Upper Las Vegas Wash/ Tule Springs, Nevada Reconnaissance Report
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Additions to the Late Pleistocene Vertebrate Paleontology of the Las
Additions to the Late Pleistocene Vertebrate Paleontology of ABSTRACT the Las Vegas Formation, Clark County, Nevada DISCUSSION Studies from the 1930s through the 1960s documented one of the most significant late The detailed mapping of over 500 vertebrate paleontologic localities Pleistocene faunas from the Mojave Desert in the Tule Springs area of North Las Vegas. in the upper Las Vegas Wash proved to be an interesting challenge in Recent field investigations in North Las Vegas by the San Bernardino County Museum Kathleen Springer, J. Christopher Sagebiel, Eric Scott, Craig Manker and Chris Austin terms of discerning the stratigraphy. Very little geologic have broadened our knowledge of this fauna across the Las Vegas Wash.Seven units, investigation had been performed in this region since the 1967 work designated A through G, have been defined in the section of the Las Vegas Wash near Division of Geological Sciences, San Bernardino County Museum, Redlands, California of Haynes. That very detailed study was geographically limited to Tule Springs State Park. Units B, D, and E have proven fossiliferous in the area of the the Tule Springs archaeologic investigation and the very near Tule Springs State Park, and date to>40,000 ybp, approximately 25,500 ybp, and about environs at a reconnaissance level. Our study area, falling mostly 14,500 to 9,300 ybp,respectively. Research across the Las Vegas Wash has resulted in within the Gass Peak S.W. 7.5’ U.S.G.S. topographic sheet, had not the discovery of several hundred new fossil localities. In describing the geology at these BACKGROUND been mapped. -
Biogeographic Distribution of Bison in Arizona
Wolff, TER-QUA PalArch’s Journal of Vertebrate Palaeontology, 10(4) (2013) HOME ON THE RANGE: BIOGEOGRAPHIC DISTRIBUTION OF BISON IN ARIZONA Sarah E. Wolff* * University of Arizona School of Anthropology, University of Arizona Tucson, AZ 85721 [email protected] Sarah E. Wolff. 2013. Home on the Range: Biogeographic Distribution of Bison in Arizona. – Palarch’s Journal of Vertebrate Palaeontology 10(4) (2013), 1-11. ISSN 1567- 2158. 11 pages + 3 figures, 1 table. Keywords: Bison, Biogeography, Arizona, Southwest historical ecology ABSTRACT The American bison are traditionally thought of as animals of the vast plains and grasslands, but paleontological and archaeological evidence supports the view that the biogeographic range of bison extended throughout the continental United States to include the American Southwest and Arizona. During the Pleistocene (2,588,000 BP to 11,700 BP), there are several paleontological and archaeological signatures of bison herds in Arizona. From approximately 12,000 BP to AD 1 there is no evidence for bison in the area. This changes around AD 1 when the climate became more favorable, and bison expanded back into Arizona. The last historic bison remains in Arizona date to AD 1650. From AD 1650 until the early 1900s, there are no bison documented in Arizona. Reintroduction of bison to Arizona’s national forests and ran- ches began in the early 1900s and continues to today. Bison can still be seen on the Arizona landscape demonstrating the temporal longevity of the biogeographic distribution of bison in Arizona. © PalArch Foundation 1 Wolff, TER-QUA PalArch’s Journal of Vertebrate Palaeontology, 10(4) (2013) Introduction Arizona is a somewhat surprising area to find bison because of the desert ecology that Biogeographic distribution of bison as previous- dominates the state today. -
Tule Springs Fossil Beds National Monument National Monument
National Park Service Tule Springs Fossil Beds U.S. Department of the Interior Tule Springs Fossil Beds National Monument National Monument Park Assets Size 22,650 acres Economic Impact Not yet measured Annual Visitation Not yet counted Tule Springs Fossil Beds National Monument was established as the 405th Park Infrastructure unit of the National Park Service Dec. 19, 2014. Scientific investigations of No park facilities the area began in the early 1900s, culminating in the 1962-63 Tule Springs expedition. A long scientific hiatus ended with exhaustive paleontological Natural Resources excavations in the 2000s. These scientific excavations and findings have • The geologic deposits in the park go back shown that the park contains the single largest and most diverse open- at least 300,000 years. Paleontologists have site assemblage of vertebrate fossils from the end of the Pleistocene discovered megafauna fossils dating between epoch found in the Mojave Desert and the southern Great Basin. While 100,000 to 13,000 years ago. Extinct large there are no facilities or marked trails at the park, at this time, there are mammals that once inhabited the area opportunities to explore more of the story and see some of the fossils. include the North American lion, Columbian The National Park Service has an exhibit on display at the Nevada State mammoth, saber-toothed cat, dire wolf, horse, Museum in Las Vegas. bison and camel and the giant ground sloth. Smaller animals, such as squirrel, marmot, vole Park Purpose and gopher have been found, along with birds The purpose of Tule Springs Fossil Beds National Monument is to conserve, like the extinct teratorn, hawk, duck and owl. -
