ICEFIELDS PARKWAY Driving Guide
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Road Biking Guide
SUGGESTED ITINERARIES QUICK TIP: Ride your bike before 10 a.m. and after 5 p.m. to avoid traffic congestion. ARK JASPER NATIONAL P SHORT RIDES HALF DAY PYRAMID LAKE (MAP A) - Take the beautiful ride THE FALLS LOOP (MAP A) - Head south on the ROAD BIKING to Pyramid Lake with stunning views of Pyramid famous Icefields Parkway. Take a right onto the Mountain at the top. Distance: 14 km return. 93A and head for Athabasca Falls. Loop back north GUIDE Elevation gain: 100 m. onto Highway 93 and enjoy the views back home. Distance: 63 km return. Elevation gain: 210 m. WHISTLERS ROAD (MAP A) - Work up a sweat with a short but swift 8 km climb up to the base MARMOT ROAD (MAP A) - Head south on the of the Jasper Skytram. Go for a ride up the tram famous Icefields Parkway, take a right onto 93A and or just turn back and go for a quick rip down to head uphill until you reach the Marmot Road. Take a town. Distance: 16.5 km return. right up this road to the base of the ski hill then turn Elevation gain: 210 m. back and enjoy the cruise home. Distance: 38 km. Elevation gain: 603 m. FULL DAY MALIGNE ROAD (MAP A) - From town, head east on Highway 16 for the Moberly Bridge, then follow the signs for Maligne Lake Road. Gear down and get ready to roll 32 km to spectacular Maligne Lake. Once at the top, take in the view and prepare to turn back and rip home. -
Herald / Harbinger the Pattern on the Plaza Maps the Movement of the Bow Glacier from the Wapta Icefield Down Toward Bow Lake
Ben Rubin and Jer Thorp Herald / Harbinger The pattern on the plaza maps the movement of the Bow Glacier from the Wapta Icefield down toward Bow Lake. LEDs, steel, granite, sound, sensors, software, electronics; 2017 Heralding the dawn of earth’s Anthropocene period, this artwork incorporates a collection of data feeds to illustrate the interrelationship between human activity in Calgary and the natural system of the Bow Glacier in the Canadian Rockies, which exists in a perpetual state of physical transformation. The artwork uses a specially constructed solar-powered seismic observatory near the glacier to monitor the Inside the lobby, the glacier’s real-time perturbations are rumblings, cracks and shifts of the moving ice. visually juxtaposed against the aggregated trajectories of The observatory continuously reports these movements via satellite to the artwork, where they are expressed as sound nearby pedestrians and vehicles in a sequence of overlapping and moving light. The glacier’s movements are rendered visualizations, while outside on the plaza the glacier’s visually as vertical displacements of horizontal scan lines, and also audibly here in the lobby and outside on the plaza. ceaseless activity is made audible, creating a visceral public presence for this restless complex of ice, rock, and water. www.artsbrookfield.com/art_collection/herald-harbinger BOW GLACIER Pedestrian traffic on the outdoor plaza is monitored using BANFF NATIONAL PARK cameras. The movements of individuals are aggregated over the course of each day and rendered as directional symbols. BOW RIVER CALGARY TO HUDSON BAY The artwork tracks average inbound and outbound vehicular traffic in real time at 14 locations around Calgary. -
Day Hiking Lake Louise, Castle Junction and Icefields Parkway Areas
CASTLE JUNCTION AREA ICEFIELDS PARKWAY AREA LAKE LOUISE AREA PLAN AHEAD AND PREPARE Remember, you are responsible for your own safety. 1 7 14 Castle Lookout Bow Summit Lookout Wilcox Pass MORAINE LAKE AREA • Get advice from a Parks Canada Visitor Centre. Day Hiking 3.7 km one way; 520 m elevation gain; 3 to 4 hour round trip 2.9 km one way; 245 m elevation gain; 2.5 hour round trip 4 km one way; 335 m elevation gain; 3 to 3.5 hour round trip • Study trail descriptions and maps before starting. Trailhead: 5 km west of Castle Junction on the Bow Valley Parkway Trailhead: Highway 93 North, 40 km north of the Lake Louise junction, Trailhead: Highway 93 North, 47 km north of Saskatchewan Crossing, • Check the weather forecast and current trail conditions. (Highway 1A). at the Peyto