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526:(3,258 ft) to the cliff bank on the first peak and 1,579 metres (5,180 ft) to the summit. Although it is called non-technical, it is considered gruelling by some. About halfway up there is a Central Gully, a huge watercourse with a well-worn path which is a dead end. Cliffs become higher and more vertical and there is no scrambling route. The real route crosses the watercourse and then immediately turns left (watch for markings). As one passes the treeline, the hiker ventures onto a feature called the "Dragon's back", where the route narrows between two steep gullies. The only real obstacle at this point is perseverance at the tread-mill like scree which slows progress to a two steps forward, one step back pattern.
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the curiously shaped wooden ships that they arrived in. We called their square-shaped homes "waskahigan", which literally means "the structure you enclose yourself in". When they were not satisfied with one enclosure they made another one around the first, which they called a "stockade". Over time, we learned to appreciate the lifestyle they introduced to us. Today, most, if not all Crees, live in these "waskahigan" style dwellings...It was only some forty or so years ago that our people began moving into these waskahigan.
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545:(1884–1963) described Mount Rundle as his, "bread and butter mountain. I never tire of painting it, for it is never the same. In deep shadow in the morning, it borrows a warm glow from the setting sun at the end of the day. Its colour runs the gamut from orange to cold blue-grey, with overtones of violet and intervals of green."
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Mount Rundle illustrates the classic limestone-shale-limestone "sandwich" of the front ranges. The basal "slice of bread" is the lower massive cliffs of tough grey
Pallister Formation limestones and dolomites. The "sandwich filling" is the Banff Formation, a layer of softer, more easily eroded, dark
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When
Europeans first came to our homeland we remarked that these people did not appear to be enthusiasts of the outdoors. They closed themselves in box-shaped structures and did whatever work (and play) they did inside. We called the Europeans wemstigooshewich or the "shaped wood people", recalling
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The complete traverse from Banff to
Canmore (staying always on the ridge) of the integral ridge was done "solo" in 1976 by the late Jean-Pierre Cadot. It required one bivouac, much scrambling, easy fifth-class rock climbing and one section was very involved and required lay-backing the ridge with a
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limestone. The top layer of the geologic sandwich is the grey limestones and dolomites of the Rundle Group that form the massive upper cliffs at the top of Mount Rundle. Between the
Palliser and the Banff lie the thin, recessive shales of the Exshaw Formation (the "lettuce leaf" of the sandwich),
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trailhead for the first peak taking the Mount Rundle Trail, is near the Spray River bridge on the road to the Banff
Springs Golf Course. The all-day hike (from 8–10 hours) from the trailhead to the peak is about 5 kilometres (3.1 mi) one-way and has an elevation gain of about 993 metres
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At the EEOR near
Canmore there is a well-known scramble, the Goat Creek hiking trail, with its starting point at parking trailhead, which starts at the Smith-Dorrien/Spray Trail just south of the Canmore Reservoir above
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about 2 million years ago with the sculpting and gouging of the
Canadian Rockies by glaciers, and then by streams and rivers. Finally, after the glaciers retreated for the last time, a series of steep, tree-covered
514:. This is also the beginning of the Mount Rundle Traverse, a demanding trek to mount all of Rundle's peaks from Goat Creek parking lot to the Banff Springs Hotel. Mount Rundle is one of the most popular
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The viewpoint from which most photographs are taken, 5 kilometres (3.1 mi) from Mount Rundle, at the end of
Vermilion Lakes road, with Vermillion Lakes in the foreground.
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eastward from Banff to
Canmore with seven distinct peaks along the way. The third peak southeast of Banff is the highest at 9,675 feet (2,949 m). West of the
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312:— locally known as EEOR—which rises above Whiteman's Gap just south of Canmore. The Rundle Peaks are part of the South Banff Ranges, along with its siblings—the
443:. Geologists consider Mount Rundle to be a classic example of a mountain cut in dipping layered rocks, with the tilted strata giving the mountain its shape.
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high degree of exposure. A long rappel was necessary to overcome a very steep section and it is most likely that the rappel station is still in place.
