The Athabasca Glacier
The athabasca Glacier national park is established in the Canadian Rockies. The good accessibility due to its place in the immediate vicinity of the Icefields Parkway makes it one of the most visited glaciers in North America.
Pictures of the Athabasca Glacier
Establishment of the Athabasca Glacier
The beautiful glacier park tongue is established on the retreat and is establish today; the athabasca glacier facts are about 1.5 km deep in the elevation to the mid-19th century. The track, which leads up to the tongue of the Columbia Icefield Centre in the beautiful glacier park, panels were erected by the National Park Administration, documenting the retreat of the ice. In athabasca glacier history, the oldest year was built in 1844 and is establish in the immediate vicinity of the visitor center. The tables highlight points, up to which the glacier once stretched. You are impressive evidence of the enormous speed of melting down.
Athabasca Glacier Tour Guide
The Columbia Icefield Centre offered an Athabasca glacier tour guided into the world of eternal. You have the possibility to explore the glacier walk led by an Athabasca glacier tour guide or visit the Athabasca Glacier in the context of an Athabasca glacier tour with special vehicles. The so-called Snowcoaches are up to 20-ton buses with extremely wide tires that go over the 300 meter-thick ice shield. In the Athabasca glacier facts, the estimated capacity of the Athabasca glacier is 640 million cubic meters. Piece by piece, down the Valley moves to the beautiful glacier park. An ice crystal needed for the hike from the top of the glacier up to the glacier tongue of about 180-200 years. The sheet of ice covers about 325 square kilometers and is one of the hugest accumulations of ice South of the Arctic circle. Numerous glacial rivers fed by the Columbia Icefields is the beautiful glacier park, which accumulate in high-altitude Lakes and as turbulent elevation rivers work their way into the Valley.
The Icefield Parkway, a road leads to the parking lot below the terminal moraine. Here, a plaque with the year 1956 refers to the former end of the glacier tongue. About the Forefield Trail, a hiking trail leads to the edge of the huge ice rink. Along the way, the Athabasca glacier history of the park is documented on boards. The way leads through Rocky fields left behind by the retreating. In the Athabasca glacier facts, Significant gradients are partially overcome, covered by loose rubble. Footwear is an essential prerequisite for this Athabasca glacier hike. The trail ends directly in front of the glacier tongue. Barriers refer to the perils of the stand-alone entering of the ice . Especially at the beginning of the summer, still loose layers of snow cover crevasses and deep holes on the ice you see during the Athabasca glacier tour. The risk is underestimated by many Athabasca glacier tours. The fall into a crevasse can have life-threatening injuries, and the body can resist the cold only a few hours.