Lake parking lot. or 3 km south of the Icefield Centre at the entrance to the Wilcox Creek Trailheads: drive 14 km from Lake Louise along the Moraine Lake Road. • Choose a trail suitable for the least experienced member in Lake Louise, Castle Junction campground in Jasper National Park. Consolation Lake Trailhead: start at the bridge near the Rockpile at your group. In the mid-20th century, Banff erected numerous fire towers From the highest point on the Icefields Parkway (2070 m), Moraine Lake. Pack adequate food, water, clothing, maps and gear. and Icefields Parkway Areas where spotters could detect flames from afar. The Castle Lookout hike beyond the Peyto Lake Viewpoint on the upper self-guided • Rise quickly above treeline to the expansive meadows of this All other trails: begin just beyond the Moraine Lake Lodge Carry a first aid kit and bear spray. -
NB4 - Rivers, Creeks and Streams Waterbody Waterbody Detail Season Bait WALL NRPK YLPR LKWH BURB GOLD MNWH L = Bait Allowed Athabasca River Mainstem OPEN APR
Legend: As examples, ‘3 over 63 cm’ indicates a possession and size limit of ‘3 fish each over 63 cm’ or ‘10 fish’ indicates a possession limit of 10 for that species of any size. An empty cell indicates the species is not likely present at that waterbody; however, if caught the default regulations for the Watershed Unit apply. SHL=Special Harvest Licence, BKTR = Brook Trout, BNTR=Brown Trout, BURB = Burbot, CISC = Cisco, CTTR = Cutthroat Trout, DLVR = Dolly Varden, GOLD = Goldeye, LKTR = Lake Trout, LKWH = Lake Whitefish, MNWH = Mountain Whitefish, NRPK = Northern Pike, RNTR = Rainbow Trout, SAUG = Sauger, TGTR = Tiger Trout, WALL = Walleye, YLPR = Yellow Perch. Regulation changes are highlighted blue. Waterbodies closed to angling are highlighted grey. NB4 - Rivers, Creeks and Streams Waterbody Waterbody Detail Season Bait WALL NRPK YLPR LKWH BURB GOLD MNWH l = Bait allowed Athabasca River Mainstem OPEN APR. 1 to MAY 31 l 0 fish 3 over 63 cm 10 fish 10 fish 5 over 30 cm Mainstem OPEN JUNE 1 to MAR. 31 l 3 over 3 over 63 cm 10 fish 10 fish 5 over 43 cm 30 cm Tributaries except Clearwater and Hangingstone rivers OPEN JUNE 1 to OCT. 31 l 3 over 3 over 63 cm 10 fish 10 fish 10 fish 5 over 43 cm 30 cm Birch Creek Beyond 10 km of Christina Lake OPEN JUNE 1 to OCT. 31 l 0 fish 3 over 63 cm Christina Lake Tributaries and Includes all tributaries and outflows within 10km of OPEN JUNE 1 to OCT. 31 l 0 fish 0 fish 15 fish 10 fish 10 fish Outflows Christina Lake including Jackfish River, Birch, Sunday and Monday Creeks Clearwater River Snye Channel OPEN JUNE 1 to OCT. -
CANADA's MOUNTAIN Rocky Mountain Goats
CANADA'S MOUNTAIN Rocky Mountain Goats CANADA'S MOUNTAIN PLAYGROUNDS BANFF • JASPER • WATERTON LAKES • YOHO KOOTENAY ° GLACIER • MOUNT REVELSTOKE The National Parks of Canada ANADA'S NATIONAL PARKS are areas The National Parks of Canada may, for C of outstanding beauty and interest that purposes of description, be grouped in three have been set apart by the Federal Govern main divisions—the scenic and recreational ment for public use. They were established parks in the mountains of Western Canada; the to maintain the primitive beauty of the land scenic, recreational, wild animals, and historic scape, to conserve the native wildlife of the parks of the Prairie Provinces; and the scenic, country, and to preserve sites of national his recreational, and historic parks of Eastern Can toric interest. As recreational areas they pro ada. In these pages will be found descriptions vide ideal surroundings for the enjoyment of of the national parks in the first group—areas outdoor life, and now rank among Canada's which lie within the great mountain regions outstanding tourist attractions. of Alberta and British Columbia. Canada's National Park system teas estab * * * lished in 1SS5, when a small area surrounding mineral hot springs at Banff in the Rocky This publication is compiled in co-operation Mountains was reserved as a public posses with the National Parks Branch, Department sion. From this beginning has been developed of Northern Affairs and National Resources. the great chain of national playgrounds note Additional information concerning these parks stretching across Canada from the Selkirk may be obtained from the Park Superintend Mountains in British Columbia to the Atlantic ents, or from the Canadian Government Travel Coast of Nova Scotia. -
