Landforms

Landforms

A.2.1] Mountains

Definition

Mountains are elevated landforms that rise prominently above the surrounding area, typically with steep slopes and a peak.

Types of Mountains

Type Description Formation
Fold Mountains Formed by the folding of rock layers due to tectonic compression Himalayas, Alps
Block Mountains Formed by the uplift and faulting of the Earth’s crust Sierra Nevada, Vosges
Volcanic Mountains Formed by the accumulation of volcanic material Mount Fuji, Mount Kilimanjaro
Dune Mountains Formed by wind deposition in arid regions Not a standard type; often confused with dunes

Formation Processes

  • Tectonic Activity: Folding, faulting, and compression
  • Volcanic Activity: Eruption and accumulation of lava and ash
  • Erosion and Uplift: Differential erosion of softer rocks

Key Facts (SSC, RRB)

  • Fold mountains are the most common type.
  • The Himalayas are the highest and youngest fold mountains.
  • Volcanic mountains are often found near tectonic plate boundaries.

A.2.2] Plateaus

Definition

Plateaus are flat-topped elevated landforms with steep slopes on at least one side.

Types of Plateaus

Type Description Formation
Volcanic Plateaus Formed by the solidification of lava flows Deccan Plateau, Columbia Plateau
Erosional Plateaus Formed by erosion of surrounding areas Tibetan Plateau
Residual Plateaus Form, due to differential erosion Chota Nagpur Plateau
Tectonic Plateaus Formed by uplift of the Earth’s crust Tibetan Plateau

Formation Processes

  • Volcanic Activity: Lava flows solidify to form flat surfaces
  • Erosion: Removal of surrounding material leaves elevated flat areas
  • Tectonic Uplift: Crustal movement raises the land

Key Facts (SSC, RRB)

  • The Deccan Plateau is a volcanic plateau formed during the Cretaceous period.
  • The Tibetan Plateau is the highest and largest plateau in the world.
  • Residual plateaus are often found in arid regions.

A.2.3] Plains

Definition

Plains are large, flat or gently undulating areas of land, typically lower in elevation.

Types of Plains

Type Description Formation
Alluvial Plains Formed by river deposition Indo-Gangetic Plain, North China Plain
Coastal Plains Formed by sea deposition Eastern Coastal Plain of India
Interior Plains Formed by erosion and deposition Great Plains of North America
Flood Plains Formed by periodic flooding Ganges-Brahmaputra flood plains

Formation Processes

  • River Deposition: Sediments carried by rivers settle to form alluvial plains
  • Marine Deposition: Sediments from the sea form coastal plains
  • Erosion and Weathering: Gradual leveling of landforms

Key Facts (SS. C, RRB)

  • The Indo-Gangetic Plain is the largest alluvial plain in the world.
  • Alluvial plains are highly fertile and important for agriculture.
  • Coastal plains are often associated with deltas and estuaries.

A.2.4] Glaciated Landforms

Definition

Glaciated landforms are features created by the movement and deposition of glaciers.

Types of Glaciated Landforms

Type Description Formation
U-shaped Valleys Formed by glacial erosion Yosemite Valley, Patagonia
Cirques Bowl-shaped depressions at the head of a valley Alps, Himalayas
Horns Sharp, pyramid-shaped peaks formed by glacial erosion Matterhorn, Pyramid Peak
Glaciers Large masses of ice that move slowly over land Greenland, Antarctica
Moraines Accumulations of rock debris deposited by glaciers Terminal, lateral, medial moraines

Formation Processes

  • Glacial Erosion: Abrasion and plucking of rock
  • Glacial Deposition: Sediment left behind as glaciers retreat

Key Facts (SSC, RRB)

  • U-shaped valleys are a hallmark of glacial activity.
  • The Alps and the Himalayas have significant glacial landforms.
  • Moraines are important indicators of past glacial activity.

A.2.5] Volcanic Landforms

Definition

Volcanic landforms are features created by volcanic activity, including eruptions, lava flows, and ash deposits.

Types of Volcanic Landforms

Type Description Formation
Volcanic Cone Cone-shaped hill formed by accumulated volcanic material Cinder cones, composite cones
Caldera Large depression formed by the collapse of a volcano Crater Lake, Yellowstone
Lava Plateaus Broad, flat areas formed by extensive lava flows Deccan Plateau, Columbia Plateau
Volcanic Domes Rounded hills formed by viscous lava Mount St. Helens
Fissure Plains Flat areas formed by fissure eruptions Iceland

Formation Processes

  • Lava Eruptions: Magma extrusion and solidification
  • Ash and Tephra Deposition: Accumulation of volcanic debris
  • Volcanic Collapse: Formation of calderas

Key Facts (SSC, RRB)

  • The Deccan Plateau is a volcanic plateau formed during the Cretaceous period.
  • Composite volcanoes are also known as stratovolcanoes.
  • Calderas are often associated with explosive eruptions.

A.2.6] Desert Landforms

Definition

Desert landforms are features created by wind erosion and deposition in arid regions.

Types of Desert Landforms

Type Description Formation
Dunes Mounds of sand formed by wind Barchan, transverse, linear dunes
Yardangs Ridge-like features formed by wind erosion Central Asia
Deflation Basins Depressions formed by removal of loose sediments Sahara Desert
Inselbergs Isolated hills or mountains in a desert Namib Desert
Alluvial Fans Fan-shaped deposits at the base of mountains Desert margins

Formation Processes

  • Wind Erosion: Abrasion and deflation of loose sediments
  • Wind Deposition: Accumulation of sand and dust

Key Facts (SSC, RRB)

  • Barchan dunes are the most common type of dune in deserts.
  • Yardangs are often found in arid regions with strong winds.
  • Inselbergs are remnants of ancient mountains.

A.2.7] Riverine Landforms

Definition

Riverine landforms are features created by the action of rivers, including erosion, transportation, and deposition.

Types of Riverine Landforms

Type Description Formation
V-shaped Valleys Formed by river erosion Young rivers
Flood Plains Flat areas formed by periodic flooding Ganges-Brahmaputra
Meanders Curved bends in a river Mature rivers
Oxbow Lakes Lake formed by the cutoff of a meander Mature rivers
Deltas Fan-shaped deposits at the mouth of a river Ganges Delta
Alluvial Fans Fan-shaped deposits at the base of mountains Desert margins

Formation Processes

  • Erosion: Cutting through rock and soil
  • Transportation: Movement of sediments by water
  • Deposition: Accumulation of sediments in low-energy areas

Key Facts (SSC, RRB)

  • Meanders are common in mature rivers.
  • Deltas are highly fertile and support agriculture.
  • Flood plains are important for agriculture and human settlement.