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Top Attractions in Banff National Park

Lake Louise

Lake Louise is a hamlet in Alberta, Canada within Improvement District No. 9 Banff . The hamlet is named for the nearby Lake Louise, which in turn was named after the Princess Louise Caroline Alberta , the fourth daughter of Queen Victoria, and the wife of John Campbell, the 9th Duke of Argyll, who was the Governor General of Canada from 1878 to 1883. The hamlet was originally called Laggan, and was a station along the Canadian Pacific Railway route. It was built in 1890. The rail station building was preserved and moved into Heritage Park in Calgary. The hamlet is separated into two communities. The main community, referred to as The Village is at a lower elevation adjacent to the Trans-Canada Highway . It has a small shopping centre, Samson Mall, which includes a park visitor centre, grocery store, bakery, deli, grill, bar and sporting goods store. The ski area, Lake Louise Mountain Resort, is located across Highway 1. The second community is at a higher elevation and is centered on the Chateau Lake Louise, adjacent to Lake Louise. The community is also located on Alberta Highway 1A, and just south of the Icefields Parkway.

Lake Louise

Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km west of the Hamlet of Lake Louise and the Trans-Canada Highway . Lake Louise is named after the Princess Louise Caroline Alberta, the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 and is drained through the 3 km long Louise Creek into the Bow River. Fairmonts Chateau Lake Louise, one of Canadas grand railway hotels, is located on Lake Louises eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway. Moraine Lake and Lake Agnes are also accessible from Lake Louise.

Valley of the Ten Peaks

Valley of the Ten Peaks is a valley in Banff National Park in Alberta, Canada, which is crowned by ten notable peaks and also includes Moraine Lake. The valley can be reached by following the Moraine Lake road near Lake Louise. The ten peaks were originally named by Samuel Allen, an early explorer of the region, who simply referred to them by using the numerals from one to ten in the Stoney First Nations Language. He may have learnt the terms from his Native American guides, who helped him with the horses. The Nakoda also known as the Stoney Indians is a tribe whose culture and dialect are closely related to that of the Assiniboine First Nation, from whom they are believed to have separated in the mid-1700s, and who roamed large parts of the prairies and mountains of western Alberta well into British Columbia. The secluded Valley of the Ten Peaks was part of their original homeland. Gradually, though, all but three of the mountains were renamed in honour of noteworthy individuals, including Allen himself. Mount Hungabee was not included in the original peak list by Allen, even though it is higher than Wenkchemna Peak, the latter of which is really an extension of Hungabee.

Banff

Banff is a town within Banff National Park in Alberta, Canada. It is located in Albertas Rockies along the Trans-Canada Highway, approximately 126 km west of Calgary and 58 km east of Lake Louise. At an elevation of 1,400 m to 1,630 m, Banff is the community with the second highest elevation in Alberta after Lake Louise. The Town of Banff was the first municipality to incorporate within a Canadian national park. The town is a member of the Calgary Regional Partnership. Banff is a resort town and one of Canadas most popular tourist destinations, known for its mountainous surroundings and hot springs. It is a destination for outdoor sports and features extensive hiking, biking, scrambling and skiing areas within the area. Sunshine Village, Ski Norquay and Lake Louise Mountain Resort are the three nearby ski resorts located within the national park.

Chateau Lake Louise

The Fairmont Chateau Lake Louise is a Fairmont Hotel on the eastern shore of Lake Louise, near Banff, Alberta. The original Chateau was gradually built up at the end of the 19th and the beginning of the 20th century by the Canadian Pacific Railway and was thus "kin" to its predecessors, the Banff Springs Hotel and the Château Frontenac. The hotels wooden Rattenbury Wing burned down on 3 July 1924, and was replaced by the current Barrot Wing one year later. The Painter Wing, built in 1913, is the oldest portion of the hotel still standing. The Mount Temple Wing, opened in 2004, is the newest wing of the hotel and features modern meeting facilities, including the Mount Temple Ballroom. The hotel was first conceived by the railway at the end of the 19th century, as a vacation destination to lure moneyed travellers into taking trains and heading West. By the time airplanes and automobiles had displaced the trains, it had gained sufficient renown to have a life of its own. In 1999, Canadian Pacific Hotels acquired Fairmont Hotels and Resorts, and adopted the Fairmont name for all of its hotels, resulting in the Chateau Lake Louise being operated as a Fairmont hotel. From the start, the goal was to exploit the stunning natural beauty of the emerald-green lake and of Victoria Glacier which rose above it. There were many hiking and canoeing itineraries for nature lovers. Eventually, all the natural areas around the hotel were incorporated into Banff National Park. This park has been declared a World Heritage Site by UNESCO. Originally built to function only in summer, the hotel was winterized in 1982 and now offers all of the regular ski resort fare during the winter months. In addition to the usual skiing, ice skating and snowboarding, there are sleigh rides, ice sculpture contests and snowshoe excursions. The hotel is also a popular place for special events, including hundreds of weddings, throughout the year. Currently, The Chateau Lake Louise resort hotel is owned by Oxford Properties, the real estate arm of OMERS and operated by Fairmont Hotels and Resorts of Toronto.