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Mt. Rundle could actually be considered a small mountain range as the mountain extends for over 12 kilometres (7.5 mi), on the south side of the
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In 2000 Dave
Birrell described Mount Rundle as one of the most recognized Canadian mountains. Painter, print-maker and art teacher,
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on the north side of the Trans-Canada. The Banff Fairmont hotel patio and restaurants look out over Mount Rundle and
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the supervisor of the Wesleyan missionaries in Rupert's Land who is credited with devising the Cree syllabics
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to become detached and slide eastward to northeastward over their neighbors, piling up to form the southern
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there—a written language developed for the Cree, as part of his missionary work. He only visited the
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Walter Phillips played an important role in the development of their visual arts program at the
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steeply to the southwest, so that the southwest-facing side of the mountain forms an extensive
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began to grow at the mouths of the deep gulches on the northeast-facing side of the mountain.
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in Calgary, Alberta holds an extensive collection of Phillips works and a research archive.
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for landscaping and building purposes. It has been used in the construction of the
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between late Jurassic and early Cretaceous time. At that time a collision of
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buildings. It is fine-grained sandstone dating back to the Triassic Period.
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in the area, and is relatively straightforward for experienced hikers.
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of the area around what is now called Mount Rundle in 1844 and 1847.
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The most recent stage in the history of Mount Rundle began in the
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Alberta Oil Magazine: the oil and gas publication of Canada
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838:. Volume XII (1891–1900). Dictionary of Canadian Biography
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415:) that underlie Canmore and the forested slopes along the
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caused huge sheets of sedimentary rock in what is now
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The northeast-facing side of the mountain, seen from
419:. The thrust faulting occurred during the Columbian
719:, then known as the Banff School of Fine Arts. Its
618:Mount Rundle and Sulphur Mountain can be seen from
469:. All the peaks seen here are part of Mount Rundle.
289:work in western Canada in the 1840s. He introduced
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1866:Canadian Rocky Mountain Parks World Heritage Site
1038:"Canadian Society of Petroleum Geologists Poster"
435:. This left the Paleozoic strata on Mount Rundle
404:that was moved up from the west along the Rundle
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1047:, Canadian Society of Petroleum Geologists, 2007
669:. The Grand Council of the Crees. Archived from
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400:The Paleozoic "sandwich" is part of the Rundle
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408:and emplaced on top of the younger rocks (the
368:) age. In ascending order, they belong to the
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1120:50 Roadside Panoramas in the Canadian Rockies
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1067:"At Kamenka Quarry, every stone has a story"
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663:"At the Conference on Construction Val d'Or"
661:Grand Chief Matthew Mukash (12 March 2009).
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2364:Alberta–British Columbia foothills forests
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1143:East End Rundle Trail from HikeAlberta.com
336:East aspect of Mount Rundle showing summit
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1876:Waterton-Glacier International Peace Park
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699:pronounced Eeyore, like the character in
634:Mount Rundle is depicted on the cover of
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1823:Category:Rivers of the Canadian Rockies
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16:Mountain in Banff National Park, Canada
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1818:List of rivers of the Canadian Rockies
1006:"The Formation of the Rocky Mountains"
878:
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384:, which was named after the mountain.
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832:"Biography – RUNDLE, ROBERT TERRILL"
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1985:Sulphur Mountain Cosmic Ray Station
955:Canadian Rockies Geology Road Trips
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922:Lexicon of Canadian Geologic Units
886:Lexicon of Canadian Geologic Units
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957:, Corax Press, pp. 118–119,
185:(South Banff Ranges/Rundle Peaks)
2411:Mountains of Banff National Park
1990:First Oil Well in Western Canada
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397:covered with debris from above.
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1065:Foubert, Tanya (Jan 13, 2006).
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1930:Jasper Park Information Centre
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583:Mount Rundle reflected in the
1:
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2369:North Central Rockies forest
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62:1,304 m (4,278 ft)
52:2,948 m (9,672 ft)
7:
2095:Dune Za Keyih (Frog-Gataga)
1584:Unnamed Alberta–BC mountain
598:Mount Rundle seen from the
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273:renamed the mountain after
269:or house mountain. In 1858
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2416:Two-thousanders of Alberta
1871:Waterton Biosphere Reserve
1122:, Rocky Mountain Books Ltd
727:, is named after him. The
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33:Mount Rundle as seen from
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253:overlooking the towns of
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2359:Alberta Mountain forests
2160:Northern Rocky Mountains
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613:Mount Rundle, south face
392:shale with thin beds of
1970:Abbot Pass Refuge Cabin
1587:(formerly Mount Pétain)
816:Rundle, Robert (1977),
721:Walter Phillips Gallery
568:Mount Rundle seen from
413:Mist Mountain Formation
388:brownish-gray to black
2324:Ecozone and ecoregions
1118:Birrell, Dave (2000),
1071:Rocky Mountain Outlook
924:, 1953, archived from
762:cdnrockiesdatabases.ca
470:
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275:Reverend Robert Rundle
115:
90:51.12417°N 115.47028°W
2115:Height of the Rockies
917:Livingstone Formation
673:on 28 February 2017.
