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Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB 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 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
Summer Trail Assessment
SUMMER TRAIL ASSESSMENT A Guide to Management of Non-motorized Trails on the Jackson Ranger District, BTNF ʹͲʹͲ Table of Contents INTRODUCTION 0 TABLE OF CONTENTS I. INTRODUCTION PURPOSE AND NEED FOR CHANGE… …………………………………………………………. 2 HOW DOCUMENT WILL BE USED……………………………………………………………….. 4 DOCUMENT STRUCTURE AND DEVELOPMENT………….……………………………………… 5 POLICY FRAMEWORK …………….. ………………………………………………………….. 6 DEFINITIONS…………………………………………………………………………………… 6 II. TRAIL SYSTEM MANAGEMENT TRAIL SYSTEM GOALS ……………………………………………………………………….. 8 TRAIL SYSTEM TASKS ………………………………………………………………………... 9 TRAIL CARE ON THE GROUND ……………………………………………………. ………… 13 THE NATURE OF TRAIL IMPACT…………………………… ………………………………… 15 TRAIL RECREATION DESIRES……………………….………………………………….. ……. 19 WILDLIFE HABITAT INFORMATION…………………………………………………………….21 III. OVERVIEW OF THE TRAIL SYSTEM SYSTEM STATUS ………………………………………………………………………………23 MAP ..…………………………………… …………………………………………………… 26 FUNDING AND BACKLOG ………………………………………………………………………27 IV. GEOGRAPHIC AREA AND TRAIL SYSTEM GUIDANCE OVERVIEW OF KEY TRAIL SYSTEM NEEDS …………………………………………………… 27 GROS VENTRE WILDERNESS ………… ………………………………………………………. 29 MOUNT LEIDY HIGHLANDS ………………………………. …………………………………32 WYOMING RANGE / WILLOW CREEK ………..……………… ………………………………...35 PALISADES WSA / SNAKE RIVER RANGE. ……………………………………………………..38 SHADOW MOUNTAIN / DITCH CREEK……...…………………. ………………………………..41 MUNGER MOUNTAIN …………………… …………………………………………………… 43 CACHE-GAME (GREATER SNOW KING) … ………………...…………………………………...47 TETON PASS …………………….............…………………. …………………………………52 JACKSON HOLE MOUNTAIN RESORT ……… -
Oxygen Isotope Analysis of Mineralized Fault Planes, Five Springs Region, Bighorn Mountains, Wyoming
Oxygen isotope analysis of mineralized fault planes, Five Springs region, Bighorn Mountains, Wyoming Valerie Esser Department of Geology, The Colorado College, 14 E Cache La Poudre St., Colorado Springs, CO 80903 Faculty Sponsor: Christine Siddoway, The Colorado College INTRODUCTION Laramide uplifts juxtapose old basement rock against sedimentary cover rocks across thrust faults with a significant vertical component. They are common throughout the Rocky Mountain foreland, and the structural evolution of many of the basement block uplifts has been extensively studied (Snoke, 1997; Narr, 1993; Spang and Evans, 1988). However, the detailed timing and uplift history, thermal evolution, and the role of fluids during faulting of these ranges remain to be determined. The Bighorn Mountains of northern central Wyoming form a Laramide basement-cored uplift, and offer an ideal location to investigate the details of fluid circulation along faults. The Five Springs fault zone (Figure 1), a structurally well-studied section along the northwest flank of the Bighorn Mountains (Wise and Obi, 1992), has mineralization along minor fault planes that indicates the presence of fluids related to faulting. In this study, using laser- based micro-analytical techniques, _18O values of quartz, feldspar, and epidote grains were measured to investigate the fluids involved in the faulting. The temperatures calculated from _18O fractionations are hotter than expected temperatures for Laramide faulting, prompting one to consider the possibility that mineralization along these fault planes pre-dated the Laramide, or that hot, mid-crustal fluids played a role in Laramide deformation. GEOLOGIC SETTING AND BACKGROUND In their structural review of the Five Springs area, Wise and Obi (1992) examined a section of pervasively faulted granite where continuous exposures of the fault system bounding the Bighorn uplift are exposed in new road-cuts along Wyoming Highway Alternate 14 (figure 1). -
