Mount Lorette and Beaver Mines, Alberta, and Steeples Bc, Spring 2020
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2018 Green Notes Newsletter
SOUTHERN ALBERTA CHAPTER GREEN NOTES NEWSLETTER SUMMER | 2018 CELEBRATING ALBERTA’S OUTDOOR HERITAGE SOUTHERN ALBERTA CHAPTER CPAWS Southern Alberta acknowledges the traditional territories of the people of the Treaty 7 region in Southern Alberta, which includes the Blackfoot Confederacy (comprising the Siksika, Piikani, and Kainai First Nations), the Tsuut’ina First Nation, and the Stoney Nakoda (including the Chiniki, Bearspaw, and Wesley First Nations). Southern Alberta is also home to Region III of the Métis Nation of Alberta. Chapter Team Anne-Marie Syslak | Executive Director Katie Morrison | Conservation Director Jaclyn Angotti | Education Director Kirsten Olson | Office & Fund Program Administrator Ian Harker | Communications Coordinator Peter Zimmerman | Parks Program Supervisor Becky Best-Bertwistle | Conservation Engagement Coordinator Vanessa Bilan | Environmental Educator, Hiking Guide Alex Mowat | Hiking Guide Julie Walker | Hiking Guide Justin Howse | Hiking Guide Lauren Bally | Hiking Guide Edita Sakarova | Bookkeeper Chapter Board of Directors Andre De Lebeeck | Secretary Jim Donohue | Treasurer, Vice Chair Doug Firby Ross Glenfield Jeff Goldberg Steve Hrudey Peter Kloiber Megan Leung Jon Mee Cinthia Nemoto Phil Nykyforuk | Chair Editorial & Design Ian Harker Neda Russell Cover Photo | Stephen Legault | Headwaters of the Sheep River, in the Burns Lake region, Elbow-Sheep Wildland Park Green Notes Newsletter is published by the Canadian Parks and Wilderness Society Southern Alberta Chapter (CPAWS SAB) (charity # 10686 5272 RR000I) © 2018. Green Notes is printed on Post Consumer recycled content. Photo | IainPhoto Reid CPAWS Southern Alberta | Celebrating Alberta’s Outdoor Heritage Keeping the West Wild Anne-Marie Syslak | Executive Director, CPAWS Southern Alberta hen you ask an Albertan about their favourite of the region, while still allowing room for park or wilderness area it doesn’t take long different recreational users. -
MOUNT LORETTE, FALL 2013 Introduction
MOUNT LORETTE, FALL 2013 With a note on the Steeples, BC, site Peter Sherrington Research Director, Rocky Mountain Eagle Research Foundation www.eaglewatch.ca Summary and highlights This was the 22nd consecutive year that some form of fall count has been conducted by RMERF members and was the 21st conducted at Mount Lorette. Despite generally favourable observing conditions and a well conducted count the combined species count of 3110 is 25.4 % below average and is the third lowest valid fall count for the site. Both the September and November counts were the lowest ever. All species occurred in below average numbers, and the count of 95 Bald Eagles was the lowest ever for the site. Of the nine species that occurred in sufficient numbers to assess median passage dates, six were later than average (although only Sharp-shinned Hawk and Cooper's Hawk were significantly so), three were earlier than average, and the combined-species passage date was one day later than average. The Golden Eagle count of 2782 is 21.8% below average and is also the third- lowest valid fall count for the site, despite the fact that the highest single day count of 496 on October 14 was the fourth highest for the site. The declining trend for the species at the site is maintained. No systematic counts were conducted at the Piitaistakis-South Livingstone site, and a reconnaissance count of sixteen short days was conducted at the Steeples site on the western flanks of the Rocky Mountains near Cranbrook, BC. Introduction The Mount Lorette site is located in the Kananaskis Valley in the Front Ranges of the Rocky Mountains (50o58’N 115o8’W) 70 km due west of Calgary and immediately north-east of the Nakiska Ski Hill on Mount Allan. -
MOUNT LORETTE, FALL 2010 with Notes on the Steeples, BC Site Www
