A Landscape-Level Management Approach for the Saline Valley Salt Tram

Total Page:16

File Type:pdf, Size:1020Kb

A Landscape-Level Management Approach for the Saline Valley Salt Tram For the Sake of Salt: A Landscape-Level Management Approach for the Saline Valley Salt Tram by Laurel E. Lueders A thesis submitted to Sonoma State University Rohnert Park, California in partial fulfillment of the requirements for the degree of MASTER OF ARTS In Cultural Resource Management Dr. Laura Watt Dr. Margret Purser Greg Haverstock, M.A. May 3rd, 2019 ii Copyright 2019 Laurel E. Lueders iii iv For the Sake of Salt: A Landscape-Level Management Approach for the Saline Valley Salt Tram Thesis by Laurel E. Lueders ABSTRACT Purpose: The intent of this thesis is to propose a collaborative landscape level management strategy for the Saline Valley Salt Tram (SVST). This unique aerial tramway was placed on the National Register of Historic Places (NRHP) in 1974 and was the first tramway to traverse an entire mountain range. With the passing of the California Desert Protection Act of 1994, this historically significant site was placed within three separate federal land managing agencies jurisdictions: Death Valley National Park (DVNP), Bureau of Land Management (BLM) Ridgecrest Field Office, and BLM Bishop Field Office. Due to this, this structure has been managed with three distinct perspectives. The goal of this study is to utilize the SVST as an example for promoting holistic landscape level preservation for cultural resources that traverse borders. Methods: A review of available literature, past and present management plans, applicable legislation, and archival material was conducted in order to create a framework for conceptualizing the current state of the Saline Valley Salt Tram. In addition, the western slope of the project area was examined as a case study for comprehensive landscape management. A pedestrian survey was conducted and two other phases of historic manipulation of the landscape were discovered: a cluster of charcoal reduction sites that predate the SVST, and the modern interactions via a cherry- stemmed four-wheel drive road that acts as an access road into the Inyo Mountain Wilderness. Each of these three human interactions with the landscape were recorded and compiled onto Geospatial Inform System (GIS) Map. Findings: Discussions with employees of DVNP, BLM Ridgecrest Field Office, and BLM Bishop Field Office highlighted both similarities and differences in each agency’s belief regarding management of a NRHP site that sits within a designated wilderness. By focusing on the western slope for the case study, a pattern in natural and human disturbances was noted amongst SVST structures. Conclusions: The management dilemma surrounding the SVST stems directly from the restructuring of borders that placed the SVST across three agencies dominion and wilderness designations that were placed on land that has an extensive history of human manipulation. Acknowledging these factors, alongside reshaping how the public defines wilderness, are the first steps in unifying management. Recently, the California Desert Protection and Recreation Act of 2019 has passed which redefines borders between the National Park Service and BLM while designating large swathes of wilderness across southern California. Therefore, establishing the possibility of potential for fragmentation of a cultural resource. MA Program: Cultural Resource Management Sonoma State University Date: May 3rd, 2019 v ACKNOWLEDGEMENTS This thesis would not have been possible without the support and encouragement of many people. I want to begin by first thanking Dr. Laura Watt and Dr. Margaret Purser, for without their constant support, enthusiasm, and guidance this project would not be completed. I have been incredibly lucky to have a Chair and committee member who cared so deeply about my work. When discussing cultural landscapes, you both harness this infectious excitement and our conversations both during and outside of class were some of the most impactful of my graduate career. Secondly, a big thanks goes out to Greg Haverstock of the BLM Bishop Field Office for his mentorship over the years. Not only did you take me under your wing early on in my studies by teaching me the basics of federal archaeology, but you provided me with an example of someone who