Chapter 3 Description of the Study Area
Chapter 3 Description of the study area Paul Taucher Melissa Thompson Nikolaus Gribb 3-17 The WBRB drainage basin covers approximately 25 percent streams and elevation. Clockwise from the Pryor Mountains in of the state in north-central and northwestern Wyoming, plus Montana, the boundary runs: smaller areas of south-central Montana. Figure 3-1 is an index map of the approximately 678 townships within the WBRB 1. Northward then southeastward along a Pryor mountain in Wyoming (625) and Montana (53). As determined from ridgeline bordering drainage intoWyoming, to the the GIS database developed for this study, the WBRB covers Wyoming/Montana state line; approximately 22,883 square miles (14.65 million acres) 2. Thence eastward along the Wyoming/Montana state line in Wyoming and 894 square miles (0.57 million acres) in and along a divide in the Bighorn Mountains; Montana. The WBRB encompasses federal, state, and privately 3. Thence generally south-southeastward along the arcuate owned land in all or part of eight Wyoming counties: ridge of the Bighorn Mountains to T39N, R87W; 4. Thence generally south-southwestward along a divide on the Casper Arch from T39N, R87W to the northwestern • All of Big Horn, Park, and Hot Springs counties tip of the Rattlesnake Hills, T34N, R89W; • Approximately 95 percent of Washakie County 5. Thence a short distance southeastward along the ridgeline • Approximately 85 percent of Fremont County of the Rattlesnake Hills into T33N, R88W; • Approximately 10 percent of Teton County 6. Thence irregularly west-southwestward along the Beaver • Small, relatively undeveloped parts of northwestern Divide (Beaver Rim) – an irregular drainage divide on Natrona and western Johnson counties the Casper arch north and west of the Granite Mountains – to T30N, R101W, where it meets the Continental Approximately 80 percent of Yellowstone National Park (in Divide; Park and Teton counties) is included in the drainage basin, as is 7. -
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Chapter 4 Geologic overview Andrea M. Loveland 4-39 he Northeast River Basins (NERB) study area covers tuations until the final retreat of the seaway in the Late Tapproximately 14.86 million acres in northeast- Cretaceous. ern Wyoming, southeastern Montana, western South Dakota, and western Nebraska. The geologic setting of The Laramide orogeny commenced in the Late the NERB includes Precambrian-cored uplifts formed Cretaceous and continued through the Early Eocene. during the Laramide orogeny and adjacent basins filled Crustal shortening was accommodated by displacement with Phanerozoic clastic and carbonate rocks. The fol- of Precambrian crystalline basement rocks and the over- lowing information regarding the NERB study area is lying sedimentary cover rocks (Brown, 1993). Basement- provided in this chapter: cored Laramide structures border the NERB on three sides: 1) the Bighorn Mountains to the west, 2) the • An overview of the geologic history Black Hills to the east, and 3) the Rattlesnake Hills and Hartville Uplift to the south (fig. 4-1). • A summary of the structural geology • An outline of significant mineral and energy The geologic setting of the NERB study area is illustrated resources on the bedrock geologic map in plate 1. This map also displays surface water, highways, political boundaries, • Geologic cross sections and state and county data. Inset maps on plate 1 show the distribution of lineaments and a structure-contour map of the top of the Precambrian basement. Nine cross sec- 4.1 GENERAL GEOLOGIC HISTORY tions show subsurface structure in the NERB (figs. 4-2 through 4-11). Descriptions of the Precambrian- through During the Paleozoic Era, the area that is now the Tertiary-aged stratigraphic units exposed in the study NERB was located on the western margin of the North area are included in appendix A, and are not addressed American craton in a shelfal environment. -
