DOCSLIB.ORG

Environmental Documents 2 of 2

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Environmental Documents 2 of 2 IrorfTl B I .TOl'N R. BYERLY. INC. I I Z Test Pit No. 6 I- Z Q >' uJ .... (!) .... U I 0:- ~ Z- <~ 0....0.. .... ....tz_ </l ::\:Z z.:;: u3 0.... uJ~ ....u vU l.:)U:- ~~ 0:0: a: ~ Izo.. ~ ....'u a.. >- :Jlt >0.. w >:11: 0: .... ~ - ~ o -- 0 I/) .... ! 6 ....~ I ~ a: o pli . Lt. brown fine to coarse sand (SW) I 100 0.5 86 '. ' .. (dry, moderately dense) 97 3.6 80 1 2 •I- ..... '.' I . ." It:l . ' .. 3 pte .' . 95 1.5 82 I 4 l- '.... 5 6 I ., '":." Grey fine to coarse sand (SW) I- '., (dry, loose) 7 ' .. I - 8 9 Total depth 10.0 feet I 10 H---l No free ground water encountered 11 I- I 12 I- Caving below 6.0 feet . I 13 I- 14 I- I 15 I- 16 I- I 17 I- 18 I- 19 I- Enclosure 2, Page 6 I Rpt. No.: 8844 20 File No.: S-4559 I ; orlTl 8 I .ro '.'i R. BYERl'{, INC. I I I Z I-z Q >-' uJ ..... l-' ..... U Tes' Pit No. 7 0:- t: z~ o(~ .... t;: 0.. .... I z_ Vl 0.....~z z.~ u~ 0.... .... t;: ........ U OU l,:). o~ w0:0:: 0: .... ,.., z0.. z~ :>- - :::di~ >0.. W I >:.: 0:: .... o 0 I/) - ....-- -- (5 ~ 2S .oJ ~ a: ·1 o Lt. brown fine to coarse sand (SW) (dry, loose, porous) 1 I 90 4.2 75 2 3 I 90 5.3 74 4 I I' 99 2.6 82 5 I 6 Grey, 1t , brown fine to coarse sand Is w/lenses of silt, (dry & loose) 7 8 I 9 10 I 11 Total depth 11.0 feet 12 No free ground water encountered I . 13 No caving 14 I . 15 16 I 17 I 18 Enclosure 2, Page 7 19 Rpt. No.: 8844 File No.: S-4559 I 20 I .JOHN R. BYERLY, INC. 1 1 I ..... z z Q '>- W ..... ~ r- Ll cr- ~ Z- <- Test Pit No. 8 wI: or- o.r- I Z_ .n ~Z U~ W z:;: OW .... U ULl :r C),t ~~ a: ~ a: a: 0. Z~ w'''' W >- - ~~ >0. o 1 >:1' a: r- - r-- 0 en - ~-- 0 S ~ a::.,j Lt. brown fine to coarse sand (5W) I 0 JlII''. ...I' . (dry, slightly dense, w/some silt) 77 I 91 1.5 1 • 'f.-:r 94 2.0 82 .... 2 i- .. 3 ',1 : I 92 2.0 80 1. -, 4 ... , , ,I', ' I 5 i- .: ,I, 6 Lt. brown to grey interbedded fine to coarse sands, (dry, loose) I 7 i- i- ' , , 8 " , , I 9 i- 10 l- I Total depth 11.0 feet II No free ground water encountered 1 12 .... 13 ~ No caving 1 14 i....- 15 .... 