Banff Springs Hotel

The Banff Springs Hotel is a luxury hotel that was built during the 19th century as one of Canadas grand railway hotels, being constructed in Scottish Baronial style and located in Banff National Park, Alberta, Canada. The hotel was opened to the public on June 1, 1888. Presently, The Fairmont Banff Springs resort hotel is owned by OMERS and operated by Fairmont Hotels and Resorts of Toronto. Banff Springs Hotel is situated at an altitude of 1414 m. The original building was designed by American architect Bruce Price. It was built between spring 1887 and spring 1888 by the Canadian Pacific Railway at the instigation of its president, William Cornelius Van Horne. The hotel is located within a spectacular setting in the Rocky Mountains, just above the Bow Falls, close to thermal springs. The main view from the hotel is across the valley and toward Mount Rundle, which frequently is cited in geology books for its exposed and tilted ancient seabeds. The hotel is within walking distance of the resort community of Banff. Starting in 1911, a wholly new structure was built in stages to replace the 1888 hotel. Prices Shingle style-influenced wooden structure was replaced with a new building of concrete and faced with stone. The new building was designed by another American architect, Walter S. Painter. Halfway up the internal staircase closest to the Bow Falls is found a noted painting of William Davidson felling trees on the Miramichi River during colonial times. Davidson, who had grown up in Moray, close to Banff, Scotland, was the first European settler in that area of Canada. The name borne by the Canadian city and the national park is derived from his native country. The painting of the pioneer is by the war artist Cyrus Cunoe, who executed a series of paintings for the Canadian Pacific Railway. Banff Springs Hotel is also reputedly haunted. Stories suggest a woman dressed in her wedding gown lost her life on the staircase. There were candles on the staircase when the bride was walking up them, when suddenly her dress caught fire, in a panic she tripped and fell down the stairs, dying from a broken neck. Many people have reported seeing her ghost in full wedding gown, often dancing in the ballroom.

Kicking Horse Pass

Kicking Horse Pass is a high mountain pass across the Continental Divide of the Americas of the Canadian Rockies on the Alberta/British Columbia border, and lying within Yoho and Banff National Parks. A National Historic Site of Canada, the pass is of historical significance because the main line of the Canadian Pacific Railway was constructed between Lake Louise, Alberta and Field, British Columbia using this route in 1880s, in preference to the originally planned route through the more northerly Yellowhead Pass. The pass was first explored by Europeans in 1858 by the Palliser Expedition led by Captain John Palliser. The pass and the adjacent Kicking Horse River were given their names after James Hector, a naturalist, geologist, and surgeon who was a member of the expedition, was kicked by his horse while exploring the region. The original route of the CPR between the summit of the pass near Wapta Lake and Field was known as "The Big Hill"; with a ruling gradient of 4.5 percent, it was the steepest stretch of main-line railroad in North America. Due to frequent accidents and expensive helper engines associated with railroading in the pass, the CPR opened a pair of Spiral Tunnels in 1909 that replaced the direct route. Although these tunnels add several kilometres to the route, the ruling grade was reduced to a more manageable 2.2 percent . The Trans-Canada Highway was constructed through the pass in 1962 following essentially the original CPR route. It reaches its highest point at the Kicking Horse Pass with an elevation of 1,643 metres . Divide Creek, a creek that forks onto both sides of the Continental Divide, is located at Kicking Horse Pass. Dave Broadfoot played The Honourable Member for Kicking Horse Pass in the CBC Television satirical series Royal Canadian Air Farce and in his personal standup routines.