carries themselves with respect when managing cultural resources. You always made time for me, even when I would stop by the office unannounced, to hear my thoughts or offer advice about my project and career trajectory. Thank you for everything, and I could not have asked for a better mentor. This thesis is heavily indebted to Jane Lakeman of Death Valley National Park and Marty Dickies of BLM Ridgecrest Field Office for without whom this project would not have expanded beyond the early parameters of my Direct Hire Authority Internship. Similarly, thank you to the staff members at the Maturango Museum and the Eastern California Museum who allowed me to pour over archival material at your repositories over the span of weeks with a fine-tooth comb. This project would not have been possible without your records and I am appreciative that you allowed me access. Thank you to Kari Lentz, Robert Watson, and cohorts of 2015, 2016, and 2017 for your friendship and moral support. The thesis process is not easy, and it was comforting to be surrounded by such determined people all working towards the same goal. To the fellow BLM Bishop Field Office staff who volunteered their time to assist in surveying the salt tram, thank you. I know you all have busy work schedules and it meant a lot that you carved out time to act as my safety buddies. I hope you found as much enjoyment out of our field days as I did. Lastly, a big thank you to my family and friends who all supported me by keeping me on track during this process and providing me with the occasional distractions. Everything from volunteering your day to hike the tramway with me to allowing me to verbalize my frustrations without judgment, your backing did not go unnoticed or unappreciated. Special thanks to my spouse, Blake Hubbard, who endured thousands of hours of conversation revolving the salt tram, always volunteered his R&R days between wildfires to survey with me and was there to refocus me when I was lacking motivation. Without you I would not have made it through this process, and I am forever grateful for your love and support. vi TABLE OF CONTENTS Acknowledgements………………………………………………………………………v Figures………………………………………………….………………………….…...viii I. Introduction…………………………………………………..…………..……………1 Goal of Study……………………………………………………………………...2 Theoretical Framework……………………………………………………………3 Organization of Study……………………………………………………………..5 II. Project Background…………………………………………………………………..6 Aerial Tramways…………………………………………………………………..6 Keane Wonder Mine………………………………………………………………8 Beveridge Mining District……………………...……………………...………...10 Cerro Gordo……………………………………………………………………...11 Saline Valley Salt Tram………………………………………………………….15 Construction of the Saline Valley Salt Tram…………………………….16 Phases of Operation and Ownership of the Saline Valley Salt Tram……18 Layers of Historic Use on the Landscape………………………………………..27 Charcoal Burners………………………………………………………...28 The Swansea Grade……………………………………………………....31 The California Desert Protection Act of 1994…………………………………...33 Death Valley National Park……………………………………………...38 The Wilderness Act of 1964……………………………………………..39 Bureau of Land Management Ridgecrest Field Office…………………..40 Bureau of Land Management Bishop Field Office……………………....42 Why Landscape Preservation Could Be the Answer………………………….…45 III. Management of Landscapes……………………………………………………….46 What is a Cultural Landscape?..............................................................................46 Westward Expansion………………………………………………….....48 Wilderness is not Truly Wild…………………………………………….51 Constriction of Landscapes via Borders……………………………………........53 Fragmentation………………………………………………………........55 Linear Features…………………………………………………………...56 Collaboration Based Landscape Projects………………………………...57 Industrial Archaeology…………………………………………………………...61 Roadways as a Landscape………………………………………………..62 Spatial Awareness………………………………………………………………..64 Creating Maps as a Representation of a Landscape……………………...65 Inventory of a Landscape………………………………………………...67 Landscapes Consist of Layers…………………………………………....68 Preserving a Landscape does not Equate to Freezing One Aspect…………........69 Modern Landscape Interactions………………………………………….72 IV. Methods of Data Collection………………………………………..