Westside Subway Extension
Appendix C GIS Archaeological Predictive Study 101 170 101 2 WEST HOLLYWOOD 101 405 BEVERLY 2 HILLS LOS ANGELES 405 10 2 10 Legend 10 sensitivity_2 SANTA 187 MONICA GRIDCODE 405 1 1 2 CULVER 3 1 CITY 0 2,000 4,000 4 Feet 187 0 0.25 0.5 0.75 1 1 187 Miles 5 405 1 inch = 4,000 feet 1:48,000 City Boundary 2 101 BEVERLY 110 5 HILLS 101 10 10 110 5 101 10 10 187 10 60 LOS 5 ANGELES COMMERCE CULVER CITY VERNON 110 MAYWOOD 405 90 90 Legend sensitivity_2 INGLEWOOD HUNTINGTON GRIDCODE PARK 1 BELL 405 2 3 INGLEWOOD 0 2,000 4,000 4 CUDAHY Feet 0 0.25 0.5 0.75 1 Miles 5 1 inch = 4,000 feet SOUTH 405 1:48,000 City Boundary GATE 101 170 101 2 WEST HOLLYWOOD 101 405 BEVERLY 2 HILLS LOS ANGELES 405 10 2 10 Legend 10 sensitivity_2 SANTA 187 MONICA GRIDCODE 405 1 1 2 CULVER 3 1 CITY 0 2,000 4,000 4 Feet 187 0 0.25 0.5 0.75 1 1 187 Miles 5 405 1 inch = 4,000 feet 1:48,000 City Boundary Memorandum Date: August 10, 2009 To: Laurie Solis From: Mark Neal Subject: MTA Westside Expansion Predictive Model Feasibility Executive Summary The purpose of this memorandum is to report on the results of a study of the feasibility of creating a geographical information system (GIS)-based model to predict the potential for the presence of previously undiscovered historic and prehistoric resources within the Area of Potential Effect (APE) of the Metro Transit Authority’s proposed Westside Expansion of the Metro Rail system. -
Palaeontologia Electronica COMPARATIVE VARIABILITY OF
Palaeontologia Electronica http://palaeo-electronica.org COMPARATIVE VARIABILITY OF INTERMEMBRANOUS AND ENDOCHONDRAL BONES IN PLEISTOCENE MAMMALS Kristina R. Raymond and Donald R. Prothero ABSTRACT Study of the embryology and ossification of modern bones predicts that fossil intermembranous bones (which ossify from connective tissue) will exhibit greater size variability than endochondral bones (which are formed from embryological cartilagi- nous precursors), because intermembranous bones are less tightly constrained by joints and articular surfaces. To evaluate this hypothesis, we measured multiple dimen- sions of 989 intermembranous bones (patellae and other sesamoids) of the saber- toothed cat Smilodon fatalis, the Ice Age lion Panthera atrox, the bison Bison antiquus, the horse Equus occidentalis, the camel Camelops hesternus, the ground sloths Paramylodon (=Glossotherium) harlani and Nothrotheriops shastensis from Rancho La Brea and from the late Pleistocene San Josecito Cave in Nuevo Leon, Mexico. These were compared to measurements of 811 endochondral bones (primarily astragali) of comparable size. Through statistical analyses (coefficients of variation, ANOVA, modi- fied Levene’s test, and t-tests) we found slight evidence of higher variability in many of the intermembranous bones of these taxa (21 out of 27 CVs were higher for intermem- branous bones than endochondral bones), although this trend is not found in all taxa. Using a modified Levene’s test, only Smilodon and some of the dimensions of horse and bison patellae are significantly more variable than the corresponding dimensions of the astragali. Although the results are mixed, at least some data show that inter- membranous bones are not as tightly constrained by growth and by adjacent tissues as are endochondral bones. -
The Geology and Paleontology of Tule Springs Fossil Beds National Monument, Nevada
The Geology and Paleontology of Tule Springs Fossil Beds National Monument, Nevada On December 19, 2014, Tule Springs Fossil Beds National Monument in Nevada was established by Congress as the 405th unit of the National Park Service to “conserve, protect, interpret, and enhance for the benefit of present and future generations the unique and nationally important paleontological, scientific, educational, and recreational resources and values of the land” (P.L. 113-291, sec. 3092). Photograph by Eric Scott, Cogstone Resource Management, Inc., used with permission. The upper Las Vegas Wash cuts through sediments formed by ancient springs and marshes that blanketed the Las Vegas Valley floor during the Pleistocene Epoch. These deposits have yielded thousands of