Supper at the Maple Leaf, banffmapleleaf.com, all 26 of us.
Top of Larch at Lake Louise on Feb. 7, 2017 John, Cindy, Rick, Dan, Maureen, Bing, Bruce, Vince
Bruce, John, Dan, Rick, Jerry L, Cindy, Vince, Maureen
Lake Louise: Helen & Jerry B, Lavora, Jerry L
Lynn, Lavora, Shirley
Lavora, Lynn
Jerry L sporting a club red bandana
Linda and Bob
Shirley, Bonnie
Cindy
Sunshine Village ski base
Sunshine Village sits high on the Continental Divide in the heart of Banff National Park just 15 minutes’ drive from the cozy mountain town of Banff.
Sunshine Village. A very scenic 20 minute gondola ride up to the base.
Banff Caribou Lodge & Spa
Feb. 6, a Monday, nobody skied. The high was -3 F. John and Dan at the Caribou Lodge staying warm.
Lunchtime on the mountain at Lake Louise.
Supper at the many restaurants to choose from in the town of Banff
View down the Banff Avenue (main street) of Banff.
Banff railroad station
The Canadian Rockies are quite different in appearance and geology from the American Rockies to the south of them. The Canadian Rockies are composed of layered sedimentary rock such as limestone and shale, whereas the American Rockies are made mostly of metamorphic and igneous rock such as gneiss and granite. The Canadian Rockies are overall more jagged than the American Rockies, because the Canadian Rockies have been more heavily glaciated, resulting in sharply pointed mountains separated by wide, U-shaped valleys gauged by glaciers, whereas the American Rockies are overall more rounded, with river-carved V-shaped valleys between them. The Canadian Rockies are cooler and wetter, giving them moister soil, bigger rivers, and more glaciers. The tree line is much lower in the Canadian Rockies than in the American Rockies. https://en.wikipedia.org/wiki/Canadian_Rockies
Sunday, Feb. 12. Waiting in comfortable surroundings for our flight out of Calgary.
Carol, Barb, Dot, Shirley
Maureen, Vince, Bruce
End of trip - Have arrived back to MSN airport. Dot's ski bag didn't survive the TSA inspection.