What landforms are created by glacial erosion?
Glaciers can change the landscape and create glacial features, like U-shaped valleys and ribbon lakes.
In this article you can learn:
- What a glacier is
- How U-shaped valleys and hanging valleys are formed
- How a ribbon lake and misfit stream are formed
- Reindeer in Scotland
This resource is suitable for Landscapes topics for primary school learners.
Video - Glaciated valley erosion
Join Isla and Connor as they explore features of glaciated erosion, such as U-shaped valleys and hanging valleys, in the Cairngorms National Park.
Watch this short video to find out about features of glaciated erosion.
CONNOR: Here we are at the Cairngorms National Park! The biggest National Park in the UK!
It's named after Cairn Gorm, the mountain we're about to climb, which is, naturally, in the Cairngorm mountain range.
ISLA: I’ve visited Scotland’s other national park, Loch Lomond and the Trossachs, and there’s always so much to see, so I’m ready to explore this one too!
CONNOR: Yeah, the national parks are really important for our wildlife and for people to enjoy access to the great outdoors.
ISLA: I bet this is a lot harder to climb in the winter.
CONNOR: We could have gone skiing then, but now it’s perfect for hiking - and of course we get these spectacular views…
ISLA: Look over there. See that U-shaped valley?
That’s Lairig Ghru. It was carved out by a glacier, a huge river of ice, during the ice age - just like corries and other glacial features.
As glaciers move downhill under the force of gravity, they erode downwards and outwards changing V-shaped valleys into U-shaped valleys with flat floors and steep sides. Glacier ice has great erosive power removing almost any obstacle in its way.
CONNOR: Wow, you wouldn’t want to get in the way of a glacier, would you?
ISLA: Luckily, they move very slowly. A U-shaped valley forms over hundreds of thousands of years, not during our lifespan. Phew! When things move that slowly it’s called geologic time.
Wow, Loch A’an is beautiful isn’t it!
CONNOR: Loch A’an is a ribbon lake - and River A’an in the distance, is a misfit stream.
ISLA: Looks like it fits to me…
CONNOR: After the ice age, once glaciers have melted away, a misfit stream, ribbon lake or a loch can sometimes form on the floor of a U-shaped valley.
A ribbon lake is a large, narrow lake found in a U-shaped valley. It forms in a hollow that a glacier has eroded more deeply.
Misfit streams or rivers meander through the flat, wide U-shaped floor. They are not powerful enough to have eroded the much larger U-shaped valley, that’s why they’re called a ‘misfit’ stream or river.
ISLA: Look at this, Coire Domhain - yet another glacial feature! See how it’s above Loch A’an, the U-shaped valley? That makes it a hanging valley.
Hanging valleys are created where smaller valleys meet the main glaciated valley. They get cut off so while erosion makes the main valley deeper and deeper, the smaller valley is left hanging higher up above the valley floor.
CONNOR: Oh wow, look!
ISLA: A ptarmigan! They’re masters of disguise. They have different colours of feathers at different times of year. White in winter to blend into the snow, dark in summer to match the grey rocky landscape. A great spot.
CONNOR: It’s flown up to the Cairngorm Plateau.
ISLA: What’s that?
CONNOR: Plateau means the top of a high area of ground. Let’s go and see it…
This is the plateau!
ISLA: Reindeer! No way!
CONNOR: It’s the only place reindeer live naturally in the UK. They were reintroduced in the 1950s and thrive because the extremely cold weather and the long-lasting snow patches make it an ideal place for them.
ISLA: Wow, you’d think it was the Arctic instead of Scotland. I love it!
CONNOR: Me too - but let’s get down to warmer temperatures.
What is a glacier?
- A glacier is a huge mass of ice that moves slowly across land.
- A moving glacier can erosionWearing away over time. the land and create features of glaciated erosion such as corries, arêtes and pyramidal peaks.
How are U-shaped valleys formed?

- Glaciers erode distinctive U-shaped valleys with a flat floor and steep sides.
- The processes of pluckingWhen 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. and abrasionA type of glaciated erosion. When rocks and stones become stuck to the bottom and sides of a glacier and erode the land as the glacier moves. widen, steepen, deepen and smooth 'V'-shaped river valleys into a 'U' shape.