Sulphur Mountain

Sulphur Mountain is a mountain in Banff National Park in the Canadian Rocky Mountains overlooking the town of Banff, Alberta, Canada. The mountain was named in 1916 for the hot springs on its lower slopes. George Dawson had referred to this landform as Terrace Mountain on his 1886 map of the area. Sanson's Peak was named in 1948 for Norman Bethune Sanson who diligently attended the observatory recording equipment atop Sulphur Mountain for nearly 30 years. Two hot springs have been commercially developed. The lowest is the Cave and Basin National Historic Site and the highest is the Banff Upper Hot Springs. A gondola on the eastern slope goes to the summit ridge which has an upper terminal containing two restaurants, a gift shop, and multiple observation decks. The summit ridge provides views both westward up and east down the Bow Valley. A boardwalk can be followed on the north side to the top of Sanson's Peak (2,256 m or 7,402 ft). The original, and more scenic, summit access is along an old fire road (Sanson Road) on the Southwest face of the mountain with a distance of 5.8 km from the Banff Sundance Canyon trail system near the Bow River. Another 5.4 km switchback Trail route exists under the Gondola with Trail-head access from the Banff Hot Springs parking lot near the Gondola terminal. Purists should note that the gondola ride down is no longer free in the summer.

Sunwapta Pass

Sunwapta Pass is a mountain pass in the Canadian Rockies in the province of Alberta. The pass marks the boundary between Banff and Jasper National Parks. The Icefields Parkway travels through Sunwapta Pass 108 km southeast of the town of Jasper and 122 km northwest of the Parkways junction with the Trans-Canada Highway near Lake Louise. The pass is the second highest point on the Icefields Parkway. Bow Summit in Banff National Park is the highest point on the parkway. Sunwapta Pass marks the watershed divide between the Athabasca River drainage to the north and the North Saskatchewan system to the south. Waters flowing north from this summit eventually reach the Arctic Ocean via the Mackenzie River, while those flowing south cross the prairies via the Saskatchewan and Nelson Rivers to Hudson Bay and the Atlantic Ocean.

Mount Assiniboine

Mount Assiniboine, also known as Assiniboine Mountain, is a mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 3,618 m, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike 27 km, three hour bike ride or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.

Mount Rundle

Mount Rundle is a mountain in Canadas Banff National Park overlooking the towns of Banff and Canmore, Alberta. The Cree name was Waskahigan Watchi or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudsons Bay Company to do missionary work in western Canada in the 1840s. He introduced syllabics there—a written language developed for the Cree, as part of his missionary work. He only visited the Stoney-Nakoda of the area around what is now called Mount Rundle in 1844 and 1847. Mt. Rundle could actually be considered a small mountain range as the mountain extends for over 12 kilometres, on the south side of the Trans-Canada Highway 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 . West of the Spray Lakes road is the East End of Rundle— locally known as EEOR—which rises above Whitemans Gap just south of Canmore. The Rundle Peaks are part of the South Banff Ranges, along with its siblings—the Sundance Range, Sulphur Mountain and the Goat Range.

Banff Upper Hot Springs

Upper Hot Springs are commercially developed hot springs located in Banff National Park in Canada, near the Banff townsite. The hot pool is outdoors and while in the pool, visitors can look across the valley to Mount Rundle. The Upper Hot Springs are one of nine different naturally occurring hot springs in the Banff area. The hot spring water flows naturally through the Sulphur Mountain Thrust Fault, with the source area located at higher elevations on either Sulphur Mountain or Mount Rundle. The flow rates fluctuate seasonally with snow melt, with highest flows in the spring and lowest during winter. Since the early 2000s, flow to the Upper Hot Springs has stopped for several months of the winter. During these times, municipal water is substituted for the recreational pools. Water temperature is kept at approximately 38°C . The Banff Springs snail is absent from the Upper Hot Springs region.

