The Road to the Place of the Eagles
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Field Trip Guide Soils and Landscapes of the Front Ranges
1 Field Trip Guide Soils and Landscapes of the Front Ranges, Foothills, and Great Plains Canadian Society of Soil Science Annual Meeting, Banff, Alberta May 2014 Field trip leaders: Dan Pennock (U. of Saskatchewan) and Paul Sanborn (U. Northern British Columbia) Field Guide Compiled by: Dan and Lea Pennock This Guidebook could be referenced as: Pennock D. and L. Pennock. 2014. Soils and Landscapes of the Front Ranges, Foothills, and Great Plains. Field Trip Guide. Canadian Society of Soil Science Annual Meeting, Banff, Alberta May 2014. 18 p. 2 3 Banff Park In the fall of 1883, three Canadian Pacific Railway construction workers stumbled across a cave containing hot springs on the eastern slopes of Alberta's Rocky Mountains. From that humble beginning was born Banff National Park, Canada's first national park and the world's third. Spanning 6,641 square kilometres (2,564 square miles) of valleys, mountains, glaciers, forests, meadows and rivers, Banff National Park is one of the world's premier destination spots. In Banff’s early years, The Canadian Pacific Railway built the Banff Springs Hotel and Chateau Lake Louise, and attracted tourists through extensive advertising. In the early 20th century, roads were built in Banff, at times by war internees, and through Great Depression-era public works projects. Since the 1960s, park accommodations have been open all year, with annual tourism visits to Banff increasing to over 5 million in the 1990s. Millions more pass through the park on the Trans-Canada Highway. As Banff is one of the world's most visited national parks, the health of its ecosystem has been threatened. -
In This Issue
In This Issue... Characteristics of polygonal faulting in the Lea Park/Milk River Formations 2019 CSPG Classic Golf 2019 – CSPG Mixed Golf 30th Anniversary Tournament RETURN UNDELIVERABLE CANADIAN ADDRESSES TO: CSPG – 150, 540 – 5th Ave SW Calgary, AB, T2P 0M2 $7.00 NOVEMBER/DECEMBER 2019 VOLUME 46, ISSUE 6 Canadian Publication Mail Contract – 40070050 December Technical Luncheon & geoLOGIC Holiday Social Fairmont Palliser | Crystal Ballroom DECEMBERDECEMBER 5th,5th, 20192019 LUNCHEONLUNCHEON SPEAKERSPEAKER Wine & Appetizers 10:30-11:30 Steven Bryant Technical Luncheon 11:30 - 1:00 Sponsored By: BOARD OF DIRECTORS 2019 CSPG OFFICE PRESIDENT PRESIDENT ELECT #150, 540 - 5th Ave SW Marty Hewitt Jen Russel-Houston Calgary, Alberta, Canada T2P 0M2 Tel: 403-264-5610 [email protected] Osum Oil Sands Corp. Web: www.cspg.org Please visit our website for all tickets sales and event/course registrations [email protected] Office hours: Monday to Friday, 8:30am to 4:00pm The CSPG Office is Closed the 1st and 3rd Friday of every month. OFFICE CONTACTS Membership Inquiries PAST PRESIDENT FINANCE DIRECTOR Tel: 403-264-5610 Email: [email protected] Clinton Tippett Ray Geuder Advertising Inquiries: Emma MacPherson Tel: 403-513-1230 Email: [email protected] [email protected] [email protected] Sponsorship Opportunities: Lis Bjeld Tel: 403-513-1235, Email: [email protected] Conference Inquiries: Kristy Casebeer Tel: 403-513-1233 Email: [email protected] Accounting Inquiries: Kasandra Amaro Tel: 403-513-1232 Email: [email protected] FINANCE DIRECTOR Education Inquiries: Kristy Casebeer Tel: 403-513-1233 Email: [email protected] DIRECTOR ELECT Laurie Brazzoni Executive Director: Lis Bjeld Kelty Latos Tel: 403-513-1235, Email: [email protected] [email protected] EDITORS/AUTHORS ConocoPhillips Canada Ltd. -
Thesis Formatting
