Structure and Petrology of Specimen Mountain, Colorado

Total Page:16

File Type:pdf, Size:1020Kb

Structure and Petrology of Specimen Mountain, Colorado BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 55, PP. 77-90, 2 PLS., 7 FIGS. JANUARY 1, 1944 STRUCTURE AND PETROLOGY OF SPECIMEN MOUNTAIN, COLORADO BY ERNEST E. WAHLSTROM CONTENTS Page Abstract........................................................................................................................................................................ 77 Introduction............................................................................................................................................................... 78 General statement............................................................................................................................................ 78 Location.............................................................................................................................................................. 78 Topography and physiography.................................................................................................................... 79 Methods of mapping....................................................................................................................................... 79 Acknowledgments............................................................................................................................................. 79 General geology......................................................................................................................................................... 79 Structure...................................................................................................................................................................... 80 Faulting and folding........................................................................................................................................ 80 Structural history............................................................................................................................................. 80 Regional relationships.............................................................................................................................................. 82 Petrography................................................................................................................................................................ 84 General statement............................................................................................................................................ 84 Basal flows.......................................................................................................................................................... 84 Pyroclastics........................................................................................................................................................ 86 Upper flows........................................................................................................................................................ 86 Plug rocks........................................................................................................................................................... 87 Differentiation........................................................................................................................................................... 88 Pneumatolytic and hydrothermal activity........................................................................................................ 89 Age................................................................................................................................................................................ 89 References cited........................................................................................................................................................ 89 ILLUSTRATIONS Figure Page 1. Outline map of north-central Colorado................................................................................................... 78 2. Geologic map of Specimen Mountain area............................................................................................. 81 3. Geologic cross sections of Specimen Mountain..................................................................................... 82 4. Idealized cross sections................................................................................................................................. 83 5. Geologic map showing relationship of flow at Iceberg Lake to Specimen Mountain................ 84 6. Larsen plots of Specimen Mountain rocks............................................................................................. 88 7. Triangular diagram....................................................................................................................................... 88 Plate Facing page 1. West side of Specimen Mountain......................................................................................................... 80 2. Volcanic rocks at Specimen Mountain................................................................................................ 