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335:
218:1888 by J.J. McArthur
1965:Twin Falls Tea House
1012:, nd, archived from
549:From Vermilion Lakes
302:Trans-Canada Highway
283:Hudson's Bay Company
95:51.12417; -115.47028
1010:Mountains in Nature
896:on 22 February 2013
820:, Glenbow Institute
818:The Rundle Journals
723:, which focuses on
497:and several of the
495:Banff Springs Hotel
251:Banff National Park
86: /
2344:Montane Cordillera
1955:Kicking Horse Pass
1369:Continental Ranges
953:Gadd, Ben (2008),
630:In popular culture
471:
338:
310:East End of Rundle
42:Highest point
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2339:Boreal Cordillera
2209:Fortress Mountain
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2140:Mount Assiniboine
2090:Close To The Edge
2085:Akamina-Kishinena
1980:Banff Park Museum
1768:Columbia Icefield
1363:Winston Churchill
994:on 19 March 2017.
964:978-0-9692631-2-8
641:Get What You Give
557:Scenic viewpoints
534:Scenic viewpoints
489:used in southern
267:Waskahigan Watchi
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116:Waskahigan Watchi
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2385:Geography portal
2244:Sunshine Village
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2120:Hole-in-the-Wall
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1803:Waputik Icefield
1687:North Kananaskis
1179:Canadian Rockies
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433:Canadian Rockies
429:British Columbia
410:Early Cretaceous
380:, topped by the
378:Banff Formations
318:Sulphur Mountain
259:Canmore, Alberta
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1999:Provincial (AB)
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1960:Skoki Ski Lodge
1935:Yellowhead Pass
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1016:on 23 July 2014
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1131:External links
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1092:"Mount Rundle"
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938:
928:on 7 July 2012
907:
890:"Rundle Group"
877:
865:Peakbagger.com
861:"Rundle Peaks"
849:
823:
808:
792:"Mount Rundle"
774:
758:"Mount Rundle"
743:
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729:Glenbow Museum
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2130:Kikomun Creek
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363:
362:Late Devonian
359:
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271:John Palliser
268:
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225:Easiest route
221:
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20:
2224:Marmot Basin
2175:
2150:Mount Robson
2145:Mount Fernie
2049:Spray Valley
1925:Jasper House
1821:
1788:Saskatchewan
1582:
1548:Stanley Peak
1533:Saskatchewan
1522:
1458:Edith Cavell
1374:
1367:
1328:South Jasper
1138:Mount Rundle
1136:Peakbagger.
1119:
1099:, retrieved
1095:
1086:
1076:February 18,
1074:. Retrieved
1070:
1060:
1049:, retrieved
1044:
1018:, retrieved
1014:the original
1009:
1000:
989:the original
984:
978:"Formations"
972:
954:
930:, retrieved
926:the original
916:
910:
898:. Retrieved
894:the original
880:
868:. Retrieved
864:
842:11 September
840:. Retrieved
836:biographi.ca
835:
826:
817:
811:
799:. Retrieved
795:
767:11 September
765:. Retrieved
761:
717:Banff Centre
711:
695:
683:
674:
671:the original
666:
656:
639:
633:
617:
552:
537:
528:
520:
512:Grassi Lakes
508:
499:Parks Canada
483:Rundle stone
482:
478:
477:
445:
406:thrust fault
402:thrust sheet
399:
394:argillaceous
386:
382:Rundle Group
348:limestones,