MOUNT LORETTE, FALL 2010 with notes on the Steeples, BC site www.eaglewatch.ca Peter Sherrington Research Director, Rocky Mountain Eagle Research Foundation Introduction The Mount Lorette site is located in the Kananaskis Valley in the Front Ranges of the Rocky Mountains (50o58’N 115o8’W) 70km due west of Calgary and immediately north-east of the Nakiska Ski Hill on Mount Allan. At this point the valley trends north-south and cuts obliquely across the NW-SE oriented trend of the Front Ranges. To the east of the observation site the Fisher Range has an average elevation of about 2500m with Mt. McDougall rising to 2726m. Mount Lorette itself is 2487m and is a continuation of the Fisher Range to the NW. To the west the mountains of the Kananaskis Range are somewhat higher and include Mount Kidd (2958m), Mount Bogart (3144m) and Mount Allan (2819m). The observation site is in a cleared area on the valley floor known as the Hay Meadow at about 1433m. The site allows 360o views of the surrounding mountains and allows monitoring of raptors moving along the mountain ridges to the east and west, and especially those crossing the valley between Mount Lorette and the north end of the Fisher Range. The site is unique in that it allows observation of approximately the same high percentage of a population of migratory Golden Eagles both in spring and fall at exactly the same site, which has in the past been occupied for up to 190 days in a year. When downslope cloud obscures these mountains an alternate site at Lusk Creek, 13km NE of the Hay Meadow site, is used to observe birds moving along the westernmost foothills ridge that have been displaced to the east from the Front Ranges. -
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 .................................................................................................................. -
Structural Control of the Morphometry of Open Rock Basins, Kananaskis Region, Canadian Rocky Mountains
5" %~ '.5" :7~, 6[mU ELSEVIER Geomorphology 22 (1998) 313-324 Structural control of the morphometry of open rock basins, Kananaskis region, Canadian Rocky Mountains D.J. Sauchyn a,*, D.M. Cruden b, X.Q. Hu c,1 a Department of Geography, University of Regina, Regina, Saskatchewan $4S OA2, Canada b Department of Civil and Environmental Engineering, University of Alberta, Edmonton, Alberta T6G 2G7, Canada c Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada Received 12 September 1996; revised 18 July 1997; accepted 14 August 1997 Abstract The morphometry of chutes (couloirs), rock funnels, and open cirques are related to the structure of dissected rock masses in the Kananaslds region of the Canadian Rocky Mountains. Data for ten morphometric variables were derived from digital elevation models of 56 open rock basins. The basins were classified structurally according to the relative orientations of bedding planes and the rock slopes. A hypothesis of no differences in morphometry among structural classes is rejected from the results of nonparametric analysis of variance and paired comparisons of rank scores. Basins on dip and overdip slopes have a distinct :size, and those on anaclinal slopes have a distinct width and shape. Variation in morphometry from low compactness and area/relief (chutes) to high compactness and low area/relief (funnels) to high compactness and area/relief (open cirques) corresponds to a change in dominant structure from orthoclinal to dip-overdip to underdip to anaclinal. The dip of bedding planes relative to the slope of rockwalls controls the mode of initial displacement of joint blocks and, thereby, the spatial distribution of the retreat of rockwalls. -
Free Flight Vol Libre
Dec/Jan 6/93 free flight • vol libre POPOTTPOPOURRIURRI YES! It’s “Don’t forget time”. The clubs must remember to record total flights for all club and private gliders at the end of the year and have the information available to fill out the stats forms mailed out by Randy Saueracker. Randy and/or your Zone Director will be contacting those clubs which are late with their returns. Thank you in advance for your prompt response in returning these statistics. Harold Eley, our Trophy and Claims Chairman, will also be expecting claims from all pilots who have made worthy flights and may be eligible for any of the SAC trophies. So pilots, get busy. Richard Longhurst, our Insurance Chairman, reports that damage claims are very high and it’s very likely that there will be some upward adjustments to premiums in the coming year. Some- how we must break the chain of BAD decisions and lack of forethought in handling our gliders. I sometimes wonder if being TOO optimistic is part of the problem. If we acted as if we were not insured, would we fly and handle our gliders with more care? Continuing with insurance information, we have a very good “out of country” policy to cover injuries and hospital care due to gliding accidents, but so far there have been very few premiums sold. Those pilots going south this winter please remember to obtain your coverage through the SAC policy. All clubs were sent brochures and application forms this spring. Everyone will have received by now their 1994 membership cards and Pioneer Trust Fund donation card and letter. -