……………...75 Landscape Designation as a Form of Preservation………………………………75 Correspondence Between Parties………………………………………………...76 Archival Research………………………………………………………………..80 vii Case Study of Landscape Preservation on the Western Slope of the Saline Valley Salt Tram…………………………………………….…………………………...81 Historic Photographs……………………………………………………………..82 Intensive Pedestrian Survey……………………………………………………...85 Recording Tower Structures and Sites…………………………………………...87 Recording Charcoal Reduction Sites…………………………………………….90 Recording the Swansea Grade…………………………………………………...91 Mapping the Western Slope……………………………………………………...92 V. Conclusions………………………………………………………………………..…94 Areas of Further Research……………………………………………………….95 Saline Valley Salt Tram is One Piece of a Larger Network……………………..95 Charcoal Reduction Sites………………………………………………………...96 Stewardship Projects with Off-Highway Vehicle Groups…………………….....97 Continuation of Survey…………………………………………………………..98 What’s Next?.........................................................................................................99 Appendix A: Salt Tram Checklist… ……………………………...…………………102 Appendix B:
Recommended publications
  • Conglomerate Mesa Action Alert Tip Sheet
    Make Your Voice Heard! A public comment period is OPEN for K2 Gold and Mojave Precious Metal’s exploratory drilling at Conglomerate Mesa. They are proposing miles of new road construction and 120 drill holes, spanning 12.1 acres of ancestral tribal lands, cultural resources, scenic landscapes, and threatened habitat. Read below to learn how to submit your public comment before August 30th to protect Conglomerate Mesa from this destructive mining project. Tips For Making Eective Comments Make it personal! Share your story of personal connection to these lands and why you want the area to be protected. Here is a sample letter - please personalize it and make it your own: To Whom it May Concern, I am a resident of [your city] and I strongly oppose K2 Gold’s exploratory drilling project at Conglomerate Mesa. This region is special to me because [insert your special connection to this place, your favorite memories here, etc. - no limit on how much you write! Some examples: ● Conglomerate Mesa is the traditional homelands of the Timbisha Shoshone and Paiute Shoshone Tribal Nations. This area is an important area for pinyon nut harvesting and is one of the many blending zones of transitional territories. Numerous leaders in local tribes have opposed the gold exploration and mining by K2 Gold. I stand united with the Indigenous people in this opposition. ● Conglomerate Mesa is designated as California Desert National Conservation Lands, and these lands are managed to conserve, protect, and restore these nationally signicant ecological, cultural, and scientic values. Mining Conglomerate Mesa would go directly against the intended management of this landscape.
    [Show full text]
  • Mineral Resources and Mineral Resource Potential of the Saline Valley and Lower Saline Wilderness Study Areas Inyo County, California
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Mineral resources and mineral resource potential of the Saline Valley and Lower Saline Wilderness Study Areas Inyo County, California Chester T. Wrucke, Sherman P. Marsh, Gary L. Raines, R. Scott Werschky, Richard J. Blakely, and Donald B. Hoover U.S. Geological Survey and Edward L. McHugh, Clay ton M. Rumsey, Richard S. Gaps, and J. Douglas Causey U.S. Bureau of Mines U.S. Geological Survey Open-File Report 84-560 Prepared by U.S. Geological Survey and U.S. Bureau of Mines for U.S. Bureau of Land Management This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1984 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Mineral resources and mineral resource potential of the Saline Valley and Lower Saline Wilderness Study Areas Inyo County, California by Chester T. Wrucke, Sherman P. Marsh, Gary L. Raines, R. Scott Werschky, Richard J. Blakely, and Donald B. Hoover U.S. Geological Survey and Edward L. McHugh, Clayton M. Rumsey, Richard S. Gaps, and J. Douglas Causey U.S. Bureau of Mines U.S. Geological Survey Open-File Report 84-560 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1984 ILLUSTRATIONS Plate 1. Mineral resource potential map of the Saline Valley and Lower Saline Wilderness Study Areas, Inyo County, California................................ In pocket Figure 1. Map showing location of Saline Valley and Lower Saline Wilderness Study Areas, California.............. 39 2.