81 ABSTRACT Specimen Mountain, an eroded Cenozoic volcano in the northwestern corner of Rocky Mountain National Park, Colorado, is flanked on the south and west by an extensive series of faulted and folded lava flows and pyroclastics. Regional studies indicate that the erupted materials spread 77 Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/55/1/77/3431269/BUL55_1-0077.pdf by guest on 29 September 2021 78 WAHLSTROM— SPECIMEN MOUNTAIN, COLORADO laterally for several miles in all directions from a single central conduit and buried a prevolcanic . surface of considerable relief. The volcanic rocks, as shown by analyses, are quartz latite and silicic rhyolite. Quartz latite flows are chilled samples of a magma which by gravitative differentiation gave rise to silicic rhyolite occurring as flows and plug rocks. Thick beds of ash, agglomerate, and breccia attest to inter­ mittent explosions of great magnitude. Inconclusive evidence suggests a Miocene or Pliocene age for the volcanics. F ig u r e 1. Outline map of north-central Colorado Showing location of Specimen Mountain area. INTRODUCTION GENERAL STATEMENT The study of Specimen Mountain was undertaken in collaboration with the National Park Service in an effort to unravel the geological history of this prominent and often-visited landmark. The project is one of several leading ultimately to the reconstruction of the geologic and physiographic history of the whole of Rocky Mountain National Park. This paper summarizes results of geologic and petrologic investigations begun in the summer of 1941 and continued intermittently through the winter of 1942-1943. LOCATION Specimen Mountain straddles the Continental Divide at the crest of the Front Range of Colorado (Fig. 1). Its western slopes drain into the headwaters of the Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/55/1/77/3431269/BUL55_1-0077.pdf by guest on 29 September 2021 INTRODUCTION 79 Colorado River in the northwestern corner of Rocky Mountain National Park. The Cache la Poudre River, a tributary of the South Platte River, drains the southern and eastern slopes. The mountain is easily reached by the Trail Ridge Road from either Grand Lake or Estes Park. A trail starting at Poudre Lake leads to the top of Specimen Mountain. TOPOGRAPHY AND PHYSIOGRAPHY The elevation of the summit of Specimen Mountain is 12,482 feet. Slopes on the northwest and south sides of the mountain drop steeply to the floors of canyons 2500 to 3000 feet below the summit. The area surrounding Specimen Mountain is exceedingly rugged and displays all the depositional and erosional features of intense alpine glaciation. Specimen Mountain itself is glaciated and is deeply embayed on its northern and western slopes by cliff-walled cirques, which are rapidly filling be­ cause of landsliding in the rapidly disintegrating volcanic rocks. Evidences of frost action and solifluxion are abundant on the upper exposed slopes. Polygonal rock patterns and rock streams are locally conspicuous. In the pre-Cambrian rocks near Specimen Mountain much of the surface has a “grain” which reflects the gneissoid structure of the underlying rocks. Lenticular masses of pegmatite and granite strike northeast and, in general, stand out in ridges formed by more rapid erosion of adjacent layers of schist and gneiss. METHODS OF MAPPING Geologic mapping was done on aerial photographs. A composite geologic map was made from the various photographs, and errors due to tilting and perspective were ad­ justed by use of a triangulation net surveyed with a plane table and alidade. The geologic map was then superimposed on a photographic enlargement of a portion of the United States Geological Survey’s topographic map of the Rocky Mountain National Park Quadrangle. Because of the inaccuracy of the enlarged topographic map only the 500-foot contours are shown in the finished maps. ACKNOWLEDGMENTS The writer wishes to express his appreciation of the assistance given in the field by Mr. Olwin Woodbury. The work was considerably expedited by the helpful co­ operation of several officials of Rocky Mountain National Park. The writer is es­ pecially indebted to Mr. David H. Canfield, Park Superintendent, Mr. Raymond Gregg, Park Naturalist, and Dr. Carroll H. Wegemann, Regional Geologist, for many courtesies. H. E. Rothrock, Assistant Chief of the Naturalist Division of
Recommended publications
  • Thesis Rapid Ascent: Rocky Mountain National Park In
    THESIS RAPID ASCENT: ROCKY MOUNTAIN NATIONAL PARK IN THE GREAT ACCELERATION, 1945-PRESENT Submitted by Mark Boxell Department of History In partial fulfillment of the requirements For the Degree of Master of Arts Colorado State University Fort Collins, Colorado Summer 2016 Master’s Committee: Advisor: Mark Fiege Ben Bobowski Adrian Howkins John Lindenbaum Jared Orsi Copyright by Mark Boxell 2016 All Rights Reserved ABSTRACT RAPID ASCENT: ROCKY MOUNTAIN NATIONAL PARK IN THE GREAT ACCELERATION, 1945-PRESENT After the Second World War’s conclusion, Rocky Mountain National Park (RMNP) experienced a massive rise in visitation. Mobilized by an affluent economy and a growing, auto- centric infrastructure, Americans rushed to RMNP in droves, setting off new concerns over the need for infrastructure improvements in the park. National parks across the country experienced similar explosions in visitation, inspiring utilities- and road-building campaigns throughout the park units administered by the National Park Service. The quasi-urbanization of parks like RMNP implicated the United States’ public lands in a process of global change, whereby wartime technologies, cheap fossil fuels, and a culture of techno-optimism—epitomized by the Mission 66 development program—helped foster a “Great Acceleration” of human alterations of Earth’s natural systems. This transformation culminated in worldwide turns toward mass-urbanization, industrial agriculture, and globalized markets. The Great Acceleration, part of the Anthropocene— a new geologic epoch we have likely entered, which proposes that humans have become a force of geologic change—is used as a conceptual tool for understanding the connections between local and global changes which shaped the park after World War II.