40° to 4S”, Capped by a Fine Granite Pinnacle. Eight Or Ten Pitches of FS of F6 on Excellent Rock Put Us on the Summit
182 THE AMERICAN ALPINE JOURNAL 40° to 4S”, capped by a fine granite pinnacle. Eight or ten pitches of FS of F6 on excellent rock put us on the summit. We found no evidence of previous climbers. NCCS III, F5 or F6. MICHAEL HELMS Washington-Cascade Mountains Witches Tower, Northeast Face. In August, 1976, Bob Gundrum, Paul McKnight, Dave Fox and I completed a new route on this face, starting in the lower left of the face. We had several hundred feet of easier climbing until we crossed the central depression to the right. Higher we recrossed the depression to the left (F8) and followed up a dihedral (FS). From there the climbing eased to the summit. NCCS II, F8. DUANE CONSTANTINO Three O’clock Rock, Darrington Area. In April Tom Saunders and I completed a new four-pitch route on this formation, “Tidbits.” Some- what left of the Big Tree 1 route, we climbed a dike on an apron below several large roofs. Near the top of the slab, we moved right to belay. We followed the slab to just below a roof (FlO), crossed the roof to a horizontal crack, proceeded up and left on a crescent-shaped ledge (F9) and moved right to belay. We climbed left on a ledge for 20 feet, diag- onaled back right to a small tree and ascended left of the tree to a belay (FlO). We climbed to a roof, which we crossed on the left, diagonaled back right to a small tree and ascended left of the tree to a belay (FlO). -
Yakima-Valley-Wineries-Map-Web.Pdf
TO CHINOOK PASS Oak Creek Bron Yr Aur Brewstillery 410 Brewing Co. Gard Ellensburg Vintners NACHES Canyon 12 Winery 821 TO WHITE PASS TIETON Yakima Rive S. Naches Road Southard Winery YAKIMA AND PACKWOOD TO ELLENSBURG Rowe Hill Dr Rowe Fontaine Estates AND SEATTLE NACHES 82 HEIGHTS 12 SELAH 823 AVA McGonagle Rd Goodlander Rd Rider Thompson Rd Nache Rive N Cellars AREA The Yakima Valley grows more hops, grapes and fruit than anywhere else in the Pacific Northwest. Cowiche Creek Valley The Bier Den Brewing Company Wherry Rd Brewing Co. AntoLin Cellars Come experience award-winning wine, unique craft beer and hand-crafted cider straight from the source. Naches Heights Weikel Rd Tieton Cider Works 5th Line Brewing Company Vineyard Visitor Information Center Fruitvale Blvd Wilridge Vineyard, 2 River Rd Winery & Distillery Hop Capital Single Hill Brewing Company Brewing Marble Rd The Distillarium YAKIMA ZILLAH PROSSER RED MOUNTAIN COLUMBIA GORGE BREWERY/CIDERY/DISTILLERY Bale Breaker Brewing Co. Swede Hill Distillery Wandering Hop Kana Winery YAKIMA Zier Rd Brewing Co. Yakima Air Terminal 24 Draper Rd MOXEE Gilbert 1 ZILLAH Cellars The KilnUNION GAP Winery Taproom Owen Roe 24 Wiley Rd Treveri Cellars RED MOUNTAIN AREA Knight Hill Winery PROSSER VanArnam Vineyards Freehand Cellars Hyatt Vineyards AREA Masset Two Mountain Winery Hightower Hamilton Ruby Magdalena Purple Star Cellars Winery Vineyards Dineen Vineyards Winery Cellars HopTown Tapteil Vineyard Wood Fired Pizza J.Bell Whitman Hill Winery 225 YAKIMA VALLEY Cellars NE Roza Road E. Corral Creek Road Silver Lake Winery/Vitis Spirits N. Whitmore PR NW E. 583 PR NE Col Solare Red Clark Rd Lombard Loop Sheridan Vineyard E. -
Department of the Interior Miscellaneous Field Studies United States Geological Survey Map Mf-1597-A Pamphlet Mineral Resource P