    [Show full text]
  • Interest and the Panamint Shoshone (E.G., Voegelin 1938; Zigmond 1938; and Kelly 1934)
    109 VyI. NOTES ON BOUNDARIES AND CULTURE OF THE PANAMINT SHOSHONE AND OWENS VALLEY PAIUTE * Gordon L. Grosscup Boundary of the Panamint The Panamint Shoshone, also referred to as the Panamint, Koso (Coso) and Shoshone of eastern California, lived in that portion of the Basin and Range Province which extends from the Sierra Nevadas on the west to the Amargosa Desert of eastern Nevada on the east, and from Owens Valley and Fish Lake Valley in the north to an ill- defined boundary in the south shared with Southern Paiute groups. These boundaries will be discussed below. Previous attempts to define the Panamint Shoshone boundary have been made by Kroeber (1925), Steward (1933, 1937, 1938, 1939 and 1941) and Driver (1937). Others, who have worked with some of the groups which border the Panamint Shoshone, have something to say about the common boundary between the group of their special interest and the Panamint Shoshone (e.g., Voegelin 1938; Zigmond 1938; and Kelly 1934). Kroeber (1925: 589-560) wrote: "The territory of the westernmost member of this group [the Shoshone], our Koso, who form as it were the head of a serpent that curves across the map for 1, 500 miles, is one of the largest of any Californian people. It was also perhaps the most thinly populated, and one of the least defined. If there were boundaries, they are not known. To the west the crest of the Sierra has been assumed as the limit of the Koso toward the Tubatulabal. On the north were the eastern Mono of Owens River.
    [Show full text]
  • Chapter 8 Manzanar
    CHAPTER 8 MANZANAR Introduction The Manzanar Relocation Center, initially referred to as the “Owens Valley Reception Center”, was located at about 36oo44' N latitude and 118 09'W longitude, and at about 3,900 feet elevation in east-central California’s Inyo County (Figure 8.1). Independence lay about six miles north and Lone Pine approximately ten miles south along U.S. highway 395. Los Angeles is about 225 miles to the south and Las Vegas approximately 230 miles to the southeast. The relocation center was named after Manzanar, a turn-of-the-century fruit town at the site that disappeared after the City of Los Angeles purchased its land and water. The Los Angeles Aqueduct lies about a mile to the east. The Works Progress Administration (1939, p. 517-518), on the eve of World War II, described this area as: This section of US 395 penetrates a land of contrasts–cool crests and burning lowlands, fertile agricultural regions and untamed deserts. It is a land where Indians made a last stand against the invading white man, where bandits sought refuge from early vigilante retribution; a land of fortunes–past and present–in gold, silver, tungsten, marble, soda, and borax; and a land esteemed by sportsmen because of scores of lakes and streams abounding with trout and forests alive with game. The highway follows the irregular base of the towering Sierra Nevada, past the highest peak in any of the States–Mount Whitney–at the western approach to Death Valley, the Nation’s lowest, and hottest, area. The following pages address: 1) the physical and human setting in which Manzanar was located; 2) why east central California was selected for a relocation center; 3) the structural layout of Manzanar; 4) the origins of Manzanar’s evacuees; 5) how Manzanar’s evacuees interacted with the physical and human environments of east central California; 6) relocation patterns of Manzanar’s evacuees; 7) the fate of Manzanar after closing; and 8) the impact of Manzanar on east central California some 60 years after closing.
    [Show full text]
  • Birds of the California Desert
    BIRDS OF THE CALIFORNIA DESERT A. Sidney England and William F. Laudenslayer, Jr. i INTRODUCTION i \ 1 The term, "California desert", as used herein, refers to a politically defined region, most of i which is included in the California Desert Conservation Area (CDCA) designated by the Federal Land ; and Management Act of 1976 (FLPMA). Of the 25 million acres in the CDCA, about one-half are i public lands, most of which are managed by the Bureau of Land Management (BLM) according to the "980 P California Desert Conservation Area Plan mandated by FLPMA. The California desert encompasses those portions of the Great Basin Desert (east of the White and lnyo Mountains and A south of the California-Nevada border), the Mojave Desert, and the Colorado Desert which occur " within California; it does not include areas of riparian, aquatic, urban, and agricultural habitats . adjacent to the Colorado River. (Also see chapters on Geology by Norris and Bioclimatology by E3irdsI4 are the most conspicuous vertebrates found in the California deserts. Records exist for at least 425 species (Garrett and Dunn 1981) from 18 orders and 55 families. These counts far exceed those for mammals, reptiles, amphibians and fish, and they are similar to totals for the entire state -- 542 species from 20 orders and 65 families (Laudenslayer and Grenfell 1983). These figures may seem surprisingly similar considering the harsh, arid climates often believed characteristic of I desert environments. However, habiiats found in the California desert range from open water and h marshes at the Salton Sea to pinyon-juniper woodland and limber pinelbristlecone pine forests on a few mountain ranges.
