Glacial Landscapes in the UKComparison

Erosional vs Depositional Landforms — Upland vs Lowland

Part of Glacial Landforms · GCSE GCSE Geography revision

This comparison covers Erosional vs Depositional Landforms — Upland vs Lowland within Glacial Landforms for GCSE Geography. Revise Glacial Landforms in Glacial Landscapes in the UK for GCSE Geography with 17 exam-style questions and 20 flashcards. This topic appears regularly enough that it should still be part of a steady revision cycle. It is section 9 of 16 in this topic. Use this comparison to connect the idea to the wider topic before moving on to questions and flashcards.

Topic position

Section 9 of 16

Practice

17 questions

Recall

20 flashcards

⚖️ Erosional vs Depositional Landforms — Upland vs Lowland

Category Landform Where Found Formation Process UK Named Example
Erosional
(Upland)
Corrie (cirque/cwm) Mountainside, north/NE facing Rotational flow + plucking (backwall) + abrasion (floor) Red Tarn, Helvellyn; Glaslyn, Snowdon
Arête Upland mountain ridges Two corries eroding from opposite sides — ridge narrows Striding Edge, Helvellyn, Lake District
Pyramidal Peak High mountain summits Three or more corries eroding from different sides of one peak Snowdon (Y Wyddfa), 1,085 m, Wales
U-shaped Valley Major valley floors Glacier transforms V-valley: lateral + vertical erosion Nant Ffrancon, Snowdonia; Langdale, Lake District
Hanging Valley Sides of U-shaped valley Tributary glacier less powerful; erodes shallower than main glacier Watendlath above Borrowdale; Pistyll Rhaeadr, Wales
Truncated Spur Sides of U-shaped valley Glacier cuts off interlocking spurs — cliff faces left Nant Ffrancon; Borrowdale, Lake District
Ribbon Lake Floor of U-shaped valley Over-deepened rock basin fills with meltwater; often moraine-dammed Windermere (17 km); Ullswater; Llyn Tegid
Depositional
(Upland & Lowland)
Drumlin Lowland valleys and plains under former ice Ice reshapes till into streamlined oval hill; stoss faces upglacier Eden Valley, Cumbria; County Down, N. Ireland
Erratic Anywhere glacier reached Rock transported from distant source and dropped as ice melts Norber Erratics, Yorkshire Dales (Silurian on Carboniferous)
Terminal Moraine At maximum glacier extent Till dumped at glacier snout as ice stops advancing Multiple in Lake District; Vale of York
Outwash Plain (Sandar) Lowland beyond terminal moraine Meltwater rivers deposit sorted, stratified sediment East Anglian lowlands; Breidamerkursandur, Iceland (largest)
Kettle Hole Outwash plain Buried ice block melts → depression forms; may fill with water Widespread in East Anglia and Midlands
Esker Outwash plain and beyond Subglacial meltwater river deposits sediment in tunnel; ice melts → ridge remains Common in Ireland, Scotland, Scandinavia

Keep building this topic

Read this section alongside the surrounding pages in Glacial Landforms. That gives you the full topic sequence instead of a single isolated revision point.

Practice Questions for Glacial Landforms

What is the name for the small lake that forms in the floor of a corrie after glaciation?

  • A. Ribbon lake
  • B. Tarn
  • C. Oxbow lake
  • D. Floodplain lake
1 markfoundation

Describe how a corrie (cirque) is formed.

2 marksstandard

Quick Recall Flashcards

What is an arête?
A narrow, knife-edge ridge between two corries or glacial valleys, formed when glaciers erode from both sides of a ridge.
What is a corrie (cwm)?
An armchair-shaped hollow in a mountainside formed by glacial erosion — rotational flow deepens the floor, plucking steepens the back wall.

17 questions on Glacial Landforms — practise free

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