DEPARTMENT OF THE INTERIOR MISCELLANEOUS FIELD STUDIES UNITED STATES GEOLOGICAL SURVEY MAP MF-1597-A PAMPHLET MINERAL RESOURCE POTENTIAL OF THE NORTHERN PART OF THE WASHAKIE WILDERNESS AND NEARBY ROADLESS AREAS, PARK COUNTY, WYOMING By John C. Antweiler, Douglas W. Rankin, Frederick S. Fisher, Carl L. Long, and J. David Love, U.S. Geological Survey and Carl L. Bieniewski and R. Craig Smith, U.S. Bureau of Mines STUDIES RELATED TO WILDERNESS Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and related acts, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as "wilderness," "wild," or "canoe" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of the suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report discusses the results of a mineral survey of the northern part of the Washakie Wilderness and nearby roadless areas, Shoshone National Forest, Park County, Wyo. The area was established as a wilderness by Public Law 88-577, September 3, 1964. The nearby roadless areas were classified as further planning areas during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. -
Annals of Wyoming
* Annate of looming VOL. 8 JULY No. 1 CONTENTS Trip of Col. James McLaughlin, Indian Inspector, — to the Big Horn Hot Springs, Wyoming By John Small Diary Kept by W. A. Richards in Summer of 1873 Boundaries of the State Reserve By Clarence T. Johnson Wyoming Birds By Mrs. E. E. Waltman Why the Meadowlark Was Chosen as the State Bird of Wyoming By Hazel Harper Sample Pickett Washakie Studies in the Settlement and Economic Development of Wyoming By Clyde Meehan Owens Accessions Published Quarterly by the STATE DEPARTMENT OF HISTORY Mrs. Cyrus Beard, Historian Cheyenne, Wyo. Annate of ^BBIpommg VOL. 8 JULY No. 1 CONTENTS Trip of Col. James McLaughlin, Indian Inspector, to the Big Horn Hot Springs, Wyoming By John Small Diary Kept by W. A. Richards in Summer of 1873 Boundaries of the State Reserve By Clarence T. Johnson Wyoming Birds —By Mrs. E. E. Waltman Why the Meadowlark Was Chosen as the State Bird of Wyoming By Hazel Harper Sample Pickett Washakie Studies in the Settlement and Economic Development of Wyoming By Clyde Meehan Owens Accessions Published Quarterly by the STATE DEPARTMENT OF HISTORY Mr§. Cyrus Beard, Historian Cheyenne, Wyo, STATE HISTORICAL BOARD Acting Governor A. M. Clark Secretary of State A. M. Clark State Librarian Mrs. Clare E. Ausherman Secretary of Board Mrs. Cyrus Beard ADVISORY BOARD Judge E. H. Fourt Lander Dr. Grace R. Hebard Laramie Mrs. C. L. Vandevender Basin Mr. L. C. Bishop Douglas Mr. Phillip E. Winter _ Casper Mrs. R. A. Ferguson Wheatland Mr. Howard B. Lott Buffalo Miss Spaeth Gillette Mrs. -
Ecology & Wonder in the Canadian Rocky Mountain Parks World Heritage Site
Ecology & Wonder Ecology & Wonder in the Canadian Rocky Mountain Parks World Heritage Site Robert William Sandford Frontispiece: The © 2010 Robert W. Sandford Grand Sentinel The Grand Sentinel is a great Published by AU Press, Athabasca University stone tower located just below 1200, 10011 – 109 Street the summit of Sentinel Pass in Edmonton, AB T5J 3S8 Banff National Park. Were it located outside of the dense cluster of astounding natural Library and Archives Canada Cataloguing in Publication features contained within Canada’s mountain parks, it Sandford, Robert W. would be one of the wonders of Ecology & wonder in the Canadian Rocky Mountain Parks World Heritage the world. As it is, it is just one Site / Robert William Sandford. more landscape miracle that can be seen from the summit Includes bibliographical references and index. of the pass. Issued also in electronic format (978-1-897425-58-9). Photograph by R.W. Sandford. ISBN 978-1-897425-57-2 1. Canadian Rocky Mountain Parks World Heritage Site (Alta. and B.C.)--Environmental conditions. 2. National parks and reserves--Canadian Rocky Mountain Parks World Heritage Site (Alta. and B.C.)--Management. 3. Environmental protection--Canadian Rocky Mountain Parks World Heritage Site (Alta. and B.C.). I. Title. II. Title: Ecology and wonder. QH106.2.R6S26 2010 333.7’209712332 C2010-900473-6 Cover and book design by Virginia Penny, Interpret Design, Inc. Printed and bound in Canada by Marquis Book Printing. This publication is licensed under a Creative Commons License, Attribution- Noncommercial-No Derivative Works 2.5 Canada, see www.creativecommons.org. The text may be reproduced for non-commercial purposes, provided that credit is given to the original author. -