1 16 I- 17 I- 1 18 >- Enclosure 2, Page 8 19 i- Rpt. No.: 8844 File No.: 5-4559 1 20 .1 I Jm,~ R. BYERLY. INC. I I z I ~ z 0 >-'" uJ ~ l-' U Test Pit no. 9 er- ~. r- <~ .... t;: z- O-~ I LIl Oz ~Z Z_ Z- W ....U ....OW ....t;: U uU :x: ~. O~ era::w a:: I- ~ W".1 a. Z~ ~ ;:)~ >0- w ,I S;:lII:_ .... a:: I- - - ~ o 0 en r- ~ 6 ~ ~ a::.oJ I o Grey fine to coarse sand (SW) (dry, moderately dense) 1 . ·1 101 2.6 87 .. 2 99 2.0 83 3 I· 4 'I '. 5 100 1.5 85 6 7 I· 8 I 9 Total depth 9.5 feet 10 No f~ee ground water encountered I 11 Caving below 3.0 feet 12 I 13 14 '1 I . 15 16 I 17 I 18 Enclosure 2, Page 9 Rpt. No.: 8844 19 File No.: 5-4559 I 20 I I for"" 8 JOHN R. BYERLY. INC. I I Z I ...- Q >- Z ...- .<tJ w U a:~ t: z~...- <~ Test Pit No. 10 ....t 0'" 0.. .... I z_ in J:Z u3 0"" ....t z= wU oU C). ~l! er j!: erer ,... a. z~ >- ::::>~ .... w >~ er - >0.. o I 0 (I).... - ....-- !-- (5 :) I ~ a:.oJ 0 .. Grey fine to coarse sand (SW) 94 1.0 80 I (dry & slightly dense w/some silt 1 :. ... and gravel) I 95 1.0 80 2 '.l- • I 91 1.0 77 3 0 D 4 1-. .. I 5 I- .. ' Total depth 6.0 feet 6 No free ground water encountered I 7 I- 8 ~ Caving below 1.0 feet I 9 ~ I 10 l- II I- , 12 ~ 13 I- I 14 I- 15 I- I 16 I- 17 I- I 18 I- Enclosure 2, Page 10 Rpt. No.: 8844 19 I- File No.: S-4559 I 20 I JO~:;~ R. BYERLY. INC. I I I Z ,I I- 0 >- .....Z I- Test Pit No. 11 ~ .... U 0::- ~ <~ 01-z- Q.I- ....tZ VI :l: Z, ..... - z.-.. u5 OW I wU vU l:)t;; ~~ 0::0:: 0:: ~ ~ w·u a.. z~ >- ::J~ >Q. w S;:l' 0:: I- ~ - ~ o 0 en I- I ~-- 0 :5 ~ ',j 0:: I 0 Lt. brown fine to coarse sand (SW) I -,: 'I 1 (dry, mod. dense w/some silt) 96 3.6 82 I'". ' . ·1 ' . 2 I " I, 102 3.6 87 3 . " I· I 4 5 'I' , , I I ,I " 6 Total depth 6.0 feet 7 No free ground water encountered I 8 Caving below 1.0 feet 9 I' 10 I 11 12 I 13 : 14 'I . 15 16 I 17 18 I Enc 108uI',;;: 2, Page 11 19 Rpt. No.: 8844 File No.: S-4559 20 I I Iform '8 JOHN R. BYERLY. INC. I I _. z I ... 0 Test Pit No. 12 z • >- W ... I!J U cr- t: ... <- wt;: z- 0.. ... I z_ VI 0'" ~z z.~ U~ OW I .... t; ~~ wU oUa: l-'. a:a: ~ zo.. .r w'''' w a: - :::>~ >0.. >:llC_'OJ ... o I 0 V'I - t--- ! O ....5 I ~ ex: o ~7 .... Grey to It. bro~l fine to coarse sand 80 2.0 70 1 .:.... (5W) (dry, loose, w/some silt) '. " I 77 2.5 67 · . " 2 I- .': . · ..'", I- ' ... 3 . ' . I . ~ ' .. 4 " .'. I 5 6 ....... I 7 ~ . .... ,' ." I 8 9 ~ .' I- :.... 10 . '. I ' ... 11 I- · . 12 I- . I · .' 13 I- :..... 14 Total depth 14.0 feet I , 15 ~ No free ground water encountered 16 I- Caving below 3.0 feet I. 17 .... I 18 I- Enclosure 2, Page 12 19 I- Rpt. No.: 8844 File No.: 5-4559 I 20 ~-~ I forl'\ 8 JOHN R. BYERLY, INC. I I I z I ... 