Coast with the Most Get a Taste of Two South Carolina Destinations
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An Overview of the Cultural Resources of the Western Mojave Desert
BLM LIBRARY BURE/ IT 88014080 An Overview of the Cultural Resources of the Western Mojave Desert by E . G ary Stic kel and - L ois J . W einm an Ro berts with sections by Rainer Beig ei and Pare Hopa cultural resources publications anthropology— history Cover design represents a petroglyph element from Inscription Canyon, San Bernardino County, California. : AN OVERVIEW OF THE CULTURAL RESOURCES OF THE WESTERN TOJAVE DESERT by Gary Stickel and Lois J. Weinman- Roberts Environmental Research Archaeologists: A Scientific Consortium Los Angeles with sections by Rainer Berger and Pare Hopa BUREAU OF LAND MANAGEMENT LIBRARY Denver, Colorado 88014680 Prepared for the UNITED STATES DEPARTMENT OF INTERIOR BUREAU OF LAND MANAGEMENT California Desert Planning Program 3610 Central Avenue, Suite 402 Riverside, California 92506 Contract No. YA-512-CT8-106 ERIC W. RITTER GENERAL EDITOR Bureau of Land RIVERSIDE, CA Management Library 1980 Bldg. 50, Denver Federal Center Denver, CO 80225 *•' FOREWORD Culture resource overviews such as this bring together much of the available information on prehistoric and historic peoples and present- day Native American groups along with their associated environments. The purpose behind these studies is to provide background information for the management of and research into these prehistoric, historic, and contemporary resources. This overview is one of seven covering the southern California deserts undertaken as part of a comprehensive planning effort by the Bureau of Land Management for these deserts. Overviews aid in the day-to-day management of cultural resources and in the completion of environmental analyses and research projects. Its general value to the public in the fields of education and recreation-interpretation must also be stressed. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 116, NUMBER 5 Cfjarle* £. anb Jfflarp "^Xaux flKHalcott 3Resiearcf) Jf tmb MIDDLE CAMBRIAN STRATIGRAPHY AND FAUNAS OF THE CANADIAN ROCKY MOUNTAINS (With 34 Plates) BY FRANCO RASETTI The Johns Hopkins University Baltimore, Maryland SEP Iff 1951 (Publication 4046) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION SEPTEMBER 18, 1951 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 116, NUMBER 5 Cfjarie* B. anb Jfflarp "^Taux OTalcott &egearcf) Jf unb MIDDLE CAMBRIAN STRATIGRAPHY AND FAUNAS OF THE CANADIAN ROCKY MOUNTAINS (With 34 Plates) BY FRANCO RASETTI The Johns Hopkins University Baltimore, Maryland (Publication 4046) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION SEPTEMBER 18, 1951 BALTIMORE, MD., U. 8. A. CONTENTS PART I. STRATIGRAPHY Page Introduction i The problem I Acknowledgments 2 Summary of previous work 3 Method of work 7 Description of localities and sections 9 Terminology 9 Bow Lake 11 Hector Creek 13 Slate Mountains 14 Mount Niblock 15 Mount Whyte—Plain of Six Glaciers 17 Ross Lake 20 Mount Bosworth 21 Mount Victoria 22 Cathedral Mountain 23 Popes Peak 24 Eiffel Peak 25 Mount Temple 26 Pinnacle Mountain 28 Mount Schaffer 29 Mount Odaray 31 Park Mountain 33 Mount Field : Kicking Horse Aline 35 Mount Field : Burgess Quarry 37 Mount Stephen 39 General description 39 Monarch Creek IS Monarch Mine 46 North Gully and Fossil Gully 47 Cambrian formations : Lower Cambrian S3 St. Piran sandstone 53 Copper boundary of formation ?3 Peyto limestone member 55 Cambrian formations : Middle Cambrian 56 Mount Whyte formation 56 Type section 56 Lithology and thickness 5& Mount Whyte-Cathedral contact 62 Lake Agnes shale lentil 62 Yoho shale lentil "3 iii iv SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. -
Glaciers of the Canadian Rockies
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter -
Oil Shale 23 Shale Gas: Part 7 – Shale Gas Production Analysis and Forecasting 30 the Contribution of Azerbaijan to the World’S Oil Industry