    [Show full text]
  • Inferences Regarding Aboriginal Hunting Behavior in the Saline Valley, Inyo County, California
    Journal of California and Great Basin Anthropology Vol. 2, No. I, pp. 60-79(1980). Inferences Regarding Aboriginal Hunting Behavior in the Saline Valley, Inyo County, California RICHARD A. BROOK HE documented use of stone "hunting a member of the 1861 Boundary Survey Party Tblinds" behind which marksmen hid them­ reconnoitering the Death Valley region. The selves "ve'/7//-6'o?m-e"i (Baillie-Grohman 1884: chronicler observed: 168) waiting for sheep to be driven along trails, can be found in the writings of a number of . curious structures ... on the tops of early historians (Baillie-Grohman 1884; round bald hills, a short distance to the Spears 1892; Muir 1901; Bailey 1940). Recent northwest of the springs, being low walls of archaeological discoveries of rock features loose stones curved in the shape of a demi­ lune, about ten feet in length and about believed to be hunting blinds at the Upper three feet high . , . , There were twenty or Warm Springs (Fig. I) in Saline Valley, Inyo thirty of them [Woodward 1961:49], County, California, provide a basis to substan­ tiate, build upon, and evaluate these observa­ This paper discusses a series of 60 such piled- tions and the ethnographic descriptions of up boulder features recorded within a I km.^ hunting in the Great Basin (Steward 1933, area at Upper Warm Springs (Fig. 2). 1938, 1941; Driver 1937; Voegelin 1938; The same chronicler offered some tentative Stewart 1941). An examination of these explanations as to their function: features, their location, orientation, and asso­ ciations in
    [Show full text]
  • Nature and Significance of the Inyo Thrust Fault, Eastern California: Discussion and Reply
    Nature and significance of the Inyo thrust fault, eastern California: Discussion and reply Discussion GEORGE C. DUNNE Department of Geosciences, California State University, Northridge, Northridge, California 91324 RACHEL M. GULLIVER Envicom Corporation, 4521 Sherman Oaks Avenue, Sherman Oaks, California 91403 INTRODUCTION Olson (1972, Fig. 2). Also included in Fig- caught between two downward-convergent ure 1 are our alternative interpretations of faults, one of which truncates the other; Stevens and Olson (1972) proposed that the geology along their cross-section lines. folding is observed in one area, but it seems a complexly faulted area at the west base of We base our interpretations on 11 days of to result from drag along one of the faults. the northern Inyo Mountains is a window field work in the Tinemaha area. Locations 2, 3: The elongate mass of Or- in a folded, large-slip fault they named the We have few disagreements with the dovician chert and an adjacent elongate ex- Inyo thrust fault. On the basis of their rec- more objective aspects of the geologic posure of Mississippian rock are essentially ognition of this window and earlier struc- mapping of Stevens and Olson. We agree in homoclinal, separated by steep faults that tural interpretations by Stevens (1969, general with their identification and map dip toward the younger sequence (see cross 1970), Stevens and Olson proposed a distribution of rock units, although we sus- section C, Fig. 1). Location 5: The tectonic model in which the Inyo thrust pect that some units on hills 1 and 4 (Fig. 1) arrowhead-shaped contact between older fault played a major role in the Mesozoic are misidentified.