339:
308:road is the
299:
266:
239:Mount Rundle
238:
237:
214:First ascent
177:Parent range
156:Mount Rundle
22:Mount Rundle
2295:Lake Louise
2253:Communities
2239:Powder King
2214:Lake Louise
2192:Ski resorts
2155:Muncho Lake
2069:Frank Slide
2039:Sheep River
2024:Ghost River
2019:Elbow-Sheep
2014:Bragg Creek
1513:Resplendent
1438:Castleguard
1408:Assiniboine
1376:Hart Ranges
1258:Livingstone
985:calfrac.com
796:Bivouac.com
688:James Evans
523:Spray River
479:Rundle rock
448:Pleistocene
306:Spray Lakes
111:Native name
93: /
81:115°28′13″W
68:Coordinates
2405:Categories
2353:ecoregions
2219:Little Mac
2054:White Goat
2029:Kananaskis
2009:Bow Valley
1945:Howse Pass
1742:Yellowhead
1667:Kananaskis
1443:Clemenceau
1253:Kananaskis
1203:Beaverfoot
1101:29 January
1096:Trail Peak
1051:30 January
1020:29 January
932:29 January
900:29 January
870:29 January
801:29 January
739:References
600:Bow Valley
390:calcareous
342:limestones
322:Goat Range
287:missionary
78:51°07′27″N
58:Prominence
2310:Valemount
2100:Elk Lakes
1758:Athabasca
1737:White Man
1727:Vermilion
1627:Crowsnest
1612:Athabasca
1543:Snow Dome
1488:Kitchener
1413:Athabasca
1403:Andromeda
1391:Mountains
1348:Vermilion
1293:President
1283:Morrissey
1248:High Rock
1243:Foothills
1228:Fairholme
1218:Crowsnest
638:'s album
516:scrambles
505:Scrambles
441:dip slope
417:Bow River
358:Paleozoic
350:dolomites
346:dolomitic
291:syllabics
279:Methodist
265:name was
131:Geography
48:Elevation
2381:See also
2333:ecozones
2300:Sparwood
2135:Kwadacha
2059:Willmore
2044:Siffleur
1905:Kootenay
1885:National
1773:Crowfoot
1751:Glaciers
1717:Sunwapta
1707:Sinclair
1692:Palliser
1652:Highwood
1642:Fortress
1622:Carcajou
1478:Hungabee
1448:Columbia
1338:Terminal
1333:Sundance
1318:Sentinel
1288:Palliser
1238:Flathead
474:Commerce
370:Palliser
320:and the
243:mountain
231:Scramble
208:Climbing
191:Topo map
165:, Canada
2275:Elkford
2265:Canmore
2234:Nakiska
1831:Peoples
1793:Vulture
1722:Tonquin
1702:Simpson
1677:Monkman
1591:Whymper
1578:Ulysses
1568:Trinity
1553:Sulphur
1528:Sarbach
1508:Pyramid
1428:Cascade
1418:Brazeau
1398:Alberta
1358:Waputik
1313:Sawback
1303:Rainbow
1273:Massive
1268:Maligne
701:Milne's
491:Alberta
467:Canmore
437:dipping
421:Orogeny
328:Geology
202:Canmore
163:Alberta
2290:Jasper
2280:Fernie
2204:Fernie
2110:Hamber
1900:Jasper
1812:Rivers
1778:Hector
1732:Wapiti
1712:Summit
1682:Muncho
1662:Jarvis
1647:Fraser
1600:Passes
1558:Temple
1538:Smythe
1523:Rundle
1518:Robson
1483:Joffre
1473:Hosmer
1468:Hector
1463:Forbes
1433:Castle
1263:Lizard
1233:Fiddle
1186:Ranges
961:
706:series
667:gcc.ca
374:Exshaw
354:shales
285:to do
261:. The
247:Canada
119:
106:Naming
2285:Field
2260:Banff
2125:Kakwa
2005:Parks
1895:Banff
1891:Parks
1798:Wapta
1783:Peyto
1657:Howse
1632:Elbow
1607:Abbot
1503:Pilot
1498:Heart
1493:Lyell
1423:Bryce
1323:Slate
1278:Misty
1041:(PDF)
992:(PDF)
981:(PDF)
648:Notes
451:epoch
255:Banff
241:is a
1910:Yoho
1820:and
1816:see
1697:Pine
1617:Bush
1573:Twin
1453:Cory
1208:Blue
1198:Bare
1193:Ball
1103:2014
1078:2018
1053:2014
1022:2014
959:ISBN
934:2014
902:2014
872:2014
844:2019
803:2014
769:2019
376:and
352:and
277:, a
263:Cree
257:and
199:82O3
123:Cree
2351:WWF
2331:CEC
1763:Bow
1637:Elk
1308:Ram
1223:Elk
1213:Bow
543:RCA
481:or
364:to
356:of
249:'s
245:in
196:NTS
2407::
1110:^
1094:,
1069:.
1043:,
1029:^
1008:,
983:.
941:^
920:,
888:.
863:.
852:^
834:.
794:.
777:^
760:.
747:^
665:.
644:.
626:.
372:,
344:,
324:.
316:,
1171:e
1164:t
1157:v
1080:.
904:.
874:.
846:.
805:.
771:.
360:(
125:)
121:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