16 Unicorns in the Garden of Good and Evil: Part 5 – Oil Shale 23 Shale Gas: Part 7 – Shale Gas Production Analysis and Forecasting 30 The Contribution of Azerbaijan to the World’s Oil Industry $10.00 MARCH 2011 VOLUME 38, ISSUE 3 Canadian Publication Mail Contract – 40070050 RESERVOIR ISSUE 3 • MARCH 2011 1 Since 1927... Build reservoir analyses. Watch your potential soar. IHS PETRA® provides a unique solution to integration, analysis and manipulation of geological, geophysical, petrophysical and engineering information. With easy data loading and a powerful and flexible database, you can both effectively manage projects and quickly visualize results using interactive mapping, cross sections, log plots, cross plots and more—all within a single system. Superior technical support and proven integration of customer enhancements make PETRA the highest-ranked 1 geological interpretation tool in the E&P industry for both reliability and accuracy and ease of use. Energy information, refined. 1 Welling & Company Geological & Geophysical Software Study, 2009 Directional Well Module 3D Visualization Module ihs.com/PETRA-cspg-1 Since 1927... MARCH 2011 – VOLUME 38, ISSUE 3 ARTICLES Unicorns in the Garden of Good and Evil: Part 5 – Oil Shale ........................................ 16 Shale Gas: Part 7 – Shale Gas Production Analysis and Forecasting ............................ 23 CSPG OFFICE The Contribution of Azerbaijan to the World’s Oil Industry ........................................ 30 #600, 640 - 8th Avenue SW Calgary, Alberta, Canada T2P 1G7 Go Take a Hike: Day Excursions Around Skoki Valley, Banff National Park ............. 32 Tel: 403-264-5610 Fax: 403-264-5898 Web: www.cspg.org To Stamp or Not to Stamp? A Perennial Question .......................................................... -
Wildlife Corridors in the Lake Louise Area, Alberta
Wildlife Corridors in the Lake Louise Area, Alberta: A Multi-Scale, Multi-Species Management Strategy Final Report Prepared for: Alan Dibb, Wildlife Specialist Kootenay, Yoho, Lake Louise District Parks Canada Box 220 Radium Hot Springs, BC V0A 1M0 Prepared by: Marie Tremblay 5704 Lakeview Drive S.W. Calgary, AB T3E 5S4 August 2001 PREFACE This report was prepared under the terms of Parks Canada contract #KKP 2064. The views expressed are those of the author and do not necessarily reflect the policies of Parks Canada. This document may be cited as: Tremblay, M. 2001. Wildlife Corridors in the Lake Louise Area, Alberta: A Multi-Scale, Multi-Species Management Strategy. Prepared for Parks Canada. 168pp. i EXECUTIVE SUMMARY BACKGROUND Habitat fragmentation is a central issue in the Lake Louise area due to the presence of a naturally fragmented landscape coupled with high levels of human activity, a situation that is believed to be constraining the movements of wildlife in the area. Human influences in the Lake Louise area include four nodes of visitor activity (the Hamlet of Lake Louise, the Upper Lake area, the Lake Louise ski area, and the Moraine Lake area), two major transportation corridors (the Trans-Canada Highway and the Canadian Pacific Railway), several high volume secondary roads, a dense network of popular hiking trails, and dispersed human activity such as off-trail hiking and snowshoeing. Although a variety of studies have been carried out to further our understanding of wildlife habitat use and movements within BNP, there has been no attempt to synthesize information from multiple sources into a single consideration of wildlife corridors specifically for the Lake Louise area. -
Skoki Valley Grand Tour Slate Range Canadian Rockies, Banff National Park Alberta and British Columbia, Canada
