Appendix F Cultural Resources Assessment
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County of Riverside General Plan San Jacinto Valley Area Plan
County of Riverside General Plan San Jacinto Valley Area Plan COUNTY OF RIVERSIDE Transportation and Land Management Agency 4080 Lemon Street, 12th Floor Riverside, CA 92501-3634 Phone: (951) 955-3200, Fax: (951) 955-1811 October 2011 Page i County of Riverside General Plan San Jacinto Valley Area Plan TABLE OF CONTENTS Vision Summary.......................................................................................................................................................... iv Introduction ................................................................................................................................................................. 1 A Special Note on Implementing the Vision ........................................................................................................ 2 Location ........................................................................................................................................................................ 3 Features ........................................................................................................................................................................ 7 Setting ....................................................................................................................................................................... 7 Unique Features ........................................................................................................................................................ 7 San Jacinto River ................................................................................................................................................ -
The History of Valentine Camp by Mary Farrell
History of Valentine Camp Mary M. Farrell Trans-Sierran Archaeological Research P.O. Box 840 Lone Pine, CA 93545 November 7, 2015 Prepared for Valentine Eastern Sierra Reserve University of California, Santa Barbara, Natural Reserve System Sierra Nevada Aquatic Research Laboratory 1016 Mt. Morrison Road Mammoth Lakes, CA 93546 Abstract Located in Mammoth Lakes, California, Valentine Camp and the nearby Sierra Nevada Aquatic Research Laboratory form the Valentine Eastern Sierra Reserve, a field research station in the University of California's Natural Reserve System. The University’s tenure at Valentine Camp began over 40 years ago, but the area’s history goes back thousands of years. Before the arrival of Euroamericans in the nineteenth century, the region was home to Paiutes and other Native American tribes. Land just east of Valentine Camp was surveyed under contract with the United States government in 1856, and mineral deposits in the mountains just west of Valentine Camp brought hundreds of miners to the vicinity in the last decades of the nineteenth century. Even as mining in the region waned, grazing increased. The land that became Valentine Camp was patented in 1897 by Thomas Williams, a rancher and capitalist who lived in Owens Valley. It was Williams’s son, also Thomas, who sold the 160 acres to Valentine Camp’s founders. Those founders were very wealthy, very influential men in southern California who could have, and did, vacation wherever they wanted. Anyone familiar with the natural beauty of Mammoth Lakes would not be surprised that they chose to spend time at Valentine Camp. Valentine Camp was donated to the University of California Natural Land and Water Reserve System (now the Natural Reserve System) in 1972 to ensure the land’s continued protection. -
Santa Rosa and San Jacinto Mountains National Monument Act of 2000
SANTA ROSA AND SAN JACINTO MOUNTAINS NATIONAL MONUMENT ACT OF 2000 Public Law 106-351 106th Congress An Act To establish the Santa Rosa and San Jacinto Mountains National Monument in the State of California. <<NOTE: Oct. 24, 2000 - [H.R. 3676]>> Be it enacted by the Senate and House of Representatives of the United States of America in Congress assembled, <<NOTE: Santa Rosa and San Jacinto Mountains National Monument Act of 2000. 16 USC 431 note.>> SECTION 1. SHORT TITLE; TABLE OF CONTENTS. (a) Short Title.--This Act may be cited as the ``Santa Rosa and San Jacinto Mountains National Monument Act of 2000''. (b) Table of Contents.--The table of contents of this Act is as follows: Sec. 1. Short title; table of contents. Sec. 2. Establishment of Santa Rosa and San Jacinto Mountains National Monument, California. Sec. 3. Management of Federal lands in the National Monument. Sec. 4. Development of management plan. Sec. 5. Existing and historical uses of Federal lands included in Monument. Sec. 6. Acquisition of land. Sec. 7. Local advisory committee. Sec. 8. Authorization of appropriations. SEC. 2. ESTABLISHMENT OF SANTA ROSA AND SAN JACINTO MOUNTAINS NATIONAL MONUMENT, CALIFORNIA. (a) Findings.--Congress finds the following: (1) The Santa Rosa and San Jacinto Mountains in southern California contain nationally significant biological, cultural, recreational, geological, educational, and scientific values. (2) The magnificent vistas, wildlife, land forms, and natural and cultural resources of these mountains occupy a unique and challenging position given their proximity to highly urbanized areas of the Coachella Valley. (3) These mountains, which rise abruptly from the desert floor to an elevation of 10,802 feet, provide a picturesque backdrop for Coachella Valley communities and support an abundance of recreational opportunities that are an important regional economic resource. -