    [Show full text]
  • Rocky Mountain National Park Lawn Lake Flood Interpretive Area (Elevation 8,640 Ft)
    1 NCSS Conference 2001 Field Tour -- Colorado Rocky Mountains Wednesday, June 27, 2001 7:00 AM Depart Ft. Collins Marriott 8:30 Arrive Rocky Mountain National Park Lawn Lake Flood Interpretive Area (elevation 8,640 ft) 8:45 "Soil Survey of Rocky Mountain National Park" - Lee Neve, Soil Survey Project Leader, Natural Resources Conservation Service 9:00 "Correlation and Classification of the Soils" - Thomas Hahn, Soil Data Quality Specialist, MLRA Office 6, Natural Resources Conservation Service 9:15-9:30 "Interpretive Story of the Lawn Lake Flood" - Rocky Mountain National Park Interpretive Staff, National Park Service 10:00 Depart 10:45 Arrive Alpine Visitors Center (elevation 11,796 ft) 11:00 "Research Needs in the National Parks" - Pete Biggam, Soil Scientist, National Park Service 11:05 "Pedology and Biogeochemistry Research in Rocky Mountain National Park" - Dr. Eugene Kelly, Colorado State University 11:25 - 11:40 "Soil Features and Geologic Processes in the Alpine Tundra"- Mike Petersen and Tim Wheeler, Soil Scientists, Natural Resources Conservation Service Box Lunch 12:30 PM Depart 1:00 Arrive Many Parks Curve Interpretive Area (elevation 9,620 ft.) View of Valleys and Glacial Moraines, Photo Opportunity 1:30 Depart 3:00 Arrive Bobcat Gulch Fire Area, Arapaho-Roosevelt National Forest 3:10 "Fire History and Burned Area Emergency Rehabilitation Efforts" - Carl Chambers, U. S. Forest Service 3:40 "Involvement and Interaction With the Private Sector"- Todd Boldt; District Conservationist, Natural Resources Conservation Service 4:10 "Current Research on the Fire" - Colorado State University 4:45 Depart 6:00 Arrive Ft. Collins Marriott 2 3 Navigator’s Narrative Tim Wheeler Between the Fall River Visitors Center and the Lawn Lake Alluvial Debris Fan: This Park, or open grassy area, is called Horseshoe Park and is the tail end of the Park’s largest valley glacier.
    [Show full text]
  • A Guide to the Geology of Rocky Mountain National Park, Colorado
    A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK COLORADO For sale by the Superintendent of Documents, Washington, D. C. Price 15 cents A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK [ COLORADO ] By Carroll H. Wegemann Former Regional Geologist, National Park Service UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE . NEWTON B. DRURY, Director UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1944 Table of Contents PAGE INTRODUCTION in BASIC FACTS ON GEOLOGY 1 THE OLDEST ROCKS OF THE PARK 2 THE FIRST MOUNTAINS 3 The Destruction of the First Mountains 3 NATURE OF PALEOZOIC DEPOSITS INDICATES PRESENCE OF SECOND MOUNTAINS 4 THE ROCKY MOUNTAINS 4 Time and Form of the Mountain Folding 5 Erosion Followed by Regional Uplift 5 Evidences of Intermittent Uplift 8 THE GREAT ICE AGE 10 Continental Glaciers 11 Valley Glaciers 11 POINTS OF INTEREST ALONG PARK ROADS 15 ROAD LOGS 18 Thompson River Entrance to Deer Ridge Junction 18 Deer Ridge Junction to Fall River Pass via Fall River .... 20 Fall River Pass to Poudre Lakes 23 Trail Ridge Road between Fall River Pass and Deer Ridge Junction 24 Deer Ridge Junction to Fall River Entrance via Horseshoe Park 29 Bear Lake Road 29 ILLUSTRATIONS LONGS PEAK FROM BEAR LAKE Front and back covers CHASM FALLS Inside back cover FIGURE PAGE 1. GEOLOGIC TIME SCALE iv 2. LONGS PEAK FROM THE EAST 3 3. PROFILE SECTION ACROSS THE ROCKY MOUNTAINS 5 4. ANCIENT EROSIONAL PLAIN ON TRAIL RIDGE 6 5. ANCIENT EROSIONAL PLAIN FROM FLATTOP MOUNTAIN ... 7 6. VIEW NORTHWEST FROM LONGS PEAK 8 7.
