December 2009

Snowshoe Rummel Lake

by Gillean Daffern on December 30, 2009

Description of snowshoe trip to Rummel Lake in the Smith-Dorrien area and how it compares to Chester Lake snowshoe trail.

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Don’t want to go out into Kananaskis Country on your own? Check out several Meetup Groups in the Calgary area that participate in a variety of activities from easy hiking and snowshoeing to trail running and scrambling.

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How to Use the Avalanche Danger Scale to Reduce Your Risk

by Tony Daffern on December 21, 2009

An explanation of each level of the Avalanche Danger Scale, including the transitions between levels, signs of instability at each level and the implications of slope angle, aspect and elevation.

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Learn more about George Pocaterra & Norma Piper

by Tony Daffern on December 15, 2009

George Pocaterra is best known for settling in the Highwood Valley and establishing the ranch made famous by R. M. Patterson in his book The Buffalo Head. The Diva & the Rancher tells the story of George and his opera singer wife Norma Piper.

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Snowshoe & Scramble up North Kent outlier

by Tony Daffern on December 11, 2009

A climb, on snowshoes and on foot, up the long ridge to the summit of North Kent’s outlier, a superb viewpoint with Mount Chester to the north and the many peaks of the Spray Mountain to the southwest.

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Grooming of Ski Trails at Ribbon Creek this Winter!

by Tony Daffern on December 8, 2009

Originally Alberta Parks said that the cross-country ski trails at Evan Thomas, Ribbon Creek, Skogan Pass and Sawmill in Kananaskis Country would not be groomed this winter. Now they will try to groom Ribbon Creek when resources are available.

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SPOT Satellite GPS Messenger – update

by Tony Daffern on December 4, 2009

SPOT is a handheld satellite communication device that can determine your location using a GPS system and send messages via its own commercial satellite network. A new SPOT Satellite GPS Messenger replaces the original SPOT Personal Tracker.

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What are Persistent Weak Layers?

by Tony Daffern on December 1, 2009

Persistent weak layers such as layers of surface hoar, cohesionless facets and old rain or sun crusts are the usual cause of avalanches that release in old snow layers.

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