UNIVERSITY of CALIFORNIA Los Angeles Southern California
UNIVERSITY OF CALIFORNIA Los Angeles Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geography by Katherine Colby Glover 2016 © Copyright by Katherine Colby Glover 2016 ABSTRACT OF THE DISSERTATION Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains by Katherine Colby Glover Doctor of Philosophy in Geography University of California, Los Angeles, 2016 Professor Glen Michael MacDonald, Chair Long sediment records from offshore and terrestrial basins in California show a history of vegetation and climatic change since the last interglacial (130,000 years BP). Vegetation sensitive to temperature and hydroclimatic change tended to be basin-specific, though the expansion of shrubs and herbs universally signalled arid conditions, and landscpe conversion to steppe. Multi-proxy analyses were conducted on two cores from the Big Bear Valley in the San Bernardino Mountains to reconstruct a 125,000-year history for alpine southern California, at the transition between mediterranean alpine forest and Mojave desert. Age control was based upon radiocarbon and luminescence dating. Loss-on-ignition, magnetic susceptibility, grain size, x-ray fluorescence, pollen, biogenic silica, and charcoal analyses showed that the paleoclimate of the San Bernardino Mountains was highly subject to globally pervasive forcing mechanisms that register in northern hemispheric oceans. Primary productivity in Baldwin Lake during most of its ii history showed a strong correlation to historic fluctuations in local summer solar radiation values. -
Chapter 9 Geology Soils and Seismicity
Chapter 9—Geology, Soils, and Seismicity 9.1 Introduction This chapter describes the existing conditions (environmental and regulatory) and assesses the potential of the 2016 Metropolitan Transportation Plan/Sustainable Communities Strategy (proposed MTP/SCS) to affect the regional geology, seismicity, soils, and mineral resources within the MTP/SCS plan area. This chapter evaluates potential impacts to geology, seismicity, soils, and mineral resources that may result from implementation of the proposed MTP/SCS. Where necessary and feasible, mitigation measures are identified to reduce these impacts. The information presented in this chapter is based on a review of existing and available information and is regional in scope. Data provided in this section is programmatic. It is appropriate for general policy planning and tiering of subsequent environmental documents; however site-specific evaluations may be necessary to determine future project-level environmental effects and appropriate mitigation. No comments regarding geology, soils, and seismicity were received during circulation of the Notice of Preparation (NOP). Appendix PD-1 includes all NOP comments received. 9.2 Environmental Setting 9.2.1 Geology and Topography This section addresses the geology and topography of the proposed MTP/SCS plan area. Figure 9.1 provides a geologic map of the SACOG region. The proposed MTP/SCS plan area includes El Dorado, Placer, Sacramento, Sutter, Yolo, and Yuba counties, which are located within the Great Valley geomorphic province and the Sierra Nevada geomorphic province. Both geomorphic provinces are discussed below. REGIONAL PHYSIOGRAPHIC SETTING OF THE MTP/SCS PLAN AREA The Great Valley of California, also called the Central Valley of California, is a nearly flat alluvial plain extending from the Tehachapi Mountains at the south to the Klamath Mountains at the north, and from the Sierra Nevada on the east to the Coast Ranges on the west. -
150 Geologic Facts About California
California Geological Survey - 150th Anniversary 150 Geologic Facts about California California’s geology is varied and complex. The high mountains and broad valleys we see today were created over long periods of time by geologic processes such as fault movement, volcanism, sea level change, erosion and sedimentation. Below are 150 facts about the geology of California and the California Geological Survey (CGS). General Geology and Landforms 1 California has more than 800 different geologic units that provide a variety of rock types, mineral resources, geologic structures and spectacular scenery. 2 Both the highest and lowest elevations in the 48 contiguous states are in California, only 80 miles apart. The tallest mountain peak is Mt. Whitney at 14,496 feet; the lowest elevation in California and North America is in Death Valley at 282 feet below sea level. 3 California’s state mineral is gold. The Gold Rush of 1849 caused an influx of settlers and led to California becoming the 31st state in 1850. 4 California’s state rock is serpentine. It is apple-green to black in color and is often mottled with light and dark colors, similar to a snake. It is a metamorphic rock typically derived from iron- and magnesium-rich igneous rocks from the Earth’s mantle (the layer below the Earth’s crust). It is sometimes associated with fault zones and often has a greasy or silky luster and a soapy feel. 5 California’s state fossil is the saber-toothed cat. In California, the most abundant fossils of the saber-toothed cat are found at the La Brea Tar Pits in Los Angeles. -
Native American Settlement to 1969