    [Show full text]
  • Summits on the Air – ARM for USA - Colorado (WØC)
    Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections.
    [Show full text]
  • Rocky Mountain National Park Geologic Resource Evaluation Report
    National Park Service U.S. Department of the Interior Geologic Resources Division Denver, Colorado Rocky Mountain National Park Geologic Resource Evaluation Report Rocky Mountain National Park Geologic Resource Evaluation Geologic Resources Division Denver, Colorado U.S. Department of the Interior Washington, DC Table of Contents Executive Summary ...................................................................................................... 1 Dedication and Acknowledgements............................................................................ 2 Introduction ................................................................................................................... 3 Purpose of the Geologic Resource Evaluation Program ............................................................................................3 Geologic Setting .........................................................................................................................................................3 Geologic Issues............................................................................................................. 5 Alpine Environments...................................................................................................................................................5 Flooding......................................................................................................................................................................5 Hydrogeology .............................................................................................................................................................6
    [Show full text]
  • Contributions to the Geography of the United States, 1922
    CONTRIBUTIONS TO THE GEOGRAPHY OF THE UNITED STATES, 1922. PENEPLAINS OF4 THE FRONT RANGE AND ROCKY MOUNTAIN NATIONAL PARK, COLORADO. By Wnxis T. LEE. PURPOSE OF THE PAPER. The purpose of this paper is to call attention to some of the major surface features in the Rocky Mountain National Park and to point out their probable correlation with similar features in neigh­ boring regions. The observations on which the paper is based were made in the summer of 1916, during an investigation in which other work demanded first consideration. This paper may therefore be considered a by-product. For the same reason many of the observa­ tions were not followed to conclusions, yet the data obtained seem to be sufficient to establish a certain order of events, the recognition of which may be of assistance in working out in detail the geologic and geographic history of the Rocky Mountain region. TWO CYCLES OF EROSION PREVIOUSLY RECOGNIZED. In an account of the general geology of the Georgetown quad­ rangle, Colo.j Ball x describes three distinct types of land forms " an old, mature mountainous upland; younger V-shaped valleys in­ cised in this upland; and glacial cirques developed at the heads of some of the streams, passing downward into U-shaped valleys." Ball describes the mountainous upland as consisting of highlands of rounded or gently sloping tops which are remnants of an ancient peneplain or old surface of erosion. Most of these remnants in the Georgetown quadrangle lie above an altitude of 11,500 feet. On thig old peneplain there were many monadnocks, some of which are now recognizable as the summits of the highest mountains.
    [Show full text]
  • Rocky Mountain National Park Geologic Resources Evaluation
    National Park Service U.S. Department of the Interior Natural Resource Program Center Rocky Mountain National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2004/004 THIS PAGE: Ypsilon Mountain, Rocky Mountain NP. ON THE COVER: Alpine Tundra looking west to the Never Summer Range, Rocky Mountain NP Photos by: NPS and Josh Heise Rocky Mountain National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2004/004 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2004 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters.