vertebrate fossils and contain valuable information on past climatic and environmental conditions. This is Tule Springs Fossil Beds National Monument. A Brief History of Tule Springs techniques with massive earth-moving animals (Haynes, 1967). Consequently, activities. Heavy construction equipment the hypothesis that early humans coexisted Vertebrate fossils have been known carved enormous trenches into the sedi- with Pleistocene megafauna at Tule from the Las Vegas Valley for more than ments at Tule Springs to expose vertical Springs was disproven, and interest in the a century, beginning in 1903 when Josiah walls as deep as 13 meters (nearly site faded. A long intermission in scientific Spurr of the U.S. Geological Survey 43 feet!), which allowed the sediments to research followed, lasting until the 2000s reported teeth and bones in the sedi- be studied in detail. Geologist C. Vance when museum scientists conducted com- ments exposed in the wash between Corn Haynes, Jr., directed the geological inves- prehensive and systematic paleontological Creek Springs and Tule Springs (Spurr, tigations and subdivided the fossil-rich excavations of the area. -
Bison Antiquus Occurrence and Pleistocene-Holocene Stratigraphy, Canada Del Buey, Pajarito Plateau, New Mexico Paul G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/58 Bison Antiquus occurrence and Pleistocene-Holocene stratigraphy, Canada del Buey, Pajarito Plateau, New Mexico Paul G. Drakos, Steven L. Reneau, and Gary S. Morgan, 2007, pp. 441-448 in: Geology of the Jemez Region II, Kues, Barry S., Kelley, Shari A., Lueth, Virgil W.; [eds.], New Mexico Geological Society 58th Annual Fall Field Conference Guidebook, 499 p. This is one of many related papers that were included in the 2007 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. -
Nevada State Museum Anthropological Papers No
NEVADA STATE MUSEUM ANTHROPOLOGICAL PAPERS NO. 13 PART 3 POLLEN ANALYSIS OF THE YULE SPRINGS AREA, NEVADA by PETER J. MEHRINGER, JR. GEOCHRONOLOGY LABORATORIES UNIVERSITY OF ARIZONA TUCSON, ARIZONA Carson City, Nevada October, 1967 • TABLE OF CONTENTS Page INTRODUCTION . • • • • • • 132 POLLEN ANALYSIS AND SOUTHWESTERN ARCHAEOLOGY 132 COLLECTION OF POLLEN SAMPLES . 135 EXTRACTION OF POLLEN . • • 136 INTERPRETING THE FOSSIL POLLEN RECORD . 138 THE STUDY AREA . 146 VEGETATION AND MODERN POLLEN SAMPLES. 149 THE FOSSIL POLLEN RECORD • 169 DISCUSSION. 186 A PLEISTOCENE (WISCONSIN) CORRIDOR IN THE EASTERN MOHAVE DESERT . 189 SUMMARY AND CONCLUSIONS. 193 REFERENCES CITED . 194 ILLUSTRATIONS Color Plate. Pleistocene pollen from the Las Vegas Valley, Nevada. (ca. 640x) . Facing 129 Figure 1. Photomicrographs of pollen from human coprolites . 133 2. Panamint Mountains modern pollen surface samples . 140 3. Modern pollen surface samples, Tule Springs and Corn Creek Sites 142 4. Lehner Ranch Arroyo. Pollen Profiles II, VII . 145 5. Map of Study Area. 147 6. View of the Tule Springs Area . 148 7. Pollen diagram of major pollen types from Kyle Canyon, Charleston Mountains . 151 8. Soil surface sample, Locality 25 . 153 9. Modern spring sample, Locality 28 153 10. View from the Tule Springs Site . 153 11. Modern surface sample, Locality 1, Kyle Canyon . 153 12. Modern sample, Locality 27, at Corn Creek Spring . 154 13. Modern surface sample, Locality 5, on Kyle Canyon Fan . 156 14. Vegetation between modern surface sample, Localities 9 and 10 in Kyle Canyon . 156 15. Modern surface sample, Locality 12, in Kyle . 156 16. Modern surface sample, Locality 15, in Kyle Canyon . 156 17. -
The Holocene History of Bison in the Intermountain West: a Synthesis of Archaeological and Paleontological Records from Eastern Oregon
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 2-2004 The Holocene History of Bison in the Intermountain West: A Synthesis of Archaeological and Paleontological Records from Eastern Oregon Nicole Anne Stutte Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Archaeological Anthropology Commons Let us know how access to this document benefits ou.y Recommended Citation Stutte, Nicole Anne, "The Holocene History of Bison in the Intermountain West: A Synthesis of Archaeological and Paleontological Records from Eastern Oregon" (2004). Dissertations and Theses. Paper 2257. https://doi.org/10.15760/etd.2254 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. THESIS APPROVAL The abstract and thesis of Nicole Anne Stutte for the Master of Arts in Anthropology were presented February 11, 2004, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: Michael T. Murphy Representative of the Office of Graduate Studies DEPARTMENT APPROVAL: Department of Anthropology ABSTRACT An abstract of the thesis of Nicole Anne Stutte for the Master of Arts in Anthropology presented February 11, 2004. Title: The Holocene History of Bison in the Intermountain West: A Synthesis of Archaeological and Paleontological Records from Eastern Oregon. Intermountain West bison abundance and chronology is much debated, but little work addressing these debates has occurred in eastern Oregon. Historic records indicate bison were absent from eastern Oregon at Euro-American contact. -
Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the Use of Paleobiology for Natural Resource Management Policy Jeffrey M
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2014 Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy Jeffrey M. Martin East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, Paleobiology Commons, and the Paleontology Commons Recommended Citation Martin, Jeffrey M., "Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy" (2014). Electronic Theses and Dissertations. Paper 2360. https://dc.etsu.edu/ etd/2360 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy ______________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences ______________________ by Jeff M. Martin May 2014 ______________________ Jim I. Mead, Chair Blaine W. Schubert Steven C. Wallace Keywords: Bison, Grand Canyon, Paleontology, Conservation, Geospatial, Paleobiology 1 ABSTRACT Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy by Jeff M. -
SHPO Letter 6 12 20
NEVADA Department of Conservation and Natural Resources STATE HISTORIC PRESERVATION OFFICE _Steve Sisolak, Governor Bradley Crowell, Director Rebecca L. Palmer, Administrator, SHPO June 12, 2020 DianeC.Siebrandt, PhD Historic Preservation Officer City of Las Vegas Dept. of Planning 333 N. Rancho Drive, 3rd Floor Las Vegas, NV 89106 RE: Hay Barn Rehabilitation, Floyd Lamb Park at Tule Springs, 9200 Tule Springs Road, Las Vegas, dark County, Nevada Dear Ms. Siebrandt: The Nevada State Historic Preservation Office (SHPO; defined as "State" in the Commission for Cultural Affairs Covenants) received the response letter and attachments for the Hay Barn rehabilitation project at Tule Springs Ranch (in Floyd Lamb Park) on May 13, 2020 and has reviewed it in accordance with the CCA Covenant that remains in effect until December 31, 2034. The SHPO's review has been conducted in accordance with The Secretary of the Interior's Standards for the Treatment of Historic Properties, Standards for Rehabilitation (Standards). The City of Las Vegas (City) submitted the materials in response to a SHPO letter dated April 14, 2020. Thank you for the response and supplementary material. The SHPO has reviewed the current submission and has the following comments. Acceptable Items Thank you for providing clarification on the following scope of work items, all of which are acceptable: • New Exits - The City has clarified that the new exits on the south elevation of the Hay Barn will be located within the third bays from each end. • Security Nylon Mesh Attachment - The SHPO acknowledges that the City intends to utilize the existing mechanical fasteners and clips to attach the new mesh. -
Rancholabrean Vertebrates from the Las Vegas Formation, Nevada
Quaternary International xxx (2017) 1e17 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint The Tule Springs local fauna: Rancholabrean vertebrates from the Las Vegas Formation, Nevada * Eric Scott a, , Kathleen B. Springer b, James C. Sagebiel c a Dr. John D. Cooper Archaeological and Paleontological Center, California State University, Fullerton, CA 92834, USA b U.S. Geological Survey, Denver Federal Center, Box 25046, MS-980, Denver CO 80225, USA c Vertebrate Paleontology Laboratory, University of Texas at Austin R7600, 10100 Burnet Road, Building 6, Austin, TX 78758, USA article info abstract Article history: A middle to late Pleistocene sedimentary sequence in the upper Las Vegas Wash, north of Las Vegas, Received 8 March 2017 Nevada, has yielded the largest open-site Rancholabrean vertebrate fossil assemblage in the southern Received in revised form Great Basin and Mojave Deserts. Recent paleontologic field studies have led to the discovery of hundreds 19 May 2017 of fossil localities and specimens, greatly extending the geographic and temporal footprint of original Accepted 2 June 2017 investigations in the early 1960s. The significance of the deposits and their entombed fossils led to the Available online xxx preservation of 22,650 acres of the upper Las Vegas Wash as Tule Springs Fossil Beds National Monu- ment. These discoveries also warrant designation of the assemblage as a local fauna, named for the site of the original paleontologic studies at Tule Springs. The large mammal component of the Tule Springs local fauna is dominated by remains of Mammuthus columbi as well as Camelops hesternus, along with less common remains of Equus (including E.