    [Show full text]
  • University of Nevada Reno HYDROLOGY and WATER
    University of Nevada Reno HYDROLOGY AND WATER BUDGET OF OWENS LAKE, CALIFORNIA A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Science in Hydrology /Hydrogeology By Thomas J. Lopes v»' October, 1987 mimes UlRAfcY The thesis of Thomas J. Lopes is approved: NlV s i s 3 3 ( o < ) \ Thesis Advisor University of Nevada Reno October, 1987 ACKNOWLEGDEMENTS Funding and data collection for this thesis was provided by the following individuals and organizations. I would like to thank: William Hutchison, Inyo County Hydrologist Los Angeles Department of Water and Power William Cox, Great Basin Air Pollution Control District Ellen Hardebeck, Great Basin Air Pollution Control District Patricia Casey Knapp, Environmental Monitoring Services, Inc. Todd Mihevc, Desert Research Institute Hydrogeologist Scott Tyler, Desert Research Institute Hydrogeologist Water Resource Center, Desert Research Institute Special thanks to my major advisor Dr. Gilbert Cochran and Brad Lyles, Desert Research Institute hydrogeologist. This project would have been much more difficult without Dr. Cochrans’ guidence and Mr. Lyles computer expertise. Finally, I would like to thank my parents for their continued support of my education. In times of doubt, they always gave me the encouragement needed to carry on with my work. ABSTRACT Owens Lake, California, is a hydrologically closed basin in southern Owens Valley. Diversion of water out of the basin has resulted in lake dessication and salt crust formation on the exposed lake bed. Salt crusts are most extensive along the southeastern to west lake bed due to small volumes of runoff from the Coso Mountains and diversion of Sierra Nevada runoff.
    [Show full text]
  • Introduction
    1 INTRODUCTION This monograph is an introductory descriptive grammar of Tlimpisa Shoshone, meant to provide both layman and specialist with a basic understanding of how the language works as a linguistic system. In this sense, it is intended to be a "nuts and bolts" grammar with lots of examples illustrating the most important grammatical elements and processes in the language. 1 Tlimpisa Shoshone is a dialect of the language most often called Panamint in the technical literature (e.g., Freeze and Iannucci 1979, Henshaw 1883, Kroeber 1939, Lamb 1958a and 1964, McLaughlin 1987, Miller 1984) . The language is also known as Panamint Shoshone (Fowler and Fowler 1971, Merriam 1904, Miller et al. 1971), Koso (= Coso) or Koso Shoshone (Kroeber 1925, Lamb 1958a), and simply Shoshone (Steward 1938). Panamint and two other closely related languages, Shoshone proper and Comanche, comprise the Central Numic branch of the Numic subfamily of the northern division of the uto-Aztecan family of American Indian languages (see Lamb 1964, Miller 1984, Kaufman and Campbell 1981). Speakers of uto-Aztecan languages occupied more territory in aboriginal America than any other group. More than 30 Uto-Aztecan languages were spoken over a vast area stretching from the Salmon River in central Idaho south through the Great Basin and peripheral areas into the Southwest and through northern and central Mexico. Colonies of Aztecan speakers were also scattered further south into Central America. At the time of 1 UTO-AZTECAN FAMILY Northern Division NUMlC Central Numic
    [Show full text]
  • The California Desert CONSERVATION AREA PLAN 1980 As Amended
    the California Desert CONSERVATION AREA PLAN 1980 as amended U.S. DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT U.S. Department of the Interior Bureau of Land Management Desert District Riverside, California the California Desert CONSERVATION AREA PLAN 1980 as Amended IN REPLY REFER TO United States Department of the Interior BUREAU OF LAND MANAGEMENT STATE OFFICE Federal Office Building 2800 Cottage Way Sacramento, California 95825 Dear Reader: Thank you.You and many other interested citizens like you have made this California Desert Conservation Area Plan. It was conceived of your interests and concerns, born into law through your elected representatives, molded by your direct personal involvement, matured and refined through public conflict, interaction, and compromise, and completed as a result of your review, comment and advice. It is a good plan. You have reason to be proud. Perhaps, as individuals, we may say, “This is not exactly the plan I would like,” but together we can say, “This is a plan we can agree on, it is fair, and it is possible.” This is the most important part of all, because this Plan is only a beginning. A plan is a piece of paper-what counts is what happens on the ground. The California Desert Plan encompasses a tremendous area and many different resources and uses. The decisions in the Plan are major and important, but they are only general guides to site—specific actions. The job ahead of us now involves three tasks: —Site-specific plans, such as grazing allotment management plans or vehicle route designation; —On-the-ground actions, such as granting mineral leases, developing water sources for wildlife, building fences for livestock pastures or for protecting petroglyphs; and —Keeping people informed of and involved in putting the Plan to work on the ground, and in changing the Plan to meet future needs.