Bankhead

Bankhead, Alberta was a small coal mining town that existed in the early twentieth century, in Banff National Park, near the town of Banff, Alberta. The mine was located at Cascade Mountain, which contains high grade anthracite coal deposits. The Bankhead coal mine was operated by the Pacific Coal Company, a subsidiary of the Canadian Pacific Railway, which needed the coal to fuel its steam engines. The mine began operations in 1903 and was the first anthracite mine in Canada. A local newspaper report published 17 June 1922 indicated that notices of the closure of the Bankhead Mines had recently been posted through that town. The notices made it clear that on and after 15 July the staff of Bankhead Mines would not be required and the coal operations would cease. The report concluded: "This would indicate that after the above date Bankhead will be a dead town so far as coal mining is concerned." This report concluded that no reasons were given for the closure, although it was generally understood that mining there had not been profitable. There had been a strike at the mine two months before this announcement, and the mines had been closed since that time. Another report on the mine closure noted that around 200 to 300 men were employed there with the output of coal running between 500 to 600 tons per day. The town population was around 1,000 people. All of Bankheads buildings were built and owned by the company and rented to the residents. In 1926, many of the towns buildings were moved to Banff and Canmore. The Bankhead Railway Station now sits on the grounds of the Banff Hostel on Tunnel Mountain Road. It has a map of the Bankhead townsite posted outside its front door. Today, an interpretive trail runs through Lower Bankhead. Signs are placed along the trail identifying the major buildings, as well as other interesting facts. Many foundations of buildings are visible. One building remains intact and contains displays viewed through the windows. Remains of the town are also visible adjacent to the Upper Bankhead parking lot. Bankhead is located on the Lake Minnewanka road, just a few minutes drive from the Banff townsite or the Trans Canada Highway. Near Bankhead was another coal mine, Anthracite. This mine was a failure because of heavy water inflow in the underground. The Anthracite mine shut down in 1904 and was abandoned.

Skoki Ski Lodge

The Skoki Ski Lodge National Historic Site of Canada was built in 1930-31 in the Skoki Valley of Canadas Banff National Park. Built by local members of the Ski Club of the Canadian Rockies, the lodge was the first commercial building built specifically to serve skiers in Canada, and possibly in North America. Design and construction work was carried out by local outfitter and builder Earl Spencer with help from Spud White and Victor Kutschera. The lodge was progressively expanded through 1936 by outfitter, guide and log home builder Jim Boyce who was also managing the Lodge the time. It has remained unaltered since that time. The Lodge operates throughout the year. The Skoki Ski Lodge is 6.8 miles from the nearest road. The lodge was conceived by Clifford Whyte and Cyril Paris. The first version of the lodge was a single story log building, 25 feet by 16 feet . A resting shelter, the Halfway Hut, was built the following year halfway between Skoki and the Lake Louise railway station. A kitchen and two cabins were also built that year. Management was taken over by Clifford Whytes younger brother Peter and his wife Catharine of whom the Whyte Museum of the Canadian Rockies is named. After the 1932 season, when a guest was killed in an avalanche, Jim Boyce took over management and continued to operate the camp through the 1930s. A major expansion took place in 1935-36. The upper story rooms were added at this time, as well as a bathhouse and more cabins. In 1972 the lease passed from the Ski Club to Lockes Resorts of the Canadian Rockies. The camp was designated a National Historic Site of Canada in 1992. The first non-native to explore the Skoki Valley was James Foster Porter of Illinois in 1911. Porter and his companions suggested many names for the beautiful place, including the "Skokie Valley" which was later revised to Skoki. Skoki, the new spelling, is a Native word for "swamp" which does not actually reflect the valley. Porter was so impressed with the name that a suburb in Chicago near his home was later renamed Skokie. The lodge was designated as a National Historic Site of Canada in 1992 for its contribution to early tourism in the national parks and as an example of the rustic designs style. During the 2011 royal tour of Canada, the Duke and Duchess of Cambridge stayed at the lodge.

Mistaya Canyon

Mistaya Canyon is a canyon in the western part of the Alberta province of Canada. It is formed by the Mistaya River. Tourists who are visiting Banff National Park often visit it because of its distinctive curvy canyon walls and because it is easy to access, being just off the Icefields Parkway. The 0.5 km trail to the canyon is located at a large parking area on the west side of the Parkway, part way up the long hill south of the North Saskatchewan River. There are actually two such parking areas on the hill; the Mistaya one is clearly marked by signs on the highway and at the beginning of the trail. The trail is an easy walk in summer but too steep for wheelchairs. The canyon is deep and there are no railings. The trail is icy in early spring. Hikers will find that the Howse Pass Trail continues past the canyon.

Bow Glacier

Bow Glacier is located in Banff National Park, Alberta, Canada, approximately 37 km northwest of Lake Louise, and can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide, and runoff from the glacier supplies water to Bow Lake and the Bow River. The glacier is credited for creating the Bow Valley before retreating at the end of the last glacial maximum. Since the end of the Little ice age in 1850, Bow Glacier has been a state of steady retreat overall. Between the years 1850 and 1953, the glacier retreated an estimated 1,100 metres, and since that period, there has been further retreat which has left a newly formed lake at the terminal moraine at the glacial snout. Sedimentation has also increased in Bow Lake due to increased erosion of soil that was previously protected by the glacier, creating a small sediment delta at the western end of the lake.
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