0 >- ....z ... (!J U Test Pit No. 13 lr- ~ ... o(~ z~ Cl. ... wt;: l.f) z_ z.~ 0'" ~z I ....... u3 0.... ....t ....u vU t:). o~_. a:: a:: a:: ~ w hJ c, z~ ~ ::)~ w ~:ll:: >Cl. a:: I- - - a -- 0 en I- - I ! 0 ....5 ~ a:: ,I o Lt. brown fine to coarse sand (SW) 88 2.0 76 1 (dry. loose w/some silt) ,I 2 3 85 4.2 73 Lt. brown fine to coarse sand (SW) I I 4 (dry, loose) I " 5 I I' Lt. brown silty fine to coarse sand (Sr- 6 (dry, loose) 7 I 8 9 I 10 Total depth 10.0 feet I 11 No free groun~ water encountered 12 No caving .1 13 14 I 15 16 I 17 18 Enclosure 2, Page 13 I 19 Rpt. No.: 8844 File No.: S-4559 20 I I I JOFN H. BYERLY. INC. I I ~ z Q Test Pit No. 14 I '>- wz ~ V' U I- <0(_ a- t: z- o..~ wt <I'l 0 .... z_ U~ ~z wI- z:: OW I U U ,I.IJ a: V a: ~ '-'~ o~~ a:1.IJ w,u a. z~ ~ ::::>~ >0.. I.IJ >:01: a: I- ~ - ~ o -- 0 cJ) ~ I ~ 6 .u:s ~ a: I 0 , I' ,I,' " ' Lt. brown silty fine to coarse sand (S~ 87 2.6 75 I 1 ,....I : I (dry, loose) 94 1.0 79 2 ~.I,·T I 3 ,... .. I. I 4 ,...,~"·I: I 5 ;.. ',I',. i 6 -1':1',.. _ 0 •• Occasional gravels at 7.0 fe~t 7 I 1.1 ." '0 I" 8 f- . (. ~ o , ' 0 I 9 f- .1·" Total depth 9.5 feet 10 - No free ground water encountered 11 I - No caving 12 - I 13 - 14 - I 15 f- I 16 - 17 - 18 I - Enclosure 2, Page 14 19 Rpt. No.: 8844 - File No.: S-4559 I 20 I JOHN R. BYERLY. INC. I ,I I z ~ Q Test Pit No. 15 >- ...,z ~ I l!l .... U a- t: <- .... t;: z- Q.~ z_ iii 0 .... ~z ........ z-~ u3 0"" I ....u oU t.:)"'=' ~~ IX IX IX s Z~ ;:l .... W hJ 11. ~ - >11. w S;:'lI:: IX ... ~ o 0 U) ...-- !-- 5 5 I ~ .... Ill: I o Lt. brown silty fine to coarse sand (SM 82 0.5 71 1 (dry, loose) I, 2 3 87 1.5 75 I 4 5 Occasional gravels at 5.0 feet " I 6 Lt. brown fine to coarse sand (SW) 7 ... I . '., 8 9 I " " .' ' .. ",. 10 Total depth 10.0 feet 11 No free ground water encountered. I 12 No caving 13 I 14 ,. I I· 15 16 I 17 18 Enclosure 2, Page 15 I 19 Rp t . No.: 8844 File No.: S-4559 20 ~-~ ,I I I, TEST DATA I LABORATORY STANDARD: ASTM D 1557-70, Mehtod A: 4-Inch Diamter Hold; 1/30 Cubic Foot Volume; 5 Lay ers ; 25 BLows Per Layer; 10 I Pound Hanmer; 18 Inch Fall; -No.4 Material. Optimum Maximum I Classification Noisture(/o) Density(PCF) A Lt. brown fine to coarse sand (SW) 12.0 115.5 ,I B Lt.
