Today, Princess Margaret Mountain is a topic of great relevance and interest to a wide range of people and communities. Whether due to its impact on society, its cultural relevance or its importance in the academic field, Princess Margaret Mountain has captured the attention of many, generating debates, reflections and research around this topic. From different perspectives and approaches, Princess Margaret Mountain has aroused great interest due to its influence on various aspects of daily life. In this article, we will explore different facets of Princess Margaret Mountain, analyzing its importance, implications and possible future developments.
Princess Margaret Mountain | |
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Highest point | |
Elevation | 2,515 m (8,251 ft) |
Prominence | 38 m (125 ft) |
Parent peak | Mount Charles Stewart 2809 m |
Listing | Mountains of Alberta |
Coordinates | 51°09′32″N 115°22′08″W / 51.15889°N 115.36889°W |
Geography | |
Alberta, Canada | |
Parent range | Fairholme Range Canadian Rockies |
Topo map | NTS 82O3 Canmore |
Climbing | |
Easiest route | rock climb |
Princess Margaret Mountain is a mountain located in the Bow River valley of Banff National Park, 2.5 km (1.6 mi) west of Mount Charles Stewart.
The mountain was named in 1958 after Princess Margaret (sister of Queen Elizabeth II), who had visited Banff and spent a night in a location near the mountain.
The mountain is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.
Based on the Köppen climate classification, it is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures in winter can drop below −20 °C (−4 °F) with wind chill factors below −30 °C (−22 °F). Weather conditions during summer months are optimum for climbing.