Features of a U-shaped valley floor
- A ribbon lake is a large, narrow lake that can be found in a U-shaped valley. It forms in a hollow where the rock is softer and a glacier has eroded the valley floor more deeply.
- Misfit streams or rivers meander through the flat, wide valley floor. They are much smaller than the valley itself, and formed after glaciation had carved out the much larger U-shaped valley.
Hanging valleys
Hanging valleys are created where smaller valleys meet the main glaciated valley. The glaciers in the smaller valleys were not so powerful, so they didn't erode such deep valleys. This means the smaller valleys are left hanging above the floor of the main valley.
Features of glacial valley erosion in pictures
Image caption, U-shaped valley
During the Ice Age, U-shaped valleys were formed in river valleys that were eroded by large large glaciers. A U-shaped valley has steep sides and a wide flat floor, like Lairig Gartain in Glen Coe. (Richard Clarkson / Alamy Stock Photo)
Image caption, Ribbon lake
Loch Lomond is the biggest loch in Scotland but did you know it's also a ribbon lake? It was formed after a glacier eroded the original V-shaped valley into a deep U-shaped valley. (Richard Johnson / Alamy Stock Photo)
Image caption, Misfit stream
A misfit stream or river meanders through the flat wide floor of a U-shaped valley. This misfit stream is in the valley of Glen Catacol on the Isle of Arran. (Les Gibbon / Alamy Stock Photo)
Image caption, Hanging valley
Coire Domhain in the Cairngorms National Park is an example of a hanging valley. A hanging valley is formed where a small glacier joins a larger glacier. The smaller glacier is less powerful and doesn't erode its valley as deeply as the large glacier. This leaves the smaller valley hanging high up the side of the main valley.(Keith Fergus / Alamy Stock Photo)
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Scottish wildlife: reindeer
In the video at the top of the page, Isla and Connor spotted reindeer on Cairn Gorm. Let's find out more about reindeer in Scotland.
- Reindeer are a type of deer.
- Reindeer are adapted to live in extremely cold, snowy conditions, like the Arctic. Their very thick fur acts as insulation that keeps them warm. They have wide hooves, which spread their weight and stop them sinking into deep snow.
- Reindeer were once native species An animal or plant that naturally lives in an area (with no humans involved). to Scotland but went extinct A species that no longer exists. in Scotland hundreds of years ago. They were reintroduced to the Cairngorms in the 1950s.
- The Cairngorm mountains have a cold climate. They are the only place in the UK where you can find free-roaming reindeer.
- There are currently around 150 reindeer in the herd on the Cairngorm mountains.


Key words about glaciated valley erosion
- national park - An area set aside by government to preserve the natural environment. A national park is also set aside because of historical or scientific interest as well as enjoyment by the public.
- glacier - A massive river of slow moving ice.
- glacial features - Landscape features that have formed by glaciers.
- geologic time - Extremely long period of time. Geologic time refers to the billions of years since Earth started developing.
- 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.
- erosion - Wearing away.
- u-shaped valley - A valley with steep sides and wide flat floor. It takes on the shape of the letter 'u'. They are formed in river valleys which, during the ice age, have been filled by a large glacier .
- hanging valley - A small valley that meets a larger glaciated valley. The smaller valleys are not powerful enough to erode deep valleys so they are left hanging above the main valley.
- ribbon lake - A large narrow lake found in a u-shaped valley. It forms in a hollow that a glacier has eroded more deeply.
- misfit stream - A steam or river that meanders through the flat wide floor of a u-shaped valley.
Test your knowledge
Quiz
Challenge

Write a poem about nature.
The Cairngorms National Park is one of the biggest national parks in the UK and the beautiful landscape there has often been a source of inspiration to artists.
Scottish poet, Nan Shepherd, was so inspired by the Cairngorms she wrote a whole collection of poetry about the area.
'Loch A’an, Loch A’an, hoo deep ye lie!Tell nane yer depth and nane shall I.'
Loch A'an written by Nan Shepherd from In the Cairngorms (Edinburgh: The Moray Press, 1934)
Research and read some of Nan Shepherd's nature poetry for some inspiration. Try writing your own nature poem about the landscape near you.
If you need help writing your poem, here is a guide to get you started: How to write a poem
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