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To See the Hike Archive
Geographical Area Destination Trailhead Difficulty Distance El. Gain Dest'n Elev. Comments Allenspark 932 Trail Near Allenspark A 4 800 8580 Allenspark Miller Rock Riverside Dr/Hwy 7 TH A 6 700 8656 Allenspark Taylor and Big John Taylor Rd B 7 2300 9100 Peaks Allenspark House Rock Cabin Creek Rd A 6.6 1550 9613 Allenspark Meadow Mtn St Vrain Mtn TH C 7.4 3142 11632 Allenspark St Vrain Mtn St Vrain Mtn TH C 9.6 3672 12162 Big Thompson Canyon Sullivan Gulch Trail W of Waltonia Rd on Hwy A 2 941 8950 34 Big Thompson Canyon 34 Stone Mountain Round Mtn. TH B 8 2100 7900 Big Thompson Canyon 34 Mt Olympus Hwy 34 B 1.4 1438 8808 Big Thompson Canyon 34 Round (Sheep) Round Mtn. TH B 9 3106 8400 Mountain Big Thompson Canyon Hwy 34 Foothills Nature Trail Round Mtn TH EZ 2 413 6240 to CCC Shelter Bobcat Ridge Mahoney Park/Ginny Bobcat Ridge TH B 10 1500 7083 and DR trails Bobcat Ridge Bobcat Ridge High Bobcat Ridge TH B 9 2000 7000 Point Bobcat Ridge Ginny Trail to Valley Bobcat Ridge TH B 9 1604 7087 Loop Bobcat Ridge Ginny Trail via Bobcat Ridge TH B 9 1528 7090 Powerline Tr Boulder Chautauqua Park Royal Arch Chautauqua Trailhead by B 3.4 1358 7033 Rgr. Stn. Boulder County Open Space Mesa Trail NCAR Parking Area B 7 1600 6465 Boulder County Open Space Gregory Canyon Loop Gregory Canyon Rd TH B 3.4 1368 7327 Trail Boulder Open Space Heart Lake CR 149 to East Portal TH B 9 2000 9491 Boulder Open Space South Boulder Peak Boulder S. -
Appendix C Table 1, Camp Area Summary
Backcountry/Wilderness Management Plan and Environmental Assessment Appendix C Appendix C Table 1, Camp Area Summary Designated Areas/Sites Individual Camp Areas Campsites People East Side 60 109 763 West Side 59 88 616 Total 119 197 1379 Group Camp Areas Campsites People East Side 10 10 120 West Side 11 11 132 Total 21 21 252 Accessible Camp Areas Campsites People East Side 1 1 12 West Side 0 0 0 Total 1 1 12 Wood Fire Camp Areas Campsites East Side 8 13 West Side 9 13 Total 17 26 Stock Areas/Sites Individual Camp Areas Campsites People Stock East Side 3 3 18 24 West Side 3 3 18 24 Total 6 6 36 48 Group Camp Areas Campsites People Stock East Side 2 2 24 32 West Side 2 2 24 32 Total 4 4 48 64 Llama only Camp Areas Campsites People Stock East Side 2 2 14 10 West Side1175 Total 3 3 21 15 Wood Fire Camp Areas Campsites East Side 8 13 West Side 9 13 Total 17 26 Rocky Mountain National Park C-1 Backcountry/Wilderness Management Plan and Environmental Assessment Appendix C Crosscountry Areas Areas Parties People East Side 9 16 112 West Side 14 32 224 Total 23 48 336 Summer Totals for Designated, Stock and Crosscountry Areas Camp Areas Campsites/Parties People East Side 80 136 1004 West Side 84 131 969 Total 164 267 1973 Bivouac Areas Areas People East Side 11 88 West Side 0 0 Total 11 88 Winter Areas Areas Parties People East Side 32 136 1632 West Side 23 71 852 Total 55 207 2484 Rocky Mountain National Park C-2 Backcountry/Wilderness Management Plan and Environmental Assessment Appendix C Appendix C Table 2, Designated Camp Area/Sites Number -
1 Andrews Glacier in August 2016 Tyndall Glacier Lidar Scan in May
Final Report for “Glacier and perennial snowfield mass balance of Rocky Mountain National Park (ROMO): Past, Present, and Future” Task Agreement Number P16AC00826 PI Dr. Daniel McGrath June 28, 2019 Department of Geosciences Colorado State University [email protected] Andrews Glacier in August 2016 Tyndall Glacier LiDAR scan in May 2016 1 Summary of Key Project Outcomes • Over the past ~50 years, geodetic glacier mass balances for four glaciers along the Front Range have been highly variable; for example, Tyndall Glacier thickened slightly, while Arapaho Glacier thinned by >20 m. These glaciers are closely located in space (~30 km) and hence the regional climate forcing is comparable. This variability points to the important role of local topographic/climatological controls (such as wind-blown snow redistribution and topographic shading) on the mass balance of these very small glaciers (~0.1-0.2 km2). • Since 2001, glacier area (for 11 glaciers on the Front Range) has varied ± 40%, with changes most commonly driven by interannual variability in seasonal snow. However, between 2001 and 2017, the glaciers exhibited limited net change in area. Previous work (Hoffman et al., 2007) found that glacier area had started to decline starting in ~2000. • Seasonal mass turnover is very high for Andrews and Tyndall glaciers. On average, the glaciers gain and lose ~9 m of elevation each year. Such extraordinary amounts of snow accumulation is primarily the result of wind-blown snow redistribution into these basins (and to a certain degree, avalanching at Tyndall Glacier) and exceeds observed peak snow water equivalent at a nearby SNOTEL station by 5.5 times. -