Resilience of Mountain Pond Communities to Extreme Thermal Regime Shifts by Mitchell Alexander Johnsen A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Ecology Department of Biological Sciences University of Alberta © Mitchell Alexander Johnsen, 2019 Abstract Elevational gradients are ideal ecological venues for testing how communities respond to environmental changes associated with global warming. Recent warming rates have been shown to increase with elevation, thereby potentially having adverse effects on cold-adapted alpine communities. Additionally, as selective pressures vary along elevational gradients, alpine and montane communities may differ in their adaptive potential to novel thermal regimes. I tested this hypothesis by conducting a replicated two-factor (source × elevation) experiment involving a reciprocal transplant of alpine and montane pond communities across two elevational sites (1390 m versus 2345 m asl). At each elevation, half of the mesocosms were inoculated with zooplankton and sedimentary egg-banks collected from alpine ponds while the other mesocosms were similarly seeded with zooplankton and sedimentary egg-banks collected from montane ponds in 2016. After overwintering, the mesocosms were sampled for temperature and plankton during the ice-free periods of 2017 and 2018. The mesocosms at the low elevation were 8.0 ± 1.2 ºC warmer than those at the high elevation. Elevation significantly affected total zooplankton biomass, whereas source effects did not. Elevation effects revealed that the temperature difference between sites affected the phenology of species within the assembled communities, but not their total biomass, and neither assemblage displayed local adaptation to a particular elevation. Functional trait analysis revealed that the warmer environment selected for smaller body size and asexual reproduction as a warmer thermal regime stimulated several small parthenogenetic herbivores while suppressing larger, obligate sexual omnivores. -
Ya Ha Tinda Elk Project Annual Report 2016-2017
Ya Ha Tinda Elk Project Annual Report 2016-2017 Ya Ha Tinda Elk Project Annual Report 2016 - 2017 Submitted to: Parks Canada, Alberta Environment and Parks & Project Stakeholders Prepared by: Hans Martin & Mark Hebblewhite University of Montana & Jodi Berg, Kara MacAulay, Mitchell Flowers, Eric Spilker, Evelyn Merrill University of Alberta 1 Ya Ha Tinda Elk Project Annual Report 2016-2017 ACKNOWLEDGEMENTS We thank Parks Canada staff Blair Fyten, Jesse, Whitington, David Gummer, and Bill Hunt for providing logistical and financial support, especially during the winter capture season. For their never-ending help, patience and understanding, we thank the Ya Ha Tinda ranch staff: Rick and Jean Smith, Rob Jennings, James Spidell and Tom McKenzie. Anne Hubbs (AB ESRD), Rachel Cook (NCASI), P.J. White (NPS), Bruce Johnson (OR DFW), Shannon Barber-Meyer (USGS), Simone Ciuti (U Alberta), and Holger Bohm (U Alberta) all provided helpful advice and discussions, and Dr. Todd Shury (Parks Canada), Dr. Geoff Skinner (Parks Canada), Dr. Asa Fahlman, Dr. Rob McCorkell (U Calgary), Dr. Bryan Macbeth, Mark Benson, Eric Knight, and Dr. Owen Smith (U Calgary) gave their time, expert knowledge, and assistance during winter captures. For guidance in dog training and for providing our project with great handlers and dogs, our appreciation goes to Julie Ubigau, Caleb Stanek, and Heath Smith from Conservation Canines. We also thank local residents, Alberta Trapper Association of Sundre and Friends of the Eastern Slopes Association for their interest in the project. University of Alberta staff, volunteers, and interns assisted for various lengths of time, in various tasks surrounding the calf captures, monitoring, and logistics. -
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. -
88 Reasons to Love Alberta Parks