skoki valley graNd tour slate range Canadian rockies, banff National Park Alberta and British Columbia, Canada DistAnce: 28 miles (43 km) round-trip tiMe: 3–4 days PhysicAl chAllenge: 1 2 3 4 5 PsychologicAl chAllenge: 1 2 3 4 5 stAging: lake louise, Alberta our t d N ra g ucked away behind the sprawling Lake Louise alley ski area, in the heart of Alberta’s Canadian v Rockies, lies the impressive Slate Range. This remote collection of 10,000-foot (3,050-m) peaks koki t harbors some of the best hiking in a part of the world S renowned for great hiking. Just beyond Deception E Pass and majestic Redoubt Mountain lies the pretty a Skoki Valley, a worthy destination in itself but also C the gateway to greater backcountry adventure farther afield. There may be no better way to sample the meri renowned beauty of Banff National Park than to trek a through this landscape. Just getting to Skoki Valley calls for a world-class hiking day. From the end of the Temple Lodge access road, behind the popular ski area, the route works up through the trees into a sprawling open meadow, and ikes of North h from there up to Boulder Pass and the first views of the C impressive peaks of the Slate Range beyond. From From the pass, the route offers spectacular views of the here, Mount Richardson, Pika Peak, and Ptarmigan peaks beyond before dropping into the Skoki Valley. Classi Peak form the impossibly dramatic climax of the Slate The last few miles come with tantalizing glimpses of Range. -
Hydrogeologic and Hydrochemical Framework of Indian Wells Valley, California: Evidence for Interbasin Flow in the Southern Sierra Nevada
HYDROGEOLOGIC AND HYDROCHEMICAL FRAMEWORK OF INDIAN WELLS VALLEY, CALIFORNIA: EVIDENCE FOR INTERBASIN FLOW IN THE SOUTHERN SIERRA NEVADA by David V. Williams ABSTRACT The Indian Wells Valley is a desert basin of southeastern California located in the transition zone of the Sierra Nevada, Great Basin, and Mojave Desert. Previous conceptual models of the groundwater system suggest that the surrounding granitic rocks are unable to transmit or store significant amounts of water and have described Indian Wells Valley as a closed hydrologic basin with limited recharge and discharge. In contrast, a comprehensive analysis of hydrologic, hydrochemical, isotopic, and structural data of the Indian Wells Valley performed in this thesis indicate a more complex model. The revised paradigm of Indian Wells Valley is one of an open basin, wherein much of the groundwater recharge is derived from outside the topographic divide by way of a unique combination of interconnected faults and fractures serving as conduits for interbasin flow. Hydrogeologic analysis suggests the aquifer flux in one portion of the valley is more than five times precipitation-based estimates using the Maxey-Eakin method. This high volumetric flux is due to a steep hydraulic gradient, which was dismissed in previous studies as an alluvial fault acting as a flow barrier. However, this study found no geophysical or hydrologic evidence to support the presence of a flow barrier, corroborating the high calculated flux. Groundwater chemistry indicates seven major hydrochemcial facies distributed within the valley and the surrounding areas. For the most part, water types are consistent with chemical evolution common to this portion of the Great Basin, but data indicate a large volume of groundwater within the basin that is not derived from within the confines of the topographic watershed. -
The Mountain Geologist Bibliography 1964
Cumulative Bibliography and Index to The Mountain Geologist, 1964 through 2009 By Michele G. Bishop The Mountain Geologist was first published in 1964 by the Rocky Mountain Association of Geologists. This Cumulative Bibliography and Index records the entire publication history from 1964 through 2009. This Bibliography will be updated every year. Hardcopies of some issues of The Mountain Geologist are available for sale from the RMAG website <www.rmag.org/publications/index.asp>. Digital copies of The Mountain Geologist issues from 1964 through 2005 are available for sale at the RMAG office (www.rmag.org). The October 1985 Volume 22 Number 4 issue of The Mountain Geologist is available for download from <www.rmag.org/publications/index.asp>. The RMAG will issue digital collections of The Mountain Geologist every 5 years. Contents Part I Author Index ……………………………………………………page 2 Part II Geographical Index……….