Winter 2009 the California Lichen Society Seeks to Promote the Appreciation, Conservation and Study of Lichens
Bulletin of the California Lichen Society Volume 16 No. 2 Winter 2009 The California Lichen Society seeks to promote the appreciation, conservation and study of lichens. The interests of the Society include the entire western part of the continent, although the focus is on California. Dues categories (in $US per year): Student and fixed income - $10, Regular - $20 ($25 for foreign members), Family - $25, Sponsor and Libraries - $35, Donor - $50, Benefactor - $100 and Life Membership - $500 (one time) payable to the California Lichen Society, PO Box 7775 #21135 , San Francisco, California 94120-7775. Members receive the Bulletin and notices of meetings, field trips, lectures and workshops. Board Members of the California Lichen Society: President: Erin Martin, shastalichens gmail.com Vice President: Michelle Caisse Secretary: Patti Patterson Treasurer: Cheryl Beyer Editor: Tom Carlberg Committees of the California Lichen Society: Data Base: Bill Hill, chairperson Conservation: Eric Peterson, chairperson Education/Outreach: Erin Martin, chairperson Poster/Mini Guides: Janet Doell, chairperson Events/field trips/workshops: Judy Robertson, chairperson The Bulletin of the California Lichen Society (ISSN 1093-9148) is edited by Tom Carlberg, tcarlberg7 yahoo.com. The Bulletin has a review committee including Larry St. Clair, Shirley Tucker, William Sanders, and Richard Moe, and is produced by Eric Peterson. The Bulletin welcomes manuscripts on technical topics in lichenology relating to western North America and on conservation of the lichens, as well as news of lichenologists and their activities. The best way to submit manuscripts is by e-mail attachments or on a CD in the format of a major word processor (DOC or RTF preferred). -
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. -
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 -
Fegel Colostate 0053N 13488.Pdf (1.978Mb)
THESIS BETWEEN A ROCK AND A HARD PLACE; THE CHEMISTRY, BIOLOGY, AND LABILITY OF GLACIAL MELTWATERS IN THE AMERICAN WEST Submitted by Timothy Scott Fegel II Graduate Degree Program in Ecology In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Spring 2016 Master’s Committee: Advisor: Jill Baron Co-advisor: Edward Hall Michael Gooseff Copyright by Timothy Scott Fegel 2016 All Rights Reserved ABSTRACT BETWEEN A ROCK AND A HARD PLACE; THE CHEMISTRY, BIOLOGY, AND LABILITY OF GLACIAL MELTWATERS IN THE AMERICAN WEST Glaciers and rock glaciers supply water and nutrients to headwater mountain lakes and streams across all regions of the American West. The resulting changes in volume, timing, and chemistry of meltwater discharged by these features appears to be having significant effects on the adjacent alpine headwater ecosystems they feed. Whereas both glaciers and rock glaciers are sources of seasonal meltwater, sediment, and solutes to headwater ecosystems, differences in meltwater characteristics between glacial types, and its affect on biological productivity, is poorly documented. Here we present a comparative study of the metal, nutrient, and microbial characteristics of glacial and rock glacial influence on headwater ecosystems in three mountain ranges of the contiguous U.S.: the Cascade Mountains, Rocky Mountains, and Sierra Nevada. Several meltwater characteristics (water temperature, conductivity, pH, heavy metals, nutrients, complexity of dissolved organic matter (DOM), and bacterial richness and diversity) differed significantly between glacier and rock glacier 2+ 3+ meltwaters, while other characteristics (Ca , Fe , SiO2 concentrations, reactive nitrogen, and microbial processing of DOM) showed distinct charcteristics between mountain ranges regardless of meltwater source. -
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. -
What Is a Lichen – a Prison Or an Opportunity? Lichens Cannot Be Classified As Plants
