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Valley of Ten Peaks, Canada

Introduction

The Valley of Ten Peaks is a mountain range in Banff National Park, Alberta, Canada. It consists of ten volcanic peaks that rise dramatically from the surrounding valleys and meadows, creating a unique landscape. The valley's name comes from its distinctive shape, with five peaks forming a "valley" or "ten peak" formation.

Key Facts

  • Location: Valley of Ten Peaks is located in Banff National Park, Alberta, Canada.
  • Elevation: The highest peak has an elevation of 3,197 meters (10,495 ft).
  • Coordinates: Latitude 51.55° N, Longitude 114.30° W.
  • Area: The valley covers an area of approximately 2,700 square kilometers (1,046 sq mi).
  • Climate: The climate in the valley is alpine, with cold winters and mild summers.

Historical Context

The Valley of Ten Peaks was formed during the Laramide orogeny, a period of mountain building that occurred around 70 million years ago. This event uplifted the surrounding rocks, creating a series of volcanic peaks that are now part of the park's landscape. The valley itself is thought to have been carved out by glaciers during the last ice age.

Significant Contributions

The Valley of Ten Peaks has made significant contributions to our understanding of geology and ecology. Its unique landscape provides a natural laboratory for studying the effects of climate change, volcanic activity, and alpine ecosystems. Additionally, the valley's diverse wildlife is an important part of its ecological integrity.

Notable Attractions

  • Mount Rundle: The highest peak in the valley, with an elevation of 3,197 meters (10,495 ft).
  • Lake Minnewanka: A large lake that forms a natural amphitheater in the valley.
  • Johnston Canyon: A scenic canyon that flows into Lake Minnewanka and offers hiking trails and waterfalls.

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  • Generation time: 2024-11-03 06:12:29
  • Keywords: Valley of Ten Peaks, Canada, wiki, history, attractions, facts
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