88 Reasons to Love Alberta Parks 1. Explore the night sky! Head to Miquelon Lake Provincial Park to get lost among the stars in the Beaver Hills Dark Sky Preserve. 2. Experience Cooking Lake-Blackfoot Provincial Recreation Area in the Beaver Hills UNESCO Biosphere Reserve. This unique 1600 square km reserve has natural habitats that support abundant wildlife, alongside agriculture and industry, on the doorstep of the major urban area of Edmonton. 3. Paddle the Red Deer River through the otherworldly shaped cliffs and badlands of Dry Island Buffalo Jump Provincial Park. 4. Wildlife viewing. Our parks are home to many wildlife species. We encourage you to actively discover, explore and experience nature and wildlife safely and respectfully. 5. Vibrant autumn colours paint our protected landscapes in the fall. Feel the crunch of fallen leaves underfoot and inhale the crisp woodland scented air on trails in many provincial parks and recreation areas. 6. Sunsets illuminating wetlands and lakes throughout our provincial parks system, like this one in Pierre Grey’s Lakes Provincial Park. 7. Meet passionate and dedicated Alberta Parks staff in a visitor center, around the campground, or out on the trails. Their enthusiasm and knowledge of our natural world combines adventure with learning to add value to your parks experiences!. 8. Get out in the crisp winter air in Cypress Hills Provincial Park where you can explore on snowshoe, cross-country ski or skating trails, or for those with a need for speed, try out the luge. 9. Devonshire Beach: the natural white sand beach at Lesser Slave Lake Provincial Park is consistently ranked as one of the top beaches in Canada! 10. -
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. -
Transfer to Highwood Pass / Ptarmigan
VBT Itinerary by VBT www.vbt.com Alberta: Banff National Park & the Canadian Rockies Bike Vacation + Air Package Witness the spectacular beauty of the wilderness up close on this dazzling ride through the Canadian Rockies. As you ride, you’ll revel in the views of rugged snow-capped peaks, crystal-clear lakes, and blossoming alpine meadows, keeping your eyes peeled for the elk, deer, mountain goats, and bighorn sheep which populate the area. Off the bike, you’ll have time to explore hiking trails leading to dramatic ridges past roaring waterfalls. Our carefully selected lodgings with hearty meals, including a traditional barbecue, ensure that your time off the bike will be just as memorable your cycling. As you experience the majesty of the Canadian wilderness with VBT, you’ll see why this vacation surpasses all other Banff bicycle tours. Cultural Highlights Learn about Banff National Park, part of a UNESCO World Heritage site and Canada’s first 1 / 8 VBT Itinerary by VBT www.vbt.com national park. Explore Banff, the highest town in Canada, by foot and by bike. View the spectacular Victoria Glacier and the emerald waters of Lake Louise. Spin downhill along the magnificent Bow Valley Parkway, a stunning wilderness corridor. Cycle the Legacy Trail, with towering Mount Rundle, Cascade Mountain, and the Three Sisters Mountains surrounding you. Pause for a beer or soda, locally made in the Bow Valley. Pass panorama after panorama of jaw-dropping alpine splendor as you cycle in Kananaskis Country. Experience a traditional barbeque lunch at Boundary Ranch. Hike the trails of Ptarmigan Cirque to an alpine meadow with epic views. -
Historic Fire Regimes in the Kananaskis Valley 1916 Photo
Historic Fire Regimes in The Kananaskis Valley 1916 Photo 1890 fire burned over part of 1858 fire Talk Outline Special Thanks to MP Rogeau and Ric Arthur for Material used for this presentation Discuss people that have studied, observed, reported and influenced the Historic Fire Regimes in Southern Rockies A few definitions of fire terms Fire Evidence used Summarize fire ecology/history studies in Kananaskis Valley Fire Patterns Discuss the findings of fire cycles/return intervals and influences on those among researchers The fire behaviour and impact of the 1936 Galatea fire, the most recent large wildfire in the part of the valley were are located for this conference and salvage logging history. How fire history can be linked to surface woody fuel load Discuss the current landscape and how past fire’s influence Controversy over historic fire regimes and