29 Context: Native American Settlement to 1969 Francisco Patencio outside the roundhouse, c. 1940. Source: Palm Springs Historical Society. FINAL DRAFT – FOR CITY COUNCIL APPROVAL City of Palm Springs Citywide Historic Context Statement & Survey Findings HISTORIC RESOURCES GROUP 30 CONTEXT: NATIVE AMERICAN SETTLEMENT TO 196923 The earliest inhabitants of the Coachella Valley are the Native people known ethnohistorically as the Cahuilla Indians. The Cahuilla territory includes the areas from the San Jacinto Mountains, the San Gorgonia Pass, and the desert regions reaching east to the Colorado River. The Cahuilla language is part of the Takic branch of the Uto-Aztecan language family and all the Cahuilla groups speak a mutually intelligible despite different dialects. The Cahuilla group that inhabited the Palm Springs area are known as the Agua Caliente Band of Cahuilla Indians. The Cahuilla name for the area that is now Palm Springs is Sec-he, “boiling water,” named for the hot springs located in what is currently the center of the Palm Springs business district. The springs have always provided clean water, bathing, and a connection to the spiritual world, and were used for ceremonial and healing purposes.24 The Cahuilla people refer to themselves as ‘ivi’lyu’atum and are ethnographically divided into two patrilineal moieties: the Wildcats and the Coyotes. Each moiety was further divided into clans which are made up of lineages. Lineages had their own territory and hunting rights within a larger clan territory. There are a number of lineages in the Palm Springs area, which each have religious and political autonomy. Prior to European contact, Cahuilla communities established summer settlements in the palm-lined mountain canyons around the Coachella valley; oral histories and archaeological evidence indicates that they settled in the Tahquitz Canyon at least 5,000 years ago.25 The Cahuilla moved each winter to thatched shelters clustered around the natural mineral hot springs on the valley floor. -
Chapter IV. ENVIRONMENTAL RESOURCES
Chapter IV. ENVIRONMENTAL RESOURCES City of Banning General Plan WATER RESOURCES ELEMENT PURPOSE The Water Resources Element addresses water quality, availability and conservation for the City’s current and future needs. The Element also discusses the importance of on-going coordination and cooperation between the City, Banning Heights Mutual Water Company, High Valley Water District, San Gorgonio Pass Water Agency and other agencies responsible for supplying water to the region. Topics include the ground water replenishment program, consumptive demand of City residents, and wastewater management and its increasingly important role in the protection of ground water resources. The goals, policies and programs set forth in this element direct staff and other City officials in the management of this essential resource. BACKGROUND The Water Resources Element is directly related to the Land Use Element, in considering the availability of water resources to meet the land use plan; and has a direct relationship to the Flooding and Hydrology Element, in its effort to protect and enhance groundwater recharge. Water issues are also integral components of the following elements: Police and Fire Protection, Economic Development, Emergency Preparedness, and Water, Wastewater and Utilities. The Water Resources Element addresses topics set forth in California Government Code Section 65302(d). Also, in accordance with the California Environmental Quality Act (CEQA), Section 21083.2(g), the City is empowered to require that adequate research and documentation be conducted when the potential for significant impacts to water and other important resources exists. Watersheds The westernmost part of the planning area is located at the summit of the San Gorgonio Pass, which divides two major watersheds: the San Jacinto River Watershed to the west and the Salton Sea watershed to the east. -
5.9 BIOLOGICAL RESOURCES the Information Contained Within This
5.9 Biological Resources 5.9 BIOLOGICAL RESOURCES The information contained within this section is summarized from the Moreno Valley General Plan EIR Biological Report (Merkel & Associates, September 2004). The report is provided in Volume II Appendix E of this EIR. The existing biological resources documented in this report were determined through an extensive review of the most current, available biological literature and Geographical Information Systems (GIS) data available for the planning area. Previous biological surveys conducted by Merkel & Associates (M&A) staff, as well as biological information gathered by other consultants for projects within Moreno Valley, were further reviewed. Vegetation communities were primarily identified based on the regional GIS data incorporated into the MSHCP (KTU+A and PSBS 1995). Floral and faunal species potential presence was determined based on vegetation community presence/absence and knowledge of species requirements. The assessment of presence or potential presence of sensitive biological resources was also based on MSHCP data, which incorporated California Natural Diversity Database records for sensitive species. In addition to the MSHCP and vegetation community information, the following sources were consulted to aid in determining faunal presence/absence: USFWS 2000b, Ericksen and Belk 1999, Sauer et al. 1996, Sauer et al. 2000, Zeiner et al. 1988, Zeiner et al. 1990a and 1990b. M&A also contacted individuals with special expertise to determine the likelihood of species presence for certain groups (e.g., bats). Additionally, M&A biologists, Craig Reiser and Diana Jensen, conducted field investigations in April 2001 to ground truth portions of the regional GIS vegetation data and record locations of identified sensitive species. -
