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  2. Peyto Lake - Wikipedia

    en.wikipedia.org/wiki/Peyto_Lake

    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

  3. Caldron Peak - Wikipedia

    en.wikipedia.org/wiki/Caldron_Peak

    Based on the Köppen climate classification, Caldron Peak is located in a subarctic climate with cold, snowy winters, and mild summers. [6] Temperatures can drop below -20 C with wind chill factors below -30 C. Precipitation runoff from Caldron Peak Peak drains into the Mistaya River which is a tributary of the North Saskatchewan River.

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  5. Peyto Glacier - Wikipedia

    en.wikipedia.org/wiki/Peyto_Glacier

    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 ...

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  8. Wapta Icefield - Wikipedia

    en.wikipedia.org/wiki/Wapta_Icefield

    The icefield is shared by Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse and Bow Rivers , as well as numerous streams and lakes.

  9. Mistaya River - Wikipedia

    en.wikipedia.org/wiki/Mistaya_River

    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.