Highway 3: Transportation Mitigation for Wildlife and Connectivity in the Crown of the Continent Ecosystem
Highway 3: Transportation Mitigation for Wildlife and Connectivity May 2010 Prepared with the: support of: Galvin Family Fund Kayak Foundation HIGHWAY 3: TRANSPORTATION MITIGATION FOR WILDLIFE AND CONNECTIVITY IN THE CROWN OF THE CONTINENT ECOSYSTEM Final Report May 2010 Prepared by: Anthony Clevenger, PhD Western Transportation Institute, Montana State University Clayton Apps, PhD, Aspen Wildlife Research Tracy Lee, MSc, Miistakis Institute, University of Calgary Mike Quinn, PhD, Miistakis Institute, University of Calgary Dale Paton, Graduate Student, University of Calgary Dave Poulton, LLB, LLM, Yellowstone to Yukon Conservation Initiative Robert Ament, M Sc, Western Transportation Institute, Montana State University TABLE OF CONTENTS List of Tables .....................................................................................................................................................iv List of Figures.....................................................................................................................................................v Executive Summary .........................................................................................................................................vi Introduction........................................................................................................................................................1 Background........................................................................................................................................................3 -
Experience the Icefields Parkway in Winter
EXPLORE! LOOKING FOR ADVENTURE? MORE INFORMATION Winter transforms the Icefields Parkway, one of the world’s most scenic drives. Ancient glaciers glow JASPER INFORMATION CENTRE: 780-852-6176 winter white under blankets of fresh snow. Quiet descends, broken only by far off sounds of ice crevasses growling as LAKE LOUISE VISITOR CENTRE: 403-522-3833 they grow. Snow-covered trails entice drivers to pull over, don snowshoes and break trail below some of the highest VALLEY OF THE FIVE LAKES MODERATE – SNOWSHOES BANFF VISITOR CENTRE: 403-762-1550 mountains in the Canadian Rockies. EXPERIENCE THE 4.5 km loop/2 hrs; 66 m elevation gain/loss pc.gc.ca/jasper Trailhead: 9 km south of Jasper, 224 km north of pc.gc.ca/banff Lake Louise ICEFIELDS LOOKING FOR A QUICK AND WANT TO STRETCH Five small, picturesque lakes in a sunny valley are CHECK THE ROAD CONDITIONS AND THE WEATHER Athabasca Glacier PARKWAY SCENIC STOP? YOUR LEGS? the highlights of this outing, a local family favourite. FORECAST BEFORE YOU LEAVE TOWN: TANGLE FALLS NIGEL PASS ROAD CONDITIONS: Call 511 • alberta511.ca IN WINTER WANT TO STRAP ON MODERATE – SNOWSHOES OR BACKCOUNTRY SKIS Trailhead: 96 km south of Jasper, 137 km north of ATHABASCA FALLS WEATHER FORECAST 14 km/5-6 hrs return; 385 m elevation gain Lake Louise EASY – WEAR STURDY BOOTS SNOWSHOES OR SKIS? Banff 403-762-2088 • Jasper 780-852-3185 This beautiful, cascading icefall right beside the road 1 km/30 mins return; no elevation gain/loss Trailhead: 116 km south of Jasper, 117 km north of weather.gc.ca • Visit an information centre Trailhead: 30 km south of Jasper, 203 km north of makes for a great photo stop. -
Canadian Rockies
