Moraines are glacially deposited ridges of debris that accumulate at the sides or terminus of a glacier. Lateral moraines form at the sides of glaciers and terminal moraines at the terminus of a glacier. Terminal moraines mark the maximum advance of a glacier. Moraines are made up of glacial debris ranging in size from enormous boulders to fine glacial flour. Boulders and rocks in moraines are generally rounded due to the churning and grinding within the glacier as it moved.
Chimney: a gap between two vertical faces of rock or ice. Often a chimney offers the only viable route to the summit of a mountain. An example of this is Black ...
Mount Garibaldi is the huge, potentially active volcano that Garibaldi Provincial Park is named after. Mount Garibaldi also lends its name to the Garibaldi ...
Alec Dalgleish (1 August 1907 - 26 June 1934) was a highly respected mountaineer and climber out of Vancouver in the 1920's and 1930's. His enthusiasm and ...
Crevasse: is a split or crack in the glacier surface, often with near vertical walls. Crevasses form out of the constant movement of a glacier over ...
Mountain hemlock is a species of hemlock that thrives along the west coast of North America from Alaska to California. In Whistler and Garibaldi Park you ...
When you hike in the alpine in Whistler and Garibaldi Provincial Park, you will often encounter unbelievably hardy and sometimes mangled looking trees. ...
The Barrier formed as a result of huge lava flows from Clinker Peak on the west shoulder of Mount Price during the last ice age. About thirteen thousand ...
Tom Fyles (27 June 1887 - 27 March 1979) was an astoundingly skilled climber that figured prominently in the climbing community of Vancouver for more than two ...