler to the region, the Mojave Indians were prosperous farmers with well- established villages and trade networks that stretched as far away as the Pacific Ocean. In the 16th Century, the time the Spanish arrived in the territory, the Mojave’s were the largest concentration of people in the Southwest. -
Miocene Low-Angle Normal Faulting and Dike Emplacement, Homer Mountain and Surrounding Areas, Southeastern California and Southernmost Nevada
Miocene low-angle normal faulting and dike emplacement, Homer Mountain and surrounding areas, southeastern California and southernmost Nevada JON E. SPENCER* U.S. Geological Survey, 345 Middlefleld Road, Menlo Park, California 94025 ABSTRACT tions, differed radically from the state of that collectively accommodated as much as 50% stress in the upper plate, as inferred from to 100% extension of upper-plate rocks (Ander- Homer Mountain and surrounding regions fault geometry. Low-angle faulting and east- son, 1971). In many areas, normal faults within are within, or adjacent to, the western part of northeast-west-southwest distension of up- upper-plate rocks merge with, or are truncated a broad region of low-angle normal faults ex- per-plate rocks reflect regional reduction of by, a basal, subhorizontal fault often referred to posed within the lower Colorado River compression in the east-northeast-west- as a "detachment fault" (for example, see Davis trough. During middle Miocene time, upper- southwest direction and associated large- and others, 1980). The term "detachment fault" plate rocks in the Homer, Sacramento, Dead, scale east-northeast-west-southwest crustal is used here to indicate a low-angle normal fault and Newberry Mountains moved eastward or extension. In contrast, concave-upward flex- that formed at a low angle (for example, Wer- northeastward, relative to the lower plate, ure of the lower plate, in response to tectonic nicke and others, 1984; Reynolds and Spsncer, above single or multiple low-angle normal denudation and resultant isostatic uplift, is in- 1985). The interpretation that detachment faults faults. Deposition of coarse clastic sedimen- ferred to have produced local subhorizontal are rooted faults that accommodate crustal ex- tary rocks occurred during extensional fault- compression at shallow crustal levels in the tension (Wernicke, 1981; Howard and John, ing and was accompanied by, and closely lower plate that overwhelmed the regional 1983; Davis and others, 1983; Allmendinger followed by, eruption of basaltic volcanics.