CANADIAN ROCKIES Banff-Lake Louise-Vancouver-Victoria September 3-11, 2014 INCLUDED IN YOUR TOUR: 4-Seasons Vacations Tour Director, Larry Alvey Tours of Calgary, Moraine Lake, Lake Louise, DELTA Airlines flights, Minneapolis to Calgary, Banff, Banff Mountain Gondola, Vancouver return Vancouver to Minneapolis Two day Daylight Rail, Banff to Vancouver, rail 8 Nights Hotel Accommodations gratuities included for Red, Silver and Gold Leaf 8 Meals: 5 breakfasts, 3 lunches, includes lunch Service at Chateau Lake Louise Baggage handling at hotels (1 bag per person) Deluxe motor coach in Canada All taxes DAY 1 WEDNESDAY Depart via Delta Airlines for Calgary, site of the famous Calgary Stampede. Our 1/2 day tour of this vibrant city includes the Olympic Park (site of the 1988 Winter Olympics) and the Stampede Grounds. DELTA BOW VALLEY DAY 2 THURSDAY (B) Our destination today is Banff, an alpine community nestled in the Rocky Mountains, a world famous resort. Tall peaks, wooded valleys, crystal-clear waters and canyons are all preserved in natural magnificence. Upon arrival in Banff, we tour lovely Bow Falls, Cascade Park, then ride the Banff Gondola to a mountain top for an unobstructed 360 degree view of the Banff town site. Our deluxe hotel is situated in the heart of Banff, providing ample opportunity to stroll the colorful streets of this quaint village. BANFF PARK LODGE (3 NIGHTS) DAY 3 FRIDAY (B, L) A wonderful day of sightseeing is in store for you today. We will visit beautiful Moraine Lake and the Valley of the Ten Peaks. Enjoy a lunch at Chateau Lake Louise. -
Fisheries Barriers in Native Trout Drainages
Alberta Conservation Association 2018/19 Project Summary Report Project Name: Fisheries Barriers in Native Trout Drainages Fisheries Program Manager: Peter Aku Project Leader: Scott Seward Primary ACA Staff on Project: Jason Blackburn, David Jackson, and Scott Seward Partnerships Alberta Environment and Parks Environment and Climate Change Canada Key Findings • We compiled existing barrier location information within the Peace River, Athabasca River, North Saskatchewan River, and Red Deer River basins into a centralized database. • We catalogued fish habitat and community data for the Narraway River watershed for use in a population restoration feasibility framework. • We identified 107 potential barrier locations within the Narraway River watershed, using Google Earth ©, which will be refined using valley confinement modeling and validated with ground truthing in 2019. Introduction Invasive species pose one of the greatest threats to Alberta native trout species, through hybridization, competition, and displacement. These threats are partially mediated by the presence of natural headwater fish-passage barriers, namely waterfalls, that impede upstream 1 invasions. In Alberta, several sub-populations of native trout remain genetically pure primarily because of waterfalls. Identification and inventory of waterfalls in the Peace River, Athabasca River, North Saskatchewan River, and Red Deer River basins isolating pure populations and their habitats is critical to inform population recovery and build implementation strategies on a stream by stream basis. For example, historical stocking of non-native trout to the Narraway River watershed may be endangering native bull trout and Arctic grayling. Non-native cutthroat trout, rainbow trout, and brook trout have been stocked in the Torrens River, Stetson Creek, and Two Lakes, all of which have connectivity to the Narraway River. -
PEG Magazine
SUMMER 2016 Dr. Steve E. Hrudey, P.Eng. APEGA's 97th President The Association of Professional apega.ca Engineers and Geoscientists of Alberta | WE SPECIALIZE IN SIMPLE, COST-EFFECTIVE AND RELIABLE FACILITY DESIGNS. Gold-plated designs are out of place under any market conditions. That’s why we focus on JVZ[LɈLJ[P]LLUNPULLYPUN[OH[ZPTWSPÄLZMHJPSP[`VWLYH[PVUZHUKTHPU[LUHUJL>LZ[YLHTSPUL LX\PWTLU[HUKKLZPNUZWLJPÄJH[PVUZ[VYLTV]LJVZ[S`V]LYKLZPNUHUKTPUPTPaLJVTWSL_P[` Put our experience to work for your project. Learn more at vistaprojects.com Contents PEG FEATURED PHOTO: SUMMER 2016 PAGE 10›› 34 52 68 FEATURES DEPARTMENTS 8 & 9 New Council, Summit Recipients 4 President's Notebook 65 Viewfinder 10 Meet the President 6 Interim CEO’s Message 72 AEF Campaign Connection 15 Council Nominations Begin 20 Movers & Shakers 75 Focal Point 40 What’s Next in Legislative Review? 34 Professional Development 82 Member Benefits 49 All About apega.ca 52 Good Works 84 Record 68 Science Plus Youth Equals This 60 And You Are COVER PHOTO: Kurtis Kristianson, Spindrift Photography PRINTED IN CANADA SUMMER 2016 PEG | 1 US POSTMASTER: PEG (ISSN 1923-0044) is published quarterly in Spring, Summer, Fall and Winter, by the Association of Professional Engineers and Geoscientists of Alberta, c/o US Agent-Transborder Mail 4708 Caldwell Rd E, Edgewood, WA 98372-9221. $15 of the annual membership dues applies to the yearly subscription of The PEG. Periodicals postage paid at Puyallup, WA, and at additional mailing offices. US POSTMASTER, send address changes to PEG c/o Transborder Mail, PO Box 6016, Federal Way, WA 98063-6016, USA. -