Load more

Recommended publications
  • Vegetation and Fire at the Last Glacial Maximum in Tropical South America
    Past Climate Variability in South America and Surrounding Regions Developments in Paleoenvironmental Research VOLUME 14 Aims and Scope: Paleoenvironmental research continues to enjoy tremendous interest and progress in the scientific community. The overall aims and scope of the Developments in Paleoenvironmental Research book series is to capture this excitement and doc- ument these developments. Volumes related to any aspect of paleoenvironmental research, encompassing any time period, are within the scope of the series. For example, relevant topics include studies focused on terrestrial, peatland, lacustrine, riverine, estuarine, and marine systems, ice cores, cave deposits, palynology, iso- topes, geochemistry, sedimentology, paleontology, etc. Methodological and taxo- nomic volumes relevant to paleoenvironmental research are also encouraged. The series will include edited volumes on a particular subject, geographic region, or time period, conference and workshop proceedings, as well as monographs. Prospective authors and/or editors should consult the series editor for more details. The series editor also welcomes any comments or suggestions for future volumes. EDITOR AND BOARD OF ADVISORS Series Editor: John P. Smol, Queen’s University, Canada Advisory Board: Keith Alverson, Intergovernmental Oceanographic Commission (IOC), UNESCO, France H. John B. Birks, University of Bergen and Bjerknes Centre for Climate Research, Norway Raymond S. Bradley, University of Massachusetts, USA Glen M. MacDonald, University of California, USA For futher
    [Show full text]
  • 1 the Stratigraphic Record of Changing Hyperaridity in the Atacama Desert Over the 1 Last 10 Ma 2 3 4 5 6 7 8 9 10 11 12 13 14 1
    *Manuscript Click here to view linked References 1 1 The stratigraphic record of changing hyperaridity in the Atacama Desert over the 2 last 10 Ma 3 Alberto Sáez1*; Lluís Cabrera1; Miguel Garcés1, Paul van den Bogaard2, Arturo Jensen3, Domingo 4 Gimeno4 5 1 Departament d’Estratigrafia, Paleontologia i Geociencies Marines, Grup de Geodinàmica i Anàlisi de Conques, 6 Universitat de Barcelona, Spain. *Corresponding author: [email protected] 7 2 GEOMAR | Helmholtz Centre for Ocean Research Kiel, Germany 8 3 Departamento de Ciencias Geológicas. Universidad Católica del Norte. Antofagasta, Chile. 9 4 Departament de Geoquímica, Petrologia i Prospecció Geológica. Universitat de Barcelona, Spain. 10 11 ABSTRACT 12 New radiometric and magnetostratigraphic data from Quillagua and Calama basins (Atacama Desert) 13 indicate that the stratigraphic record over the last 10 Ma includes two hiatuses, lasting approximately 2 and 4 14 million years respectively. These sedimentary gaps are thought to represent prolonged periods of 15 hyperaridity in the region, with absence of sediment production and accumulation in the central depressions. 16 Their remarkable synchrony with Antarctic and Patagonian glacial stages, Humboldt cold current 17 enhancement and cold upwelling waters lead us to suggest long-term climate forcing. Higher frequency 18 climate (orbital precession and eccentricity) forcing is thought to control the sequential arrangement of the 19 lacustrine units deposited at times of lower aridity. Hyperaridity trends appear to be modulated by the activity 20 of the South American Summer Monsoon, which drives precipitation along the high altitude areas to the east 21 of Atacama. This precipitation increase combined with the eastward enlargement of the regional drainage 22 during the late Pleistocene enabled water transfer from these high altitude areas to the low lying closed 23 Quillagua basin and resulted in the deposition of the last widespread saline lacustrine deposits in this 24 depression, before its drainage was open to the Pacific Ocean.
    [Show full text]
  • A World Revealed by Language: a New Seri Dictionary and Unapologetic Speculations on Seri Indian Deep History
    A World Revealed by Language: A New Seri Dictionary and Unapologetic Speculations on Seri Indian Deep History JIM HILLS AND DAVID YETMAN Comcáac quih Yaza quih Hant Ihíip hac: Diccionario Seri-Español- Ingles, compiled by Mary Beck Moser and Stephen A. Marlett. Illustrated by Cathy Moser Marlett. Published by Plaza y Valdés Editores, Mexico City. 947 pages. ISBN: 970–722–453–3. The philosopher Ludwig Wittgenstein once mentioned that to imagine a language was to imagine a form of life (Wittgenstein 1953: 19). A comprehensive dictionary of any language exemplifies Wittgenstein’s point, but none more than the trilingual dictionary of the Seri language compiled by Mary Beck Moser and Steven Marlett. The work represents more than fifty years of research and over thirty years of living with the Seris in El Desemboque, Sonora, Mexico, in connection with the Summer Institute of Linguistics of the Wycliffe Bible Translators. The entries are in Seri, Spanish, and English, making the work of value to speakers of all three languages. The roughly six hundred Seris are already using the dictionary. Outsiders visiting them would be well advised to use it as well. The authors included Seri consultants at every step of the compilation. Seris reviewed the entries, suggesting changes and additions. Part of the dictionary’s usefulness lies in its incorporation not merely of single-word or phrase translations, but also of sentences or short paragraphs typically generated by Seris. This is critically important, since meanings are frequently so complex that a simple word-by-word translation simply will not do. As Moser and Marlett have realized, JIM HILLS is a longtime Seri hand and trader in Tucson, Arizona.