Preliminary Geologic Map of the Little Piute Mountains, San Bernardino County, California
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary Geologic Map of the Little Piute Mountains, San Bernardino County, California by Keith A. Howard1, Michael L. Dennis2, Karl E. Karlstrom3, and Geoffrey A. Phelps1 Open-File Report 95-598 1995 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purpose only and does not imply endorsement by the U.S. Government. 1 Menlo Park, California 94025 2 Northern Arizona University, Flagstaff, Arizona 86002 3 University of New Mexico, Albuquerque, New Mexico 87131 Mapped 1978-1993 by K. Howard, P. Stone, K. Karlstrom, G. Phelps, M. Dennis, and students from Northern Arizona University. GEOLOGIC SUMMARY Introduction The Little Piute Mountains in the eastern Mojave Desert expose a series of folds and thrust faults involving metamorphosed Paleozoic strata (Miller and others, 1982; Stone and others, 1983). Detailed mapping of these structures was undertaken to help elucidate regional Mesozoic structural evolution. Earlier geologic maps were prepared by Cooksley (1960a,b,c,d, generalized by Bishop, 1964) and Stone and others (1983). Deformed and metamorphosed Paleozoic and Triassic rocks form a stratal succession that was originally deposited in shallow seas on the North American craton. Based on lithologic sequence the units are correlated with unmetamorphosed equivalents 200 km to the northeast in the Grand Canyon, Arizona, and 35-50 km to the west in the Marble, Ship, and Providence Mountains, California (Stone and others, 1983). -
DRAFT 2021 Interregional Transportation Strategic Plan
DRAFT Interregional Transportation Strategic Plan Caltrans AUGUST 2021 ACCESSIBILITY ASSISTANCE Caltrans makes every attempt to ensure our documents are accessible. Due to variances between assistive technologies, there may be portions of this document which are not accessible. Where documents cannot be made accessible, we are committed to providing alternative access to the content. Should you need additional assistance, please contact us at [email protected] or visit https://dot.ca.gov/request- ada-compliant-documents. For individuals with disabilities, this document is available in Braille, large print, audiocassette, or computer disc. It is also available in alternative languages. To obtain a copy in one of these formats, please email us at [email protected] or call (916) 654-2397, TTY: 711. The Plan is also available online at https://dot.ca.gov/programs/legislative- affairs/reports. Caltrans® and the Caltrans logo are registered service marks of the California Department of Transportation and may not be copied, distributed, displayed, reproduced or transmitted in any form without prior written permission from the California Department of Transportation. © 2021 California Department of Transportation. All Rights Reserved i – Table of Contents Gavin C Newsom Governor State of California David S Kim Secretary California State Transportation Agency Toks Omishakin Director California Department of Transportation Mike Keever Chief Deputy Director California Department of Transportation ii – Table of Contents ACKNOWLEDGEMENTS This document would not have been possible without the contributions of many people, past and present, from department staff and managers, and partner agencies, to California tribal governments, key stakeholders, advocacy organizations, and the public at large. -
Two Southern California Trade Trails
UC Merced Journal of California and Great Basin Anthropology Title Two Southern California Trade Trails Permalink https://escholarship.org/uc/item/3632g2w5 Journal Journal of California and Great Basin Anthropology, 2(1) ISSN 0191-3557 Author Johnston, Francis J Publication Date 1980-07-01 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Journal of California and Great Basin Anthropology Vol. 2, No. I, pp. 88-96(1980). Two Southern California Trade Trails FRANCIS J. JOHNSTON T is generally considered by historians that Los Angeles Basin, is not considered here, nor I Spanish overland communication from is the Yuman Trail from the Yuma Crossing to Upper California to Mexico by way of Sonora San Diego. ceased with the abandonment of the Anza THE MARICOPA TRAIL Trail after the Colorado River Campaign of 1781-1783. Communication was maintained The Maricopa are a Gila River tribe living by sea, either direct from ports in Upper Cali along that river in Arizona. In historic time fornia or by courier to Lower California and they were located well east of the Quechan, thence to the mainland by sea (Brumgardt who inhabited the area where the Gila and the 1976:83). Colorado rivers come together (White 1974: The route was essentially reopened for 128). sporadic mail and dispatch service, and for In 1821, a Maricopa leader called Jose migration to and from Sonora through a Cocomaricopa and a few companions combination of circumstances including mili appeared at San Gabriel Mission saying they tary expeditions and operations of the wanted to trade.