…………..……………………….page 65 Part III Topical Index……………………………….…………………page 79 The first cumulative bibliography for The Mountain Geologist was prepared by John W. Oty and published in the January 1975 issue. It covered Volumes 1 to 11 (1964-1974) and was largely geographic in its categorization of papers. In 1992 Stephen D. Schwochow published a cumulative bibliography and index of The Mountain Geologist for the years 1975 through 1991 (see The Mountain Geologist, v. 29, no. 4, pages 101- 130). He then published yearly indices from 1992 through 1995 in The Mountain Geologist. In 1999, Mary P. (Penny) Frush assembled and published these indices and added the additional years with guidance from the format that Stephen Schwochow outlined (see The Mountain Geologist, v. -
Economic Impact Study
ECONOMIC IMPACT STUDY EVENT 2011 LAKE LOUISE WINTERSTART WORLD CUP NOVEMBER 26‐27 & DECEMBER 1‐4, 2011 THE SPORT ALPINE SKIING THE LOCATION LAKE LOUISE, ALBERTA THE VENUE LAKE LOUISE SKI RESORT Credit: Roger Witney/Alpine Canada Alpin THE HOST ORGANIZATION WINTERSTART Survey and Data Management Consultant Discovery Research Ltd. Software S.I.M.A. (Sport Impact Model – Alberta) Developed by: Econometric Research Limited Release Date: June 6, 2013 TABLE OF CONTENTS PAGES SECTION A: GENERAL OVERVIEW OF ECONOMIC IMPACT ANALYSIS 1‐2 1. Introduction to Economic Impact Analysis 1 2. Sport Impact Model for Alberta (S.I.M.A.) 1 3. Methodology 2 4. General Assumptions 2 SECTION B: EVENT OVERVIEW & ECONOMIC IMPACT REPORT 3‐6 1. Background 3 2. Venue Overview 3 3. Event Overview 3‐5 a. Event Dates 3 b. Participating Countries 3 c. Media Exposure 4 d. Attendance 4 i. Media & VIP 4 ii. Volunteers & Officials 4 iii. Spectators 4 iv. Team Visitors 4 v. Attendance by “Type” 4 vi. Attendance by “Origin” 4 e. Event Operational Revenue Summary 5 h. Event Operational Expense Summary 5 4. EVENT ECONOMIC IMPACTS 6‐7 a. Economic Impacts Province‐Wide 6 b. Economic Impacts to local Region ONLY 6 c. Graph #1: EXPENDITURES AND VALUE‐ADDED ECONOMIC IMPACTS 7 d. Graph #2: TOTAL VISITOR EXPENDITURES BY PERCENTAGE AND BY ORIGIN OF VISITOR 7 e. Graph #3: VISITOR EXPENDITURES BY PERCENTAGE OF TYPE (AND AMOUNT SAMPLES) 7 f. Graph #4: TAX IMPACTS BY REGIONAL‐ONLY AND PROVINCE‐WIDE 8 g. Graph #5: TAX IMPACTS, PROVINCE‐WIDE, BY 8 RECEIVING BY RECEIVING LEVEL OF GOVERNMENT APPENDIX A: GLOSSARY 9 SECTION A: GENERAL OVERVIEW OF ECONOMIC IMPACT ANALYSIS 1. -
Annotated Wildlife Reference for Banff and Jasper National Parks
QL 221 .A4 M33 1985 c.3 ANNOTATED WILDLIFE REFERENCES FOR BANFF AND JASPER NATIONAL PARKS by Keith A. McDougall Joe R. McGillis Geoffrey L. Holroyd fF 0 P LIB BOX 90()~ BANFF, AS T1L 1K2 PH .. (403) 162 .. 1500 Prepared for: PARKS CANADA by Canadian Wildlife Service Edmonton MARCH 1985 ABSTRACT This compilation lists 315 annotated references to reports on the wildlife of Banff and Jasper National Parks. The references are listed by author alphabetically and the citation includes an annotation and list of keywords. The index identifies the reports that have each keyword. We recommend a more complete document be prepared when manpower and funding permit. i TABLE OF CONTENTS Page ABSTRACT i INTRODUCTION 1 FORMAT OF THE REPORT 1 ANNOTATED BIBLIOGRAPHY 3 INDEX 86 ii INTRODUCTION During the course of the ecological (biophysical) wildlife inventories of these two national parks, many references to wildlife reports were reviewed in various libraries and archives. Some references were used in the final report of the inventory, (Holroyd, G.L. and K. J. Van Tighem. 1983. Ecological [Biophysical] Land Classification of Banff and Jasper National Parks. Volume III: The Wildlife Inventory produced for Parks Canada by Canadian Wildlife Service, Edmonton. 691 pp.), and some were not. The references presented here, therefore, duplicate some from the Volume III report and include all those references that were reviewed and annotated but not used in the report. However, there are other references in the report which are not presented here. We recommend that these references be annotated and combined with this report to form a complete wildlife bibliography which can be compiled and distributed both electronically in an existing library catalogue and on paper. -
