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Transcanada Highway
Calgary - Banff - Lake Louise

Driving time Calgary - Banff: 2 hours

Olympic Ski-Jumps

West of Calgary the Transcanada Highway passes the Olympic ski-jumps used during the Winter Games in 1988.

The open landscape of the Great Plains, where huge buffalo herds used to roam until the 19th century, slowly turns into the foothills of the Rocky Mountains.
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Stoney Indian Reserve

Past Calaway Park, an amusement park with roller coasters and carousels, the Transcanada Highway cuts through the Stoney Indian reserve. Many native scouts working for the surveyor teams of the transcontinental railroad in the 19th century came from this First Nation.

The prairie grasslands are slowly interrupted by small groves of lodgepole pines and aspen. The glacial moraines of this region are remnants of the ice ages that helped form this region.
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Kananaskis Region

The exit to Kananaskis country leads into an area offering numerous recreational facilities.

The foothills of the Rocky Mountains, the lowest mountain range at the eastern edge of the mountain chain, is the least spectacular. The mountains slowly rise from the glacial moraines further east.

The first street signs caution drivers against wild animals on the road. Bears, wapitis, moose and other animals are possibly dangerous. Each year bears or wapitis attack unsuspecting visitors to these areas. Therefore caution is advised.
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Lac des Arcs

On the north shore of the lake Lac des Arcs a huge cement plant digs into the mountain behind it. This weakens the mountainside continuously. Geologists warn of a possible disaster. They fear a landslide might destroy this part of the valley.

In the second mountain range of the Rocky Mountains, the front ranges, the rock composition of the mountains changes. Here the geological layers consist of shales, limestone and sandstone. The mountains reach elevations of up to 2500 m. The highest mountain of the front ranges is Mt. Oliver (3009 m).
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Canmore

During the Olympic Winter Games in 1988 some of the sport events took place close to Canmore. Many of the new suburbs were used as accommodation for the competitors. Today Canmore is a tourist center close to Banff National Park which offers accommodation, restaurants and other amenities.

Hotels in Canmore

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Banff National Park

Rocky Mountains around Banff The entrance station to Banff National Park lies just a few kilometers behind Canmore. Anybody who wants to spend a night in the National Park has to pay entrance fees. Who is just passing through on the Transcanada Highway and does not plan to spend a night in Banff, Lake Louise or Field or visit any of the sights along the way can pass without paying.

Shortly before the turnoff to Banff there are gravel hills on each side of the Transcanada Highway. Geologists believe them to be remnants of a huge mudslide that filled the Bow River Valley, when the glacial lake water of Bow Glacier soaked through the terminal moraine at the end of the lake. This material eventually covered the valley in an enormous mudslide.

Hotels in Banff

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Driving time Banff - Lake Louise: 45 minutes

From Banff to Lake Louise

The highway passes Vermillion Lakes after the turnoffs to Banff. This is moose habitat. Dall sheep, ospreys and bald eagles can also been spotted.

The mountains around the lake are Tunnel Mountain around which the town of Banff has been built. Mt. Rundle (2949 m) can be recognized easily. It is the mountain behind town that seems to grow out of the bottom at an angle. The long mountain to the right is Sulphur Mountain (2451 m). Next to it follows the Sundance Range. The highest mountain to the west is Mt. Bourgeau (2931 m), one of the major mountains of the Massive Range.
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Sunshine Valley

The next major turnoff leads to Sunshine Valley, a ski area close to Banff. The Sunshine Village gondola offers one of the longest gondola rides in Canada. It transports skiers over a length of 5 kilometers.
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Exit to Bow Valley Parkway

Bow Valley Parkway follows the Bow River Valley. If you are lucky you may see bears, dall sheep or wapitis. The best times of day to watch out for animals are mornings and evenings. There also are some hiking trails along this road leading to different areas in the mountains.
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Castle Mountain (2766 m)

A huge turnout to the right offers good views of the surrounding area. Not to be missed is the castellate mountain ahead. This is Castle Mountain. It received its name from Dr. James Hector of the Palliser Expedition in 1858. Castle Mountain

After the Second World War it was known under a different name for a while. The Scots decided then to present Dwight D. Eisenhower, a general of the allied forces, with a castle and thus thank him for his services during the war. Canada also wanted to reward Eisenhower and renamed Castle Mountain in his honor. However, the people living in this area did not like this. Therefore the mountain got his old name back in 1979 by government decision. Today only the first tower is named Eisenhower Peak while the treeless plain below it irreverently is called Eisenhower's Golf Course.
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Sawback Range

Sawback Range can be seen from this viewpoint. A row of rock faults separates the younger rocks of the front ranges from the older ones of the main ranges. The front ranges, of which the Sawback Range is part, lie in the eastern part of the Rocky Mountains. Their rocks were formed 250 to 350 million years ago. The mountains of the main range consist of rocks older than 500 million years. At the time of their creation these layers were accumulated horizontally and were only tilted when the Rocky Mountains were formed 70 million years ago. Erosion has carved out these nearly vertical layers and created the sawtooth like mountain summits.
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Mt. Temple (3544 m)

Fall in the Canadian Rockies Mt. Temple is the highest mountain in the Lake Louise area and the third highest mountain in Banff National Park. It consists of layers of quartz sandstone and limestone that were formed during the precambrium more than 500 million years ago. At this time only very primitive life forms existed in the oceans and no life existed on land.
Mt. Temple was named after Sir Richard Temple, an English scientist, who led an expedition through the Canadian Rockies in 1884.
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Exit to Lake Louise

From here the view of Mt. Temple is most impressive. Behind it lies the glaciated peak of Mt. Victoria (3463 m) on the far end of Lake Louise. To the left of it is Mt. Fairweather (2744 m), while the Beehive is on the right side of the Lake.

Hotels in Lake Louise

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Additional Links:
City Guide Calgary
City Guide Banff
Guide Lake Louise
TravelWorldOnline Alberta Travel Guide

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