Search results
Results from the WOW.Com Content Network
The lake is best seen from Bow Summit, the highest point on the Icefields Parkway. [4] The lake is fed by Peyto Creek, which drains water from Caldron Lake and Peyto Glacier (part of the Wapta Icefield). Peyto Lake is the origin of the Mistaya River, [5] which heads northwest from the lake's outflow. Peyto Lake seen from Bow Summit
Mount Jimmy Simpson is a 2,966-metre (9,731-foot) summit located 3 kilometres (1.9 miles) northwest of Bow Lake in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Thompson , 3.0 km (1.9 mi) to the southwest. [ 2 ]
Peyto Peak is a mountain in the Waputik Range, part of the Canadian Rockies in Alberta, Canada. It lies at the north end of the Wapta Icefield , in Banff National Park , about one km (0.6 mi) east of the border with British Columbia and 32 km (20 mi) north of the town of Field .
Other scenic lakes near the parkway include Bow Lake, and Peyto Lakes, both north of Hector Lake. The Parkway then crosses Bow Summit (2,088 m (6,850 ft)), and follows the Mistaya River to Saskatchewan Crossing, where it converges with the Howse and North Saskatchewan River. Bow Summit is the highest elevation crossed by a public road in Canada ...
Mistaya River originates in Peyto Lake, a glacial lake of typical blue colour (due to rock flour). Mistaya flows north-west, receiving the waters of creeks such as Delta, Silverhorn, Cirque, Noyes, Chephren, Totem, Epaulette, Bison, Kaufmann and Sarbach. A series of elongated lakes are formed along the river: Mistaya Lake and Waterfowl Lakes.
The search engine that helps you find exactly what you're looking for. Find the most relevant information, video, images, and answers from all across the Web.
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
As is true for the vast majority of glaciers worldwide, Peyto Glacier has been retreating rapidly, especially since the last half of the 20th century, and has reportedly lost 70% of its mass since it was first researched (Demuth and Keller, 2006). Between 1896 and 1966, the total volume loss of the Peyto Glacier was 1088.5 x 10 6 m 3 (Wallace ...