[Italic Page Numbers Indicate Major References] Abajo Mountains, 314
Index [Italic page numbers indicate major references] Abajo Mountains, 314 andesite, 70, 82, 86, 267, 295, 297, terranes, 36, 644 Abert Lake-Goose Lake area, 343 299, 303, 305, 308, 310, 343, volcanic. See volcanic arcs Abert Rim area, 303, 377 345, 350, 371, 375, 483, 527, volcanism, 74, 81, 89, 299, 300, Absaroka Range, 290, 354 543, 644, 654 320, 385, 482, 491, 642 Absaroka system, 592 Aneth Formation, 45 waning, 643 Absaroka thrust, 172, 219, 594, 599, Angora Peak member, 316 See also specific arcs 601 Angustidontus, 34 Archean, 629, 632, 651, 652 Absaroka volcanic field, 218, 297, Anita Formation, 275 arches, 15, 46 300, 486, 491 anorthosite, 412, 633 archipelago, volcanic, 453 accretion, 36, 111, 127, 128, 131, Antelope Mountain Quartzite, 38, 40, arenite, 142 141, 168, 242, 252, 254, 262, 420 argillite, 11, 16, 31, 34, 38, 41, 62, 265, 273, 450, 468, 534, 545, Antelope Range Formation, 28 70, 81, 85, 87, 89, 111, 128, 555, 636, 646, 664, 677, 693 Antelope Valley Limestone, 22, 23, 24 130, 133, 136, 138, 141, 160, accretionary prism, 37, 127, 141, 241, anticlines, 213, 319, 340 162, 164, 281, 434, 543, 547, 281, 422, 423, 432, 436, 468, antimony, 643, 644 635, 658, 663, 671, 676 471, 621, 654, 676 Antler allochthon, 422, 431 Argus Range, 365, 600 actinolite, 528, 637 Antler assemblage, 419, 422, 450 Arikaree Formation, 286 Adams Mine, 632 Antler foredeep basin, 35, 61, 62, 74, Arizona, 140, 597 Adaville Formation, 219 94, 96, 420, 425, 430, 471 south-central, 323 Adel Mountain volcanic field, 218, Antler foreland basin, 28, 42, -
Cumulative Bibliography and Index: the Mountain Geologist 1964-2010
Cumulative Bibliography and Index to The Mountain Geologist, 1964 through 2010 By Michele G. Bishop The Mountain Geologist was first published in 1964 by the Rocky Mountain Association of Geologists. This Cumulative Bibliography and Index records the entire publication history from 1964 through 2010. Contents Part I Author Index ……………………………………………………page 2 Part II Geographical Index……….…………..……………………….page 66 Part III Topical Index……………………………….…………………page 80 The first cumulative bibliography for The Mountain Geologist was prepared by John W. Oty and published in the January 1975 issue. It covered Volumes 1 to 11 (1964-1974) and was largely geographic in its categorization of papers. In 1992 Stephen D. Schwochow published a cumulative bibliography and index of The Mountain Geologist for the years 1975 through 1991 (see The Mountain Geologist, v. 29, no. 4, pages 101-130). He then published yearly indices from 1992 through 1995 in The Mountain Geologist. In 1999, Mary P. (Penny) Frush assembled and published these indices and added the additional years with guidance from the format that Stephen Schwochow outlined (see The Mountain Geologist, v. 36, no. 1, p. 1-56). The Cumulative Bibliography and Index was brought up to date in 2001, again in 2010 and now in 2011, by Michele G. Bishop. Many additional people have given guidance or proofed various updates and their time and ideas are very much appreciated. The 2010 update version was reviewed by Ira Pasternack, Mark Longman, Joy Rosen-Mioduchowski, Jeanette Dubois, and Kristine Peterson. Hardcopies of some issues of The Mountain Geologist are available for sale from the RMAG website <www.rmag.org/publications/index.asp>.