    [Show full text]
  • Sonny Bono Salton Sea National Wildlife Refuge Complex
    Appendix J Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex Appendix J: Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex The following sections describe the cultural setting in and around the two refuges that constitute the Sonny Bono Salton Sea National Wildlife Refuge Complex (NWRC) - Sonny Bono Salton Sea NWR and Coachella Valley NWR. The cultural resources associated with these Refuges may include archaeological and historic sites, buildings, structures, and/or objects. Both the Imperial Valley and the Coachella Valley contain rich archaeological records. Some portions of the Sonny Bono Salton Sea NWRC have previously been inventoried for cultural resources, while substantial additional areas have not yet been examined. Seventy-seven prehistoric and historic sites, features, or isolated finds have been documented on or within a 0.5- mile buffer of the Sonny Bono Salton Sea NWR and Coachella Valley NWR. Cultural History The outline of Colorado Desert culture history largely follows a summary by Jerry Schaefer (2006). It is founded on the pioneering work of Malcolm J. Rogers in many parts of the Colorado and Sonoran deserts (Rogers 1939, Rogers 1945, Rogers 1966). Since then, several overviews and syntheses have been prepared, with each succeeding effort drawing on the previous studies and adding new data and interpretations (Crabtree 1981, Schaefer 1994a, Schaefer and Laylander 2007, Wallace 1962, Warren 1984, Wilke 1976). The information presented here was compiled by ASM Affiliates in 2009 for the Service as part of Cultural Resources Review for the Sonny Bono Salton Sea NWRC. Four successive periods, each with distinctive cultural patterns, may be defined for the prehistoric Colorado Desert, extending back in time over a period of at least 12,000 years.
    [Show full text]
  • Exploring the Function of Lake Cahuilla Fish Traps
    UC Merced Journal of California and Great Basin Anthropology Title Fish Traps on Ancient Shores: Exploring the Function of Lake Cahuilla Fish Traps Permalink https://escholarship.org/uc/item/1hk9f8px Journal Journal of California and Great Basin Anthropology, 29(2) ISSN 0191-3557 Authors White, Eric S. Roth, Barbara J. Publication Date 2009 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Journal of California and Great Basin Anthropology | Vol. 29, No. 2 (2009) | pp. 183–193 REPORT Fish Traps on Ancient Shores: California and occupied the Salton Trough. Today’s Salton Sea occupies the same geographic location, but is Exploring the Function of much smaller (Fig. 1). The lake formed when the deltaic Lake Cahuilla Fish Traps activity of the Colorado River caused a shift in its course, causing it to flow northward into the Salton Trough ERIC S. WHITE and creating a large freshwater lake. Lake Cahuilla was K6-75, Pacific Northwest National Laboratory, six times the size of the Salton Sea, measuring at its PO Box 999, Richland, WA 99352 maximum 180 km. in length and 50 km. in width, making Barbara J. Roth it one of the largest Holocene lakes in western North Department of Anthropology, University of Las Vegas, Las Vegas, Nevada 89154-5003 America. The Colorado Desert is one of the most arid regions in the West, so the presence of a large freshwater This paper examines the use of V-style fish traps on the lake would have been a significant environmental feature western recessional shorelines of ancient Lake Cahuilla.