    [Show full text]
  • Report 2008–1360
    The Search for Braddock’s Caldera—Guidebook for Colorado Scientific Society Fall 2008 Field Trip, Never Summer Mountains, Colorado By James C. Cole,1 Ed Larson,2 Lang Farmer,2 and Karl S. Kellogg1 1U.S. Geological Survey 2University of Colorado at Boulder (Geology Department) Open-File Report 2008–1360 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D.Myers, Director U.S. Geological Survey, Reston, Virginia 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Cole, James C., Larson, Ed, Farmer, Lang, and Kellogg, Karl S., 2008, The search for Braddock’s caldera—Guidebook for the Colorado Scientific Society Fall 2008 field trip, Never Summer Mountains, Colorado: U.S. Geological Survey Open-File Report 2008–1360, 30 p. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. 2 Abstract The report contains the illustrated guidebook that was used for the fall field trip of the Colorado Scientific Society on September 6–7, 2008. It summarizes new information about the Tertiary geologic history of the northern Front Range and the Never Summer Mountains, particularly the late Oligocene volcanic and intrusive rocks designated the Braddock Peak complex.
    [Show full text]
  • Viewshed of Analysis of Native American Sacred Landscapes
    Viewshed Analysis of Native American Sacred Landscapes Dr. David M. Diggs, Dr. Robert Brunswig, and Sara Jo Lambert Departments of Geography and Anthropology University of Northern Colorado, Greeley, CO Abstract. Rocky Mountain National Park (RMNP), USA, is rich in Native American sites, many believed to have served religious purposes. Field and consultation data have been incorporated into successive generations of a Geographic Information System (GIS) project designed to model and predict the spatial distribution of sacred sites and ritual features believed to have constituted long-lost landscapes. In recent iterations of the RMNP sacred landscape modeling research, a Weights-of-Evidence site location predictive model was developed. This model showed the strong influence of the relative visibility of five sacred landmarks. This paper uses multi-feature and multi-landmark viewshed analysis techniques to evaluate the relative and absolute visibility of the above mentioned five landmarks. Landmarks are assessed both individually, in total, and in strength of visibility. The research suggests that both strength of visibility and total number of landmarks visible are strongly associated with the location of sacred features. Introduction Since 1998 the University of Northern Colorado (UNC) has conducted archaeological surveys and research in Rocky Mountain National Park. Early results of these interrelated projects suggested that many of these sites had been associated with past ritual/ceremonial activities (Brunswig 2003). This was supported by earlier research that had identified areas within and just outside the park boundaries that were known or thought to be sacred landmarks to Arapahoe, Ute, and other Native American groups (see for example discussions in Benedict 1985; McBeth 2007; Toll 2003).
    [Show full text]
  • The Geologic Story of the Rocky Mountain National Park, Colorado
    782 R59 L48 flforttell Uniucraitg ffitbrarg THE GIFT OF UL.5. SoLpt. o|: Doca-manis, ^^JflAgJJ^-J^HV W&-J 1079F hiiUBfeillW^naf Cornell University Library F 782R59 L48 3 1924 028 879 082 olin Cornell University Library The original of this bool< is in the Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924028879082 DEPARTMENT OF THE INTERIOR FRANKLIN K. lANE, Secretary NATIONAL PARK SERVICE STEPHEN T. MATHER, Director THE GEOLOGIC STORY OF THE ROCKY MOUNTAIN NATIONAL PARK COLORADO BY WILLIS T. LEE, Ph. D. Geologist, United States Geological SuiTey WASHINGTON GOVERNMENT PRINTING OFFICE 1917 n ^HnH- CONTENTS. Page. Introduction 7 Location and character 7 A brief historical sketch ^ 9 In the days of the aborigines 11 Accessibility 11 A general outlook 12 The making and shaping of the mountains 14 Geology and scenery 14 Before the Rockies were bom 15 The birth of the Rockies 19 How the mountains grew 21 How the mountains were shaped 22 Work of rain 23 Work of frost 24 Work of streams 25 Methods of work 25 Streams of park exceptional 27 Stripping of the mountains 27 An old plain of erosion'. 28 Many periods of uplift 28 Work of ice 29 . When and why glaciers form. •. 29 ' Living glaciers • 29 Ancient glaciers 31 Fall River Glacier 32 Thompson Glacier 32 Bartholf Glacier 33 Mills Glacier 33 Wild Basin Glacier 34 Glaciers of North Fork and its tributaries 84 Glaciers in the northern part of the park 37 How the glaciers worked 37 Approaches to the park 38 Loveland to Estes Park 38 Lyons to Estes Park - 41 Ward to Estes Park 42 Grand Lake route 43 The park as seen from the trails 45 Black Canyon trail 45 Lawn Lake 47 Hagues Peak and Hallett Glacier 47 Roaring River 49 Horseshoe Falls 50 Fall River road 50 Trail ridge 54 3 4 CONTENTS.
