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Glaciated mountain erosion features

Glaciers are massive rivers of ice that move across land. They can change the landscape and create glacial features on mountains, like corries and 补谤锚迟别s.

In this article you can learn:

  • What a glacier is
  • How corries and 补谤锚迟别s are formed
  • How a pyramidal peak is formed
  • How to stay safe when climbing mountains

This resource is suitable for Landscapes topics for primary school learners.

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Video - Features of glaciated erosion

Join Isla and Connor as they climb Ben Nevis and explore features of glaciated erosion: corries, 补谤锚迟别s and pyramidal peaks.

Watch this short video to find out about the features of glacial erosion.

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What is a glacier?

  • A glacier is a huge mass of ice that moves slowly across land.
  • A glacier needs very cold temperatures and lots of snow to form.
  • Air temperature gets lower the higher up you are from . That's why you can often see snow on mountain tops.
  • Glaciers usually form high up on mountains because the temperature is much lower.
The Perito Moreno glacier
Image caption,
A glacier is a massive river of slow moving ice. There are no glaciers left in the UK but their erosive powers can be seen in our landscape. This huge glacier is the Perito Moreno Glacier in Argentina. (Renato Granieri / Alamy Stock Photo)

Glaciers in Scotland

During the last , Scotland was often covered in . They formed high on mountains and flowed downhill. Now the glaciers have gone we can see how they shaped the mountains, forming corries, 补谤锚迟别 and pyramidal peaks.

Labelled cross-section of a u-shaped valley showing features of mountain erosion
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What is a corrie?

  • A corrie is an armchair-shaped hollow found on the side of a mountain. It is the place where a once formed.
  • Most corries were formed during .
  • Snowflakes collect in a hollow. As more snow falls, the snow gets squashed (compressed) and air is squeezed out.
  • Over thousands of years, the compacted snow becomes hard glacier ice.
  • The hard glacier ice gets so heavy that it begins to move downhill. Ice that has melted into water underneath helps the glacier to move.
  • Eventually, the moving glacier the surface of the corrie. This is glaciated erosion.

Glaciated erosion takes place in two ways:

  1. Plucking steepens the back wall of the corrie.
  2. Abrasion deepens the hollow of the corrie.
A diagram showing how a glacier erodes in two ways: plucking and abrasion

What happens when corries form back-to-back?

  • When two corries form back-to-back, a steep ridge called an 补谤锚迟别 is created.
  • When three or more corries erode a mountain back-to-back, the 补谤锚迟别s form a pyramidal peak. This is the classic mountain shape that looks like a pyramid.
Image gallerySkip image gallerySlide 1 of 3, Corrie and lake high in the Black Cuillin mountains, Corrie A corrie is a large hollow on the side of a mountain. A glacier often forms in a hollow and over time the glacier erodes the mountain, making the hollow bigger and forming a corrie. This corrie can be found high in the Black Cuillin mountains on the Isle of Skye. (Photimageon / Alamy Stock Photo)
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Key words sticker

Key words about glaciated mountain erosion

  • glacier - A massive river of slow moving ice.
  • glacial features - Landscape features that have formed by glaciers.
  • corrie - An armchair shaped hollow found on the side of a mountain. This is where a glacier once formed.
  • 补谤锚迟别 - A steep ridge created when two corries form back-to-back.
  • pyamidal peak - When three or more corries erode a mountain back-to-back, ridges (补谤锚迟别s) form a pyramidal peak. This is the classic mountain shape that looks like a pyramid.
  • compact - When two or more objects are closely packed together and there's no space between them. For example, snow can become compacted so there is no room for air between the snowflakes.
  • erosion - Wearing away.
  • plucking - When rocks and stones become frozen to the bottom or the sides of a glacier. The rocks and stones are plucked from the ground or rock face as the glacier moves. Plucking leaves behind a jagged landscape.
  • abrasion - When rocks and stones become stuck to the bottom and sides of a glacier. The rocks and stones rub against the bedrock (at the bottom of the glacier) and rock faces (at the sides of the glacier) as the glacier moves.
  • The Ice Age - A long period of time when the Earth's temperature became very low. The Earth's surface was buried under sheets of ice. It was at its peak about 22,000 years ago.
  • munro - A Scottish mountain that is over 3000 feet (914 metres) high.
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Mountain climbing safety

In the video at the top of the page, Isla and Connor climbed Ben Nevis to explore features of glacial erosion.

Mountain climbing can be very dangerous and you should never try it on your own. Always make sure you have a responsible adult who has climbing experience with you.

You should always tell someone:

  1. Where you are going
  2. The path you are taking
  3. When you expect to be back

Remember to bring:

  • Warm waterproof clothes
  • High energy snacks and a drink
  • A whistle
  • A torch
  • A first aid kit
  • A map
  • A compass

Find out more:

Climbing equipment needed for winter and summer
Two climbers on mountain ridge
Image caption,
Mountain climbing is a popular activity but it can be dangerous. It's really important to follow safety advice.
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Test your knowledge

Quiz

Challenge

Challenge

Design your own 3D mountain.

Use your art and design skills to create a 3D mountain peak. Can you include some glacial features, like corries and 补谤锚迟别s, in your design?

Think about what kind of materials you will need.

Here are some guides to help you with design techniques using paper: Design techniques: Paper cutting

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