The Matterhorn oxygen Leyland is a classic example of:The Matterhorn ...
Explanation:
The Matterhorn oxygen Leyland is a classic example of a Pyramid Peak. Let's understand what is a pyramid peak and why Matterhorn oxygen Leyland is an example of it.
What is a Pyramid Peak?
Pyramid Peak is a type of mountain peak that resembles a pyramid or a sharp pointed peak. It has steep sides that converge to a point at the top. These peaks are usually formed by glacial erosion and can be seen in mountain ranges all over the world.
Why is Matterhorn Oxygen Leyland a Classic Example of Pyramid Peak?
Matterhorn Oxygen Leyland is a classic example of a Pyramid Peak because of its unique shape. It has a sharp point at the top and steep sides that converge to the top. The Matterhorn is a mountain in the Alps on the border between Switzerland and Italy. It rises to an altitude of 4,478 meters (14,692 feet) and is one of the highest peaks in the Alps.
The Matterhorn was formed by glacial erosion, which is why it has a distinctive pyramid shape. The peak was first climbed in 1865 by a team led by Edward Whymper. The ascent was controversial and resulted in the death of four of the team members.
Conclusion:
In conclusion, the Matterhorn Oxygen Leyland is a classic example of a Pyramid Peak. Its unique shape and formation make it one of the most recognizable peaks in the world. The Matterhorn is a popular destination for climbers and hikers, and its history and beauty continue to fascinate people all over the world.
The Matterhorn oxygen Leyland is a classic example of:The Matterhorn ...
The Matterhorn is a mountain in the Alps, straddling the border between Switzerland and Italy. It is a classic example of a pyramid peak, which is a type of mountain that has a triangular or pyramidal shape. A pyramid peak is formed when three or more glaciers erode away the surrounding landscape, leaving a sharp peak with steep sides. The Matterhorn is one of the most famous pyramid peaks in the world, known for its iconic shape and challenging climbing routes.
Option (a) refers to a bergschrund, which is a crevasse that forms at the top of a glacier where it separates from the rock face.
Option (c) refers to a corrie lake, also known as a cwm, which is a bowl-shaped depression at the head of a valley that is formed by glacial erosion.
Option (d) refers to a cirque, which is a bowl-shaped depression at the head of a valley that is formed by glacial erosion. A cirque is typically smaller and shallower than a corrie lake.