    [Show full text]
  • An Environmental History of the Kawuneeche Valley and the Headwaters of the Colorado River, Rocky Mountain National Park
    An Environmental History of the Kawuneeche Valley and the Headwaters of the Colorado River, Rocky Mountain National Park Thomas G. Andrews Associate Professor of History University of Colorado at Boulder October 3, 2011 Task Agreeement: ROMO-09017 RM-CESU Cooperative Agreement Number: H12000040001 Table of Contents Acknowledgements i Abbreviations Used in the Notes iv Introduction 1 Chapter One: 20 Native Peoples and the Kawuneeche Environment Chapter Two: 91 Mining and the Kawuneeche Environment Chapter Three: 150 Settling and Conserving the Kawuneeche, 1880s-1930s Chapter Four: 252 Consolidating the Kawuneeche Chapter Five: 367 Beaver, Elk, Moose, and Willow Conclusion 435 Bibliography 441 Appendix 1: On “Numic Spread” 477 Appendix 2: Homesteading Data 483 Transcript of Interview with David Cooper 486 Transcript of Interview with Chris Kennedy 505 Transcript of Interview with Jason Sibold 519 i Acknowledgements This report has benefited from the help of many, many people and institutions. My first word of thanks goes to my two research assistants, Daniel Knowles and Brandon Luedtke. Both Dan and Brandon proved indefatigable, poring through archival materials, clippings files, government reports, and other sources. I very much appreciate their resourcefulness, skill, and generosity. I literally could not have completed this report without their hard work. Mark Fiege of Colorado State University roped me into taking on this project, and he has remained a fount of energy, information, and enthusiasm throughout. Maren Bzdek of the Center for Public Lands History handled various administrative details efficiently and with good humor. At the National Park Service, Cheri Yost got me started and never failed to respond to my requests for help.
    [Show full text]
  • Rocky Mountain National Park Multiple Resource Area
    NPS Form 10-900-b OMB No. 1024-0018 (Revised March 1992) United States Department of the Interior National Park Service National Register of Historic Places Multiple Property Documentation Form This form is used for documenting multiple property groups relating to one or several historic contexts. See instructions in How to Complete the Multiple Property Documentation Form (National Register Bulletin 16B). Complete each item by entering the requested information. For additional space, use continuation sheets (Form 10-900-a). Use a typewriter, word processor, or computer, to complete all items. New Submission XXX Amended Submission A. Name of Multiple Property Listing Rocky Mountain National Park MPS (Additional documentation- Trails) B. Associated Historic Contexts (Name each associated historic context, identifying theme, geographical area, and chronological period for each.) I. Pioneer Settlement and Development of the Resort Industry, applied to Trails 1900-1945 IV. Transportation, Prehistoric and Historic Trails 6,000/7,000 years ago – 1920s V. NPS Naturalistic Design, Construction of Trails 1920-1945 C. Form Prepared by name/title Sierra Standish/ contract position (RMNP contacts- Dr. Bill Butler and Cheri Yost) organization Rocky Mountain National Park date September 27, 2004 street & number 1000 U.S. Highway 36 telephone (970) 586-1332 city or town Estes Park state Colorado zip code 80517 D. Certification As the designated authority under the National Historic Preservation Act of 1966, I hereby certify that this documentation form meets the National Register documentation standards and sets forth requirements for listing of related properties consistent with the National Register criteria. This submission meets the procedural and professional requirements set forth in 36 CFR Part 60 and the Secretary of the Interior's Standards and Guidelines for Archaeology and Historic Preservation.
    [Show full text]