Commissioner Report-1913.Pdf
Photo by John Woodruff. Reflection of Mt. Run die in Vermilion Lakes, Banff, DEPARTMENT OF THE INTERIOR DOMINION OF CANADA. REPORT COMMISSIONER OF DOMINION PARKS FOlt TUB YEAR ENDING MAliCH 31 1913 I'ART V., ANNUAL REPORT, 1918 OTTAWA GOVERNMENT PRINTING BUREAU 1914 50406—1} DOMINION PARKS REPORT OF THE COMISSIONER OF DOMINION PARKS. DOMINION PARKS BRANCH, OTTAWA, September 30, 1913. W. W. CORY, Esq., C.M.G., Deputy Minister of the Interior. SIR,—I beg to submit my second annual report as Commissioner of Dominion Parks, covering the fiscal year 1912-13. Appended to it are reports from the Chief Superintendent of Dominion Parks and from the Superintendents of the various Parks. These reports show in detail the substantial progress made during the year in the matter of development work. My own report, therefore, is confined largely to a statement concerning the purposes served by National Parks and the useful develop ment work that such purposes suggest. CANADA'S PARKS. Extract from an address delivered at Ottawa. March 12, 1913, by His Royal Highness, the Duke of Connaught, before the Canadian Association for the Pre vention of Tuberculosis:— ' I feel that some apology is necessary for referring to the subject on which I now desire to touch, but the fact that this is the last onuortunity I shall have for public speaking before I go to England on leave must be my excuse. Also, the subject is allied with public health, which is one more reason for me to request your indulgence. ' I desire to refer shortly to the question of your Dominion Parks. -
Conodont Biofacies in a Ramp to Basin Setting (Latest Devonian and Earliest Carboniferous) in the Rocky Mountains of Southernmost Canada and Northern Montana
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Conodont biofacies in a ramp to basin setting (latest Devonian and earliest Carboniferous) in the Rocky Mountains of southernmost Canada and northern Montana by Lauret E. Savoy1 and Anita G. Harris 2 Open-File Report 93-184 This report is preliminary and has not been reviewed for conformity with Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. \ Department of Geology and Geography, Mount Holyoke College, South Hadley, MA 01075 2 U.S. Geological Survey, Reston, VA 22092 1993 TABLE OF CONTENTS ABSTRACT 1 INTRODUCTION 2 LITHOSTRATIGRAPHY AND DEPOSITIONAL SETTING 2 CONODONT BIOSTRATIGRAPHY AND BIOFACIES 8 Palliser Formation 8 Exshaw Formation 13 Banff Formation 13 Correlative units in the Lussier syncline 15 PALEOGEOGRAPfflC SETTING 17 CONCLUSION 23 ACKNOWLEDGMENTS 23 REFERENCES CITED 24 APPENDIX 1 38 FIGURES 1. Index map of sections examined and major structural features of the thrust and fold belt 3 2. Correlation chart of Upper Devonian and Lower Mississippian stratigraphic units. 4 3. Selected microfacies of the Palliser Formation. 5 4. Type section of Exshaw Formation, Jura Creek. 6 5. Lower part of Banff Formation, North Lost Creek. 7 6. Conodont distribution in Palliser and Exshaw formations, Inverted Ridge. 9 7. Conodont distribution in upper Palliser and lower Banff formations, Crowsnest Pass. 11 8. Conodont distribution in upper Palliser, Exshaw, and lower Banff formations, composite Jura Creek - Mount Buller section. 12 9. -
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 -
Michelle Nicole Murphy
Alberta Ski Resorts on the Eastern Slopes and Environmental Advocacy: Conservation Politics and Tourism Developments in Kananaskis Country, 1980-2000 By Michelle Nicole Murphy A thesis submitted in partial fulfillment of the requirements for the degree of Master of Arts in Recreation and Leisure Studies Faculty of Kinesiology, Sport, and Recreation University of Alberta © Michelle Nicole Murphy, 2018 ii Abstract This study investigates ski resort development and proposals on the eastern slopes of Alberta between 1980 and 2000 with a specific focus on Kananaskis Country. It highlights issues between conservation imperatives and recreation and sport development. It examines the site selection for the 1988 Winter Olympic Games to uncover