In this article, we will explore the topic of Mont Shefford from different perspectives and with the aim of providing a comprehensive view on its importance, impact and relevance today. Through a detailed and rigorous analysis, we will examine the various aspects related to Mont Shefford, addressing both its origin and its evolution over time. Likewise, we will delve into the practical and theoretical implications that Mont Shefford has in different contexts, as well as its influence on society and daily life. With a critical and reflective approach, this article seeks to offer an enriching and in-depth look at Mont Shefford, providing knowledge and perspectives that invite reflection and debate.
This article needs additional citations for verification. (February 2024) |
Mont Shefford | |
---|---|
Highest point | |
Elevation | 526 m (1,726 ft) |
Coordinates | 45°21′49″N 72°37′33″W / 45.36361°N 72.62583°W |
Geography | |
Shefford, 12 kilometers southeast of Granby, Quebec, Canada | |
Parent range | Monteregian Hills |
Topo map | NTS 31H7 Granby |
Geology | |
Age of rock | Early Cretaceous |
Mountain type | Intrusive stock |
Mont Shefford is a Monteregian Hill located in Shefford in the Estrie region of Quebec, Canada.
Mont Shefford is 526 metres (1,726 ft) tall, and was home to the Ski Shefford ski resort which closed in 2006.
Mount Shefford was formed some 125 million years ago during an underground intrusion of magma. This magma did not reach the Earth's surface and remained in a deep freeze. The mountain appeared following the erosion of nearby sedimentary rocks by glaciers. The sedimentary rock was more fragile than the metamorphic rock formed by the contact of the magma and the surrounding sedimentary rock.