Glacier Fluctuations in the Canadian Rockies
GLACIER FLUCTUATIONS IN THE CANADIAN ROCKIES Calvin J. HEUSSER Department of Exploration ann Field Hesl'an'h .\Ilh'ri{'H II (;t'ographi{'al Soeiel:-" :\"t' W York. :\"t>w York Synopsis Through the use of survey and botanieal teehniques. reeent gladPI' fluctuations ill the Canadian Ho(:kies were measured and dated. Twelve gladers in nritish Columbia Hn<1 Alberta were studied between the )Iount Hobson area in the northwest and the vicinity of Kicking Horse Pass in the southeast. Two of them. Rob~ol\ and Yoho (;laeiers. are on the western slopes; ten, Angel, Columbia, Dome, Atha basku, unnamed at the head of Hilda Creek, Saskatchewan, Southeast LyeJJ , Fresh field, Peyto, and How Glaeiers drain on the east. Some of these flow from the salll(, i(,e field: ::<onw from independent nev<'~s, a])(1 some are merely hanging iee masses. (;laeier advun(,es arc dated from iee-tilted trees. glaeier retreat from the age of trees that have beeOlne established on reeessional'moraines. Re(,ords of this study show that glaeiers attained maxima and receded between the late seventeenth and late nineteenth eenturies. Bow Glaeier reeeded as e~lI'ly as lG7H; six glaciers receded frolll maxima in the eighteenth century and five withdrew during t.he nineteenth eentury. These data eompare with results of similar studies elsewhere in British Columbia, in Oregon, and in Alaska. Ko evidence of major twentieth ('entur~' ad Vt\lH'P was oiJservpd as is known for certain ('oastal Aluskan glaciers. Introduction Thb paper constitutes a report or the 19,,8 field work on twelve gill<'iers draining the northeast and southwest slopes of the Hocky Mountains in Alberta a.nd British Columhia, Dominion of Canada. -
Persistence of Branchinecta Paludosa (Anostraca) in Southern Wyoming, with Notes on Zoogeography
This file was created by scanning the printed publication. Errors identified by the software have been corrected; however, some errors may remain. JOURNAL OF CRUSTACEAN BIOLOGY, 13(1): 184-189, 1993 PERSISTENCE OF BRANCHINECTA PALUDOSA (ANOSTRACA) IN SOUTHERN WYOMING, WITH NOTES ON ZOOGEOGRAPHY James F. Saunders III, Denton Belk, and Richard Dufford ABSTRACT The fairy shrimp Branchinectapaludosa is a persistentresident of aestival ponds at high elevation in the Medicine Bow Mountains of southernWyoming. These populationsare far removed from the Arctic tundrahabitat that typifiesthe distributionof the species, and appear to representthe southern margin of the range in North America. All of the records for the northernUnited States and southernCanada appear to lie along the CentralFlyway that is a major migrationroute for waterfowland shorebirdsthat nest in the Arctic. Passive dispersal probablyprovides for frequentcolonization of marginalhabitats and gene flow to established populations. The fairy shrimp Branchinectapaludosa have been deposited in the University of (Muller)is widely distributedin the circum- Colorado Museum (UCM 2192, 2193, polar tundra of the Holarctic region (Vek- 2194). The Snowy Range is an axial rem- hoff, 1990). In Europe, it occurs chiefly at nant which rises about 300 m above the latitudes above 60?N, but there are isolated surrounding Medicine Bow Mountains recordsfrom the High Tatra Mountains on (Houston and others, 1978). The ponds are the borderbetween Czechoslovakiaand Po- mainly in the upperTelephone Creek drain- land at about 49?N (Brtek, 1976). Records age at elevations of 3,200-3,350 m. Most for Russia are typically along the Arctic of the ponds are underlainby the Nash Fork margin, but include the southern tip of the formation (Houston and others, 1978), and Kamchatka Peninsula at 52?N (Linder, the characteristicmetadolomite is present 1932).