Dr. Ram Prasath Manohar IAS

Aspire

Dr. Ram

Study Materials

General Studies - Geography

Glacial Landforms – Erosional & Depositional

Glacier

  • Glacier = moving mass of ice (a few meters/day)
  • Acts as an agent of erosion, transportation & deposition
  • Carries rock debris → strong abrasive power

 Types of Glaciers

1. Continental Glaciers

  • Large ice sheets
  • Found in:
    • Antarctica
    • Greenland

2. Ice Caps

  • Cover mountain tops
  • Feed valley glaciers

3. Piedmont Glaciers

  • Form a continuous sheet at the mountain base
  • Example: Southern Alaska

4. Valley (Alpine) Glaciers

  • Found in high mountain ranges
  • In India:
    • Siachen Glacier (≈72 km)
    • Gangotri Glacier (≈25 km)

 Glacial Erosional Landforms

1. Cirque / Corrie

  • A bowl-shaped hollow on mountain side
  • Steep on 3 sides, open on 1 side
  • Flat bottom
  • May form Tarn Lake after melting

2. Glacial Trough (U-shaped Valley)

  • Modified river valley
  • Broad floor + steep sides
  • Uniform vertical & lateral erosion
  • Mature stage valley

3. Hanging Valley

  • The smaller tributary valley remains at a higher level
  • Joins the deeper main valley
  • Often forms waterfalls

4. Arete

  • Narrow sharp ridge
  • Formed between two cirques

5. Horn

  • Pyramidal peak
  • Formed when 3+ cirques erode a summit
  • Example: Matterhorn (Switzerland)

6. Fjord

  • A drowned U-shaped valley at the coast
  • Deep, narrow, steep-sided
  • Found in:
    • Norway
    • New Zealand
    • Greenland

 Glacial Depositional Landforms

1. Outwash Plain (Till Plain)

  • Stratified sediments
  • Sand, gravel, clay
  • Formed at the glacier’s melting front

2. Moraine

  • Accumulation of debris
  • Types:
    • Ground moraine
    • Lateral moraine
    • Terminal (End) moraine
    • Medial moraine

3. Esker

  • Long winding ridge
  • Deposited by sub-glacial streams
  • Often used for roads

4. Drumlin

  • Inverted boat-shaped hill
  • Indicates glacier movement direction

5. Kame Terraces

  • Irregular mound-like deposits
  • Form along glacier sides

6. Kettle Holes

  • Depressions in the outwash plain
  • Formed due to the melting of buried ice blocks
  • May become kettle lakes

Glacial Cycle of Erosion

Youth

  • Cirque formation
  • Initial valley cutting
  • Aretes & horns developing

Maturity

  • Hanging valleys visible
  • The glacial trough is well developed
  • Stepped valley profile

Old Age

  • Fully developed U-shaped valley
  • Prominent depositional features
  • Outwash plain formation

Rapid Revision Table

Erosional

Depositional

Cirque

Moraine

Arete

Esker

Horn

Drumlin

U-shaped valley

Kame

Hanging valley

Kettle hole

Fjord

Outwash plain

 

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