Wsgs-2016-Ofr-04.Pdf
WYOMING STATE GEOLOGICAL SU RVEY OPEN FILE REPORT 2016-4 Th omas A. Drean, Director and State Geolog ist Ervay Basin SW 1:24,000-scale Laramie, Wyoming Bedrock Geolog ic Map (M Interpreting the past, providing for the future E R A IL R A E ) N S C P C M A H ( G ) (ERVAY BASIN) Qal 46 Qls ^cr EXPLANATION ^cr Kf Kmr CORRELATION OF MAP U NITS Qp 21 45 DESCRIPTION OF MAP U NITS Cenozoic Qal Holocene Qls Qve Qp ? QU AT ERNARY Kt Pleistocene Qal ^Pg Qal ? ? ? j Alluvium (Holocene)— U nconsolida ted to poorly consolida ted sa nd, silt, cla y, coa rse gra vels, a nd 34 Pliocene 31 20 ? cobbles, m a inly a long loca l interm ittent strea m courses; loca lly interm ixed with colluvium . T hickness Qp Jm Kcv U nconform ity T NEOGENE less tha n 8 m (26 ft) ^cp Js 24 ^ca E Qls Tsr Miocene Landslide deb ris (Holocene and Pleistocene[?])— Blocks a nd slum ps of loca lly derived bedrock from 29 10 R steep a nd unsta ble slopes; m ost com m on in Cloverly Form a tion a s well a s Wa gon Bed Form a tion Qp U nconform ity *t 19 a long Bea ver Rim . T hickness less tha n 122 m (400 ft) 11 T CENOZ OIC 20 ^cr Twr Oligocene Qve I Volcanic eluvium (Holocene and Pleistocene[?])— U nconsolida ted rem na nts derived from in situ *Ma *t R U nconform ity wea thering of Ra ttlesna ke Hills volca nic rocks; gra des into Ra ttlesna ke Hills volca nics a nd volca nic *t A A conglom era tes within Wa gon Bed Form a tion. -
The Fate of Dinwoody Glacier: Present State of Mass Balance and Downstream Impacts of Glacier Runoff
THESIS THE FATE OF DINWOODY GLACIER: PRESENT STATE OF MASS BALANCE AND DOWNSTREAM IMPACTS OF GLACIER RUNOFF. Submitted by Brooke E. Stamper Graduate Degree Program in Ecology In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Summer 2018 Master’s Committee: Advisor: Andrew K. Bliss Neil S. Grigg Steven R. Fassnacht Copyright by Brooke E. Stamper 2018 All Rights Reserved ABSTRACT THE FATE OF DINWOODY GLACIER: PRESENT STATE OF MASS BALANCE AND DOWNSTREAM IMPACTS OF GLACIER RUNOFF. The Wind River Range in Wyoming supports many of the few remaining continental glaciers of the North American Rocky Mountains; the glacier meltwater runoff feeds four major river sys- tems within the U.S. West. Runoff from glaciers affects downstream ecosystems by influencing the quantity, seasonality, and chemistry of the water. We describe the present state of Dinwoody Glacier, the fourth largest glacier in the Wind River Range. We utilize photogrammetry, snow depth measurements, and ablation measurements to characterize surface mass balance for summer of 2017. Localized and nearby stream gauge measurements help to quantify glacial meltwater runoff inputs to Dinwoody Creek. Both of these methods allowed us to put the changes of the Dinwoody Glacier into the broader context of the Missouri River Watershed. If melted, Dinwoody Glacier would no longer provide a reliable source of melt water for thousands of people living in the Missouri River Watershed. Understanding how shrinking glaciers and decreasing melt-water runoff will impact communities and ecosystems downstream is critical for effective environmental management. The response of the Wind River glaciers to future climate is uncertain; however, past research has shown declines in glacial mass, snow cover, snowmelt timing and stream power.