What is a lichen – a prison or an opportunity? Lichens cannot be classified as plants. They are associations between cup fungi ascomycetes plus either green algae (Trebouxia sp.) or cyanobacteria (e.g. Nostoc), members of three kingdoms outside the plant kingdom. Simon Schwendener discovered the dual nature of lichens in 1869 : Ascomycetes surround some single- celled green algae with a fibrous net to compel the new slaves to work for them, a view that was replaced with romanticized notion of a harmonious symbiosis. Mycobiont gets sugar alcohols from green algae or glucose + nitrogen from cyanobacteria, which are stored in an inacessible form (e.g. mannitol). Lichens Species & Diversity Lichens consist of a fungus (the mycobiont, mostly an ascomycete ) & a photosynthetic partner (the photobiont or phycobiont ), usually either a green alga (commonly Trebouxia ) or cyanobacterium (c. Nostoc ) All lichens have an upper cortex , which is a dense, protective skin of fungal tissue that acts l ike a blind that opens after watering . Below that is a photosynthetic layer, which can be a colony of either green algae or cyanobacteria. Then there is a layer of loose threads (hyphae) of the fungus, called the medulla or the medullary layer . Fructicose & Foliose lichens have a lower cortex , others just have an exposed medulla. Crustose lichens never have a lower cortex-their fungal layer attaches firmly to the substrate. What is that? Is that a plant? Is that a fungus? Is that a lichen? What the …halloh! Spanish moss (Tillandsia usneoides ) Usnea is a lichen (a composite organism closely resembles its namesake ( Usnea , or made from algae and fungi) and is referred beard lichen), but in fact it is not to as Old Man's Beard. -
Frey† Udc 577.13 : 582.29
FACTA UNIVERSITATIS Series: Physics, Chemistry and Technology Vol. 14, No 2, 2016, pp. 125 - 133 DOI: 10.2298/FUPCT1602125Z ISOLATION AND IDENTIFICATION OF SECONDARY METABOLITES OF UMBILICARIA CRUSTULOSA (ACH.) FREY† UDC 577.13 : 582.29 Ivana Zlatanović, Goran Petrović, Olga Jovanović, Ivana Zrnzević, Gordana S. Stojanović Department of Chemistry, Faculty of Sciences and Mathematics, University of Niš, Niš, Serbia Abstract. Herein, we have studied secondary metabolites of Umbilicaria crustulosa (Ach.) Frey. By using preparative HPLC, four compounds were isolated from the U. crustulosa methanol extract. The structure of isolated lichen substances was determined on the basis of their 1H, 13C and 2D NMR spectra as follows: methyl orsellinate, lecanoric acid, methyl lecanorate and gyrophoric acid. In addition to methanol, the composition of acetone and ethanol extracts were also studied (analytical HPLC). Relative distributions (%) of the detected constituents were as follows (in methanol/acetone/ethanol extracts): methyl orsellinate (5.7/1.5/0.9), lecanoric acid (17.9/5.7/6.7), crustinic acid (8.0/2.8/2.5), methyl lecanorate (4.8/0/0) and gyrophoric acid (59.2/78.0/85.7). A significant difference in the chemical profiles of the studied extracts was in the presence/absence of methyl esters of lichen acids. Nonetheless, the chemical composition of the ethanol extracts (no ethyl esters were detected) and the fact that treatment of acetone and ethanol extracts with methanol does not lead to changes in their composition suggests that methyl esters were not artifacts of the isolation procedure. The lower content of methyl orsellinate and the absence of methyl lecanorate from acetone and ethanol extracts may be the result of different solubilities of these compounds in methanol, ethanol and acetone. -
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. -
Fall 2020 Newsletter
Windmill Hill Pinnacle Association Pinnacle News Fall 2020 Pivoting in the Pandemic By John Gregg The Pinnacle trails have remained a popular outlet during the COVID-19 pandemic, and we hope you are continuing to enjoy them. A walk in the woods with a friend—socially distanced and with a mask at hand, of course—is one of the best ways to relieve some stress, get some exercise, and enjoy the natural world around us. Regrettably, the ongoing pandemic has forced us to cancel much of our programming, including Accessi- bility Day. But we do have something to look forward to as the weather gets a little colder. Later this fall, we will be offering a program highlighting the new book The Windmill Hill Pinnacle Association Story: How did they get all that land?, which tells the history of the Windmill Ridge Nature Reserve and its trails, and how it came to be. Authors Rosalyn Shaoul and Libby Mills will discuss what’s in the book—including detailed maps, graceful paintings, and key photos—and how a grassroots effort that started in Westminster West soon grew to encompass about 2,100 acres in five towns, stretching from Westminster to Grafton and including Brookline, Rockingham, and Athens. In addition, the program will also include the first public airing of How It All Began, a 16-minute video on the Pinnacle Association by Wendy Wallas, co-produced with Libby and Rosalyn. The video includes footage of the dedication of the Jamie Latham Trail in 1997. Stay tuned for more details on when and how to view the program.