    [Show full text]
  • 4.5 Cultural Resources
    4.5 – Cultural Resources 4.5 Cultural Resources This section identifies cultural and paleontological resources along the IC Project Alignment, identifies applicable significance thresholds, assesses the IC Project’s impacts to these resources and their significance, and recommends measures to avoid or substantially reduce any effects found to be potentially significant. Cultural resources are defined as any object or specific location of past human activity, occupation, or use that is identifiable through historical documentation, inventory, or oral evidence. Cultural resources can be separated into three categories: archaeological, building/structural, and traditional resources. Archaeological resources include prehistoric and historic remains of human activity. Prehistoric resources can be composed of lithic scatters, ceramic scatters, quarries, habitation sites, temporary camps/rock rings, ceremonial sites, and trails. Historic-era resources are typically those that are 50 years or older. Historic archaeological resources can consist of structural remains (e.g., concrete foundations), historic objects (e.g., bottles and cans), features (e.g., refuse deposits or scatters), and sites (e.g., resources that contain one or more of the aforementioned categories). Built environment resources range from historic buildings to canals, historic roads and trails, bridges, ditches, cemeteries, and electrical infrastructure, such as transmission lines, substations, and generating facilities. A traditional cultural resource is a resource associated with the cultural practices, traditions, beliefs, lifeways, arts, crafts, or social institutions of a living community. They are rooted in a traditional community’s history and are important in maintaining the continuing cultural identity of the community. See Section 4.18, Tribal Cultural Resources, for a discussion on cultural resources of potential importance to California Native American tribes.
    [Show full text]
  • Cambrian Transition in the Southern Great Basin
    The Sedimentary Record 2000; Shen and Schidlowski, 2000). Due to The Precambrian- endemic biotas and facies control, it is diffi- cult to correlate directly between siliciclas- Cambrian Transition in the tic- and carbonate-dominated successions. This is particularly true for the PC-C boundary interval because lowermost Southern Great Basin, USA Cambrian biotas are highly endemic and Frank A. Corsetti James W.Hagadorn individual, globally distributed guide fossils Department of Earth Science Department of Geology are lacking (Landing, 1988; Geyer and University of Southern California Amherst College Shergold, 2000). Los Angeles, CA 90089-0740 Amherst, MA 01002 Determination of a stratigraphic bound- [email protected] [email protected] ary generates a large amount of interest because it provides scientists with an oppor- ABSTRACT:The Precambrian-Cambrian boundary presents an interesting tunity to address a variety of related issues, stratigraphic conundrum: the trace fossil used to mark and correlate the base of the including whether the proposed boundary Cambrian, Treptichnus pedum, is restricted to siliciclastic facies, whereas position marks a major event in Earth histo- biomineralized fossils and chemostratigraphic signals are most commonly obtained ry. Sometimes the larger-scale meaning of from carbonate-dominated sections.Thus, it is difficult to correlate directly between the particular boundary can be lost during many of the Precambrian-Cambrian boundary sections, and to assess details of the the process of characterization. This is timing of evolutionary events that transpired during this interval of time.Thick demonstrated in a plot of PC-C boundary sections in the White-Inyo region of eastern California and western Nevada, USA, papers through time (Fig.
    [Show full text]