reasons for lack of fire Southern Rocky Mountain Wise Guy I can explain the meaning of life but have no idea what the historic fire regime is in the Kananaskis Valley and what influences it !!! Fire Ecologist Studying, Observing, Reporting and Influencing Historic Fire Regimes in Southern Rockies Pocaterra Palliser Rogeau Arthur Johnson/students Van Wagner The First Residents Landscape 100 yrs later White Rummel Hawkes E.A. Johnson, K. Miyanishi, G.I Fryer, C.P.S. Larson, W.J. Reed, M.P. Rogeau, S. Jevons, C.E. Van Wagner, B.C. Hawkes, S. Barrett, Photo credit: Ric Arthur C. White, M. Heathcott, and R. Arthur. Definitions • Fire Regime: type, frequency, size, seasonality, severity, spatial pattern, and cause • Mean Fire Return Interval: represents the average from all fire intervals calculated at each sampling site (stand level). -
Canadian Rockies Hiking Trail List
Canadian Rockies Hiking Trail List The following hiking trails are detailed in the Canadian Rockies Trail Guide: BANFF NATIONAL PARK Banff—Lake Minnewanka Sunshine Meadows 25. Sunshine Meadows Loop 1. C Level Cirque Trail 26. Quartz Hill—Citadel Pass Trail 2. Johnson Lake Trail 27. Simpson Pass—Healy Meadows Trail 3. Lake Minnewanka Trail 4. Alymer Lookout Trail Bow Valley Highline 5. Cascade Amphitheatre Trail 28. Healy Pass—Egypt Lake Trail 6. Elk Lake Trail 29. Egypt Lake via Pharaoh Creek Trail 7. Stoney Squaw Trail 30. Redearth Creek—Shadow Lake Trail 8. Fenland Trail 31. Twin Lakes Trail 9. Tunnel Mountain Trail 32. Arnica Lake—Twin Lakes Trail 10. Sulphur Mountain Trail 33. Bow Valley Highline Trail 11. Sundance Canyon Trail 34. Boom Lake Trail 12. Mount Rundle Trail 35. Smith Lake Trail 13. Spray River Circuit Trail 36. Taylor Lake Trail 14. Goat Creek Trail 15. Rundle Riverside Trail Lake Louise—Moraine Lake 37. Lake Louise Lakeshore Trail Bow Valley Parkway—Sawback Range 38. Fairview Lookout Trail 16. Cory Pass—Mt. Edith Trail 39. Lake Agnes Trail 17. Edith Pass via Forty Mile Creek Trail 40. Plain of the Six Glaciers Trail 18. Muleshoe Trail 41. Saddleback Trail 19. Johnston Canyon—Ink Pots Trail 42. Paradise Valley Loop 20. Sawback Trail 43. Larch Valley—Sentinel Pass Trail 21. Sawback Range Circuit 44. Eiffel Lake—Wenkchemna Pass Trail 22. Rockbound Lake Trail 45. Consolation Lakes Trail 23. Castle Lookout Trail 46. Moraine Lakeshore Trail 24. Bourgeau Lake Trail Boulder Pass—Skoki Valley 47. Boulder Pass—Skoki Valley Trail 48. -
Big Horn Sheep
2.11 SHEEP: Bighorn Sheep (Ovis canadensis, Ovis dalli: ssp: dalli, stonei) Appearance and Size California and Rocky Mountain bighorns look similar, but the California subspecies is slightly darker in colour, and in rams the horns flare outward more than those of Rocky Mountain (Photo: BC Parks) rams. Bighorn Sheep have a rich brown coat with a contrasting ivory–white rump patch, a white muzzle, and white trim on the back of all four legs. The brown coat fades to a drab grey-brown by late winter. The adult ram’s massive, brown, spiralled horns grow throughout the sheep’s life, and can be as long as 127 cm around the curve and as thick as 40 cm around the base. Ewes have slightly curved horns about 30 cm long. Adult rams stand about 100 cm high at the shoulder, and usually weigh 90 kg to 135 kg. Ewes are about two thirds the size of rams. (Photo: William S. Keller, US National Park Service) Life History Bighorn Sheep are among the most social of British Columbia’s hoofed mammals. They breed between early November and mid-December. Most ewes do not breed until they are two years old; and rams until they are seven or eight years old. Gestation lasts about 6 months, and lambs are born from the last week in April to early June. As lambing time nears, pregnant ewes leave their social group and isolate themselves in rugged lambing cliffs near the winter-spring range. They usually produce a single lamb that weighs 3 kg to 5 kg, but some well- nourished females produce occasional twins.