    [Show full text]
  • The Salton Sea California's Overlooked Treasure
    THE SALTON SEA CALIFORNIA'S OVERLOOKED TREASURE by Pat Laflin Canoeing off Date Palm Beach, Salton Sea TABLE OF CONTENTS PART I BEFORE THE PRESENT SEA Page Chapter 1 The Salton Sea-Its Beginnings 3 Chatpter 2 Lost Ships of the Desert 9 Chapter 3 The Salt Works 11 Chapter 4 Creating the Oasis 13 Chapter 5 The Imperial Valley is Born 17 Chapter 6 A Runaway River 21 PART II LIVING WITH THE SEA Chapter 7 Remembering the Salton Sea's First 31 Years Chapter 8 Mudpots, Geysers and Mullet Island 33 Chapter 9 Sea of Dreams 37 Chapter 10 Speedboats in the Desert 45 Chapter 11 Fishing the Salton Sea 51 Chapter 12 Where Barnacles Grow on the 53 Sage PART III WHAT ABOUT THE FUTURE? Chapter 13 Restoring the Salton Sea 57 Bibliography 58 Postscript 59 THE SALTON SEA CALIFORNIA'S OVERLOOKED TREASURE PART I BEFORE THE PRESENT SEA Chapter 1 THE SALTON SEA -- ITS BEGINNINGS The story of the Salton begins with the formation of a great shallow depression, or basin which modem explorers have called the Salton Sink. Several million years ago a long arm of the Pacific Ocean extended from the Gulf of California though the present Imperial and Coachella valleys, then northwesterly through the Sacramento and San Joaquin valleys. Mountain ranges rose on either side of this great inland sea, and the whole area came up out of the water. Oyster beds in the San Felipe Mountains, on the west side of Imperial Valley are located many hundreds of feet above present sea level.
    [Show full text]
  • SANDSTONE FEATURES ADJACENT to LAKE CAHUILLA Stephanie
    SANDSTONE FEATURES ADJACENT TO LAKE CAHUILLA and Stephanie Rose and Cheryl Bowden-Renna the KEA Environmental, Inc. surr 1420 Kettner Blvd, Ste. 620 qu ie San Diego, CA 92101 insic two arc~ the ABSTRACT and that Recent investigations at the Salton Sea Test Base revealed a number of features, including 110 this hearths or fire-affected rock clusters, 22 fish traps, and 198 rock enclosures. All of these features are located at very low elevations, ranging from 20 to 225 feet below sea level. Excavations in and around these features provided information on their structure and composition, as well as their possible function. as Ie Although little was recovered from the hearths and fish traps, units excavated at the rock enclosures ft le\ contained fish bone, sometimes in substantial quantities. OCCl was bo n ~ INTRODUCTION together at 16 sites, and a single site consisted of lake a hearth feature with no visible associated cultural Investigations at Salton Sea Test Base material. Subsurface examinations were (S STB) , on the west side of the Salton Sea, conducted in 40 hearths. Only about 30% of recorded 170 archaeological sites. These sites these had positive results, generally consisting of contained a total of 336 prehistoric features, a thin layer of charcoal flecks and a small amount of including 110 hearths, 22 rock constructions fish bone. Little additional cultural material was foun interpreted as fish traps, and 198 sandstone rock recovered subsurface. of tl­ enclosures. Subsurface data were provided by east. 135 shovel test pits and 25 units, placed at 159 of featL the features.
