Mount Andromache is a 3,033-metre (9,951-foot) mountain summit located in the Bow River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Mount Hector, 4.00 km (2.49 mi) to the south.[1] Mount Andromache can be seen from the Icefields Parkway as the road traverses the western base of the peak. Topographic relief is significant as the summit rises 1,180 m (3,870 ft) above the parkway in 1.5 km (0.93 mi). The Molar Glacier is situated on the northeast aspect of the mountain. Precipitation runoff from Mount Andromache drains into tributaries of the Bow River.
Based on the Köppen climate classification, Mount Andromache is located in a subarctic climate with cold, snowy winters, and mild summers.[5] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for viewing and climbing this mountain.
Geology
Like other mountains in Banff Park, Mount Andromache is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.[6] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[7]