the provincial government and Olympic Organizer’s lack of concern towards environmental issues and disregard for concerns brought up by environmental non-governmental organizations (ENGOs), recreational skiers, and the public. An analysis of conservation politics regarding the site selection of Mount Allan, the potential use of Mount Whitehorn (Lake Louise), and the Spray Lakes Ski Resort proposal looks closely at the strategies used by ENGOs to advocate for the environment. Through an exploration of conservation politics and land-use debates, this research project probes the role of Kananaskis Country as a multiple-use landscape to argue that between 1980 and 2000, a pro-development provincial government placed minimal value on environmental knowledge and expertise and chose to sacrifice important Alberta mountain habitats for ski resort development and economic gains. This was contrary to opposition from ENGOs, like the Sierra Club of Western Canada, and the public, who utilized strategic discourse to draw attention to environmental threats as a form of resistance to government decision- making. -
Mount Lorette and Vicki Ridge, Alberta Fall 2017
MOUNT LORETTE AND VICKI RIDGE, ALBERTA FALL 2017 With notes on the extended reconnaissance count at Steeples, BC Peter Sherrington Research Director, Rocky Mountain Eagle Research Foundation www.eaglewatch.ca Summary and highlights This was the 26th consecutive year that some form of fall count has been conducted by RMERF observers at Mount Lorette, it was the 4th consecutive count at Vicki Ridge which was the first complete count there, and the 9th consecutive reconnaissance count at the Steeples site in BC. All three counts experienced cooler weather than in recent years as La Niña oceanic conditions prevailed, and November was particularly cold and snowy. At Mount Lorette the combined species total of 3672 was 8.9% below the long-term average for valid counts and the Golden Eagle count of 3233 was 6% below the long-term average. Sixteen raptor species were recorded, but only 5 occurred in above average numbers. The high single- day Golden Eagle count of 426 on October 6 is the highest since 2013 and was 7.1% above average. The Golden Eagle immature:adult ratio of 0.49 is the highest ever and indicates a successful breeding season and the probable culmination of the current boreal Snowshoe Hare cycle. Seven species moved later than normal and 5 moved earlier, and the combined-species median passage date of October 14 was 2 days later than average. The first complete Vicki Ridge count in SW Alberta produced a record 4237 migrants of 17 species in 52 days, including record counts of 16 raptor species, most notably 515 Rough-legged Hawks which is a new record for any RMERF count. -
Environmentally Significant Areas Inventory of The
Environmentally Significant Areas Inventory of the Rocky Mountain Natural Region of Alberta Final Report by Kevin Timoney Treeline Ecological Research 21551 Twp. Rd. 520 Sherwood Park, AB T8E 1E3 email: [email protected] for Corporate Management Service Alberta Environmental Protection 12th Floor, Oxbridge Place 9820 - 106 St. Edmonton, AB T5K 2J6 17 January 1998 Contents ___________________________________________________________________ Abstract........................................................................................................................................ 1 Acknowledgements................................................................................................................... 2 Color Plates................................................................................................................................. 3 1. Purpose of the study ........................................................................................................... 6 1.1 Definition of AESA@................................................................................................... 6 1.2 Study Rationale ............................................................................................................ 6 2. Background on the Rocky Mountain Natural Region ............................................ 7 2.1 Geology ......................................................................................................................... 7 2.2 Weather and Climate...................................................................................................