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.