    [Show full text]
  • PDF Linkchapter
    Index [Italic page numbers indicate major references] Abajo Mountains, 382, 388 Amargosa River, 285, 309, 311, 322, Arkansas River, 443, 456, 461, 515, Abort Lake, 283 337, 341, 342 516, 521, 540, 541, 550, 556, Abies, 21, 25 Amarillo, Texas, 482 559, 560, 561 Abra, 587 Amarillo-Wichita uplift, 504, 507, Arkansas River valley, 512, 531, 540 Absaroka Range, 409 508 Arlington volcanic field, 358 Acer, 21, 23, 24 Amasas Back, 387 Aromas dune field, 181 Acoma-Zuni scction, 374, 379, 391 Ambrose tenace, 522, 523 Aromas Red Sand, 180 stream evolution patterns, 391 Ambrosia, 21, 24 Arroyo Colorado, 395 Aden Crater, 368 American Falls Lava Beds, 275, 276 Arroyo Seco unit, 176 Afton Canyon, 334, 341 American Falls Reservoir, 275, 276 Artemisia, 21, 24 Afton interglacial age, 29 American River, 36, 165, 173 Ascension Parish, Louisana, 567 aggradation, 167, 176, 182, 226, 237, amino acid ash, 81, 118, 134, 244, 430 323, 336, 355, 357, 390, 413, geochronology, 65, 68 basaltic, 85 443, 451, 552, 613 ratios, 65 beds, 127,129 glaciofluvial, 423 aminostratigraphy, 66 clays, 451 Piedmont, 345 Amity area, 162 clouds, 95 aggregate, 181 Anadara, 587 flows, 75, 121 discharge, 277 Anastasia Formation, 602, 642, 647 layer, 10, 117 Agua Fria Peak area, 489 Anastasia Island, 602 rhyolitic, 170 Agua Fria River, 357 Anchor Silt, 188, 198, 199 volcanic, 54, 85, 98, 117, 129, Airport bench, 421, 423 Anderson coal, 448 243, 276, 295, 396, 409, 412, Alabama coastal plain, 594 Anderson Pond, 617, 618 509, 520 Alamosa Basin, 366 andesite, 75, 80, 489 Ash Flat, 364 Alamosa
    [Show full text]
  • The California Deserts: an Ecological Rediscovery
    3Pavlik-Ch1 10/9/07 6:43 PM Page 15 Rediscovery Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 16 Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 17 Indians first observed the organisms, processes, and history of California deserts. Over millennia, native people obtained knowledge both practical and esoteric, necessitated by survival in a land of extremes and accumulated by active minds recording how nature worked. Such knowledge became tradition when passed across generations, allowing cul- tural adjustments to the changing environment. The depth and breadth of their under- standing can only be glimpsed or imagined, but should never be minimized. Indians lived within deserts, were born, fed, and raised on them, su¤ered the extremes and uncertainties, and passed into the ancient, stony soils. Theirs was a discovery so intimate and spiritual, so singular, that we can only commemorate it with our own 10,000-year-long rediscov- ery of this place and all of its remarkable inhabitants. Our rediscovery has only begun. Our rediscovery is not based upon living in the deserts, despite a current human pop- ulation of over one million who dwelling east of the Sierra. We do not exist within the ecological context of the land. We are not dependant upon food webs of native plants and [Plate 13] Aha Macav, the Mojave people, depicted in 1853. (H. B. Molhausen) REDISCOVERY • 17 Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 18 Gárces 1776 Kawaiisu Tribal groups Mono Mono Tribe Lake Aviwatha Indian place name Paiute Inyo Owens Valley
    [Show full text]
  • Fishingin the DESERT
    AN ARCHAEOLOGICAL TIME C APSULE • MYSTERIOUS, MAGNIFICENT C AHOKIA american archaeologyWINTER 2000–2001 american archaeologyVol. 4 No. 4 a quarterly publication of The Archaeological Conservancy FishingIN THE DESERT When a lake came and went, the Cahuilla people had to adapt. Archaeologists are learning how they did it. $3.95 american archaeology a quarterly publication of The Archaeological Conservancy Vol. 4 No. 4 winter 2000–2001 C O VER F EATURE FISHING IN THE DESERT 20 BY RICK DOWER When a vast lake suddenly formed in their desert and then gradually evaporated, the Cahuilla people were forced to adapt. 12 DISCOVERING AN ARCHAEOLOGICAL TIME CAPSULE BY LANCE TAPLEY Archaeologist Jeffrey Brain is excavating Popham Colony, an undisturbed site as old as Jamestown and in some ways more important. 27 OF MOUNDS AND MYSTERIES BY JOHN G. CARLTON AND WILLIAM ALLEN Archaeologists have been working for years at Cahokia Mounds State Historic Site to better understand the 2 Lay of the Land remarkable Mississippians. 3 Letters 34 A CULTURAL AFFILIATION CONTROVERSY 5 Events BY JOANNE SHEEHY HOOVER 7 In the News Chaco Culture National Historical Park has determined the The Slow Process of Navajo are culturally affiliated with the Anasazi. Some Repatriation • Native Americans and archaeologists strongly disagree. Archaeologists Rediscover Ancient 38 new acquisition: Maya Center • LEARNING ABOUT THE TATAVIAM Shipwreck Appears to Be Blackbeard’s The Conservancy’s acquisition of Lannan Ranch may Queen Anne’s Revenge provide important information about a little-known people. 40 new acquisition: 42 Field Notes HISTORY ON THE SHORES OF BIG LAKE 44 Expeditions Once the traditional homesite of Passamaquoddy Indian 46 Reviews chiefs, Governor’s Point in Maine is the Conservancy’s northeastern-most preserve.
    [Show full text]
  • Eagle Mountain Pumped Storage Project No. 13123 Final License Application Technical Appendices for Exhibit E, Applicant Prepared Environmental Impact Statement
    PUBLIC Eagle Mountain Pumped Storage Project No. 13123 Final License Application Technical Appendices for Exhibit E, Applicant Prepared Environmental Impact Statement. Volume 3 of 6 Palm Desert, California Submitted to: Federal Energy Regulatory Commission Submitted by: Eagle Crest Energy Company Date: June 22, 2009 GEI Project No. 080473 ©2009 Eagle Crest Energy Company 12 Appendix C – Technical Memoranda 12.9 Class I Cultural Resources Investigation for the Proposed Eagle Mountain Pumped Storage Project. A CLASS I CULTURAL RESOURCES INVESTIGATION for the PROPOSED EAGLE MOUNTAIN PUMPED STORAGE PROJECT, RIVERSIDE COUNTY, CALIFORNIA Prepared for: Eagle Crest Energy Company 1 El Paseo West Building, Suite 204 74199 El Paseo Drive Palm Desert, CA 92260 Prepared by: Jerry Schaefer ASM Affiliates, Inc. 2034 Corte del Nogal Carlsbad, California 92011 PN 14011 Keywords: USGS 7.5-minute Corn Springs, Desert Center, East of Victory Pass, and Victory Pass quads; Chuckwalla Valley, Eagle Mountain Mine, Riverside County; Desert Training Center, Camp Desert Center, World War II, Historic Trash Scatters; Class III Field Inventory. April 2009 Table of Contents TABLE OF CONTENTS Chapter Page MANAGEMENT SUMMARY .................................................................iii 1. PROJECT DESCRIPTION..............................................................1 2. ENVIRONMENTAL AND CULTURAL CONTEXT .............................5 NATURAL SETTING .............................................................................. 5 Geomorphology and Geology
    [Show full text]
  • Review and Annotated Bibliography of Ancient Lake Deposits (Precambrian to Pleistocene) G-I in the Western States As Jz;
    o 00 o H Review and Annotated Bibliography of Ancient Lake Deposits (Precambrian to Pleistocene) g-i in the Western States as Jz; GEOLOGICAL SURVEY BULLETIN 1080 02 O PH O z eq P S3 Review and Annotated Bibliography of Ancient Lake Deposits (Precambrian to Pleistocene) in the Western States By JOHN H. FETH GEOLOGICAL SURVEY BULLETIN 1080 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library catalog card for this publication appears after page 119. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract_________._.______-___--__--_---__-_-_------.--_-_-_-__ 1 Introduction.________________________----_-_-____--__-__---._-___- 2 Definitions__ _ _____________--__-_-_--__--_--___-___-___---______ 13 Maps.._____-_______--_-__--------------------------------------- 13 Criteria for the recognition of lake deposits. __-_______.___-_-__.-_____ 17 Definitive criteria____ _ _____-____-__-________---_-___-----_._ 17 Fossils. _-_--____---__-_.---_-------_-----__-_------_. 17 Evaporite deposits..._-_------_------_-------_--------_---. 20 Shore features_________---__-_-------__-_---_-_-_--_-_--_ 21 Suggestive criteria.______.-_-_--___-____---_.-____-__-____.--_. 21 Regional relations._.._-_..-____-..--...__..._..._._.._.... 21 Local evidence.___-__---_--------_--__---_-----_--------__ 22 Grain size, bedding, and lamination...._._.____.___.___.
    [Show full text]