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Revision: Geography of India >> Soils in India Geography (English Medium) ICSE Class 10 CISCE

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Definitions [1]

Definition: Soil Erosion

The loss of soil or disturbance of the soil structure is called soil erosion.

Key Points

Key Points: Introduction to Soil in India
  • Soil is a thin layer of weathered rock and humus that supports life.
  • Soil forms slowly due to weathering, water, wind, and organic processes.
  • Humus increases soil fertility.
  • Soil erosion is caused by deforestation and overgrazing.
  • Soils are residual or transported (e.g., alluvial soil).
Key Points: Soil Formation and Factors Affecting It
  • Soil formation (pedogenesis) occurs due to disintegration and denudation of rocks.
  • Parent rock decides the type of soil, e.g. black soil from basalt rock.
  • Vegetation adds humus, increases fertility, and reduces soil erosion.
  • Climate controls the rate and type of weathering and decomposition.
  • Soils are of two types: Residual (zonal) soils formed in situ and Transported (azonal) soils like alluvial soil.
Key Points: Types of Soil > Alluvial Soil
  • Alluvial soil is formed by river deposits (alluvium) and is also called riverine soil.
  • It covers about 40% of India, mainly in the Northern Plains, coastal plains, and river deltas.
  • Alluvial soil is of two types: Bhangar (old, less fertile) and Khadar (new, very fertile).
  • It is a mixture of sand, silt, and clay (loam) and is rich in minerals like potash and lime.
  • It is suitable for crops like rice, wheat, sugarcane, cotton, jute, and oilseeds.
Key Points: Types of Soil > Black Soil
  • Black soil is also called Black Cotton soil or Regur soil and is formed from weathered volcanic (basalt) rocks.
  • It is an in-situ (residual) soil mainly found in the Deccan Plateau (Maharashtra, Gujarat, MP, Karnataka, Telangana).
  • This soil is fine-grained, clayey, and highly moisture-retentive, making it suitable for dry farming.
  • In dry season it develops deep cracks and is called self-ploughing soil, which helps maintain fertility.
  • It is rich in iron, lime, and potash but poor in nitrogen and humus, and is ideal for cotton, wheat, jowar, and oilseeds.
Key Points: Types of Soil > Red Soil
  • Red soil is formed by the weathering of ancient crystalline and metamorphic rocks and gets its red colour from iron oxide.
  • It is the second largest soil group in India, mainly found in the Peninsular Plateau (Tamil Nadu, Karnataka, Andhra Pradesh, Maharashtra, Odisha, Chhattisgarh, and parts of North-East India).
  • Red soil is porous, loose, and generally shallow, with low moisture-retention capacity.
  • It is poor in nitrogen, phosphorus, humus, and lime, but rich in potash, and responds well to irrigation and fertilizers.
  • It is suitable for dry farming and crops like rice, ragi, pulses, groundnut, tobacco, potatoes, and oilseeds.
Key Points: Types of Soil > Laterite Soils
  • Laterite soil is formed due to heavy rainfall and high temperature with alternate wet and dry periods, causing leaching (desilication).
  • It is a residual soil, red in colour due to iron oxide, and is acidic in nature.
  • Laterite soil is poor in nutrients like nitrogen, lime, humus, and magnesium, and has low moisture-retention capacity.
  • It is mainly found on the Western and Eastern Ghats and in parts of Kerala, Karnataka, Odisha, Maharashtra, Andhra Pradesh, and Tamil Nadu.
  • It is suitable for plantation crops like tea, coffee, rubber, cashewnut, and is also used as building material when hardened.
Key Points: Soil Erosion
  • Soil erosion is the removal of the top fertile layer of soil by water, wind, and human activities.
  • Soil erosion by water includes sheet erosion, rill erosion, gully erosion, leaching, sea erosion, and stream-bank erosion.
  • Wind erosion occurs in dry and semi-arid regions where loose soil is carried away by strong winds, reducing soil fertility.
  • Human activities such as deforestation, overgrazing, improper farming, and shifting cultivation greatly increase soil erosion.
  • Soil erosion reduces agricultural productivity, leads to land degradation, and creates a cycle of poverty.
Key Points: Causes of Soil Erosion
  • High population pressure on land leads to deforestation and overuse of land, which is a major cause of soil erosion in India.
  • Nature of rainfall in India—heavy monsoon rains and frequent droughts—causes floods and washing away of fertile topsoil.
  • Overgrazing by cattle removes vegetation cover, leaving soil exposed to wind and water erosion, especially in Rajasthan.
  • Bad farming practices like lack of terracing, contour ploughing, crop rotation, and improper use of manure increase soil erosion.
  • Steep slopes and deforestation in hilly regions such as the Shiwaliks, Himalayas, and parts of South India make these areas highly prone to soil erosion.
Key Points: Prevention of Soil Erosion
  • Terrace farming and contour ploughing reduce soil erosion on hilly slopes by slowing down running water.
  • Afforestation and shelter belts protect soil by holding soil particles, reducing wind speed, and increasing water percolation.
  • Strip cropping and crop rotation help prevent erosion by holding soil with crop roots and maintaining soil fertility.
  • Dams, embankments, and plugging of gullies control soil erosion caused by rivers and surface runoff.
  • Soil conservation is vital because soil forms very slowly, supports food production, biodiversity, and climate balance, and its loss leads to droughts, floods, and reduced fertility.
Key Points: Soil Conservation
  • Soil conservation means protecting soil from erosion and maintaining its fertility.
  • Soil erosion causes loss of fertile topsoil, leading to reduced agricultural productivity.
  • Soil conservation helps maintain soil moisture and raise the groundwater level.
  • It prevents silting of rivers, floods, droughts, and landslides, especially in hilly areas.
  • Soil conservation is essential because soil forms very slowly but can be destroyed quickly, and it supports plants, animals, and human life.
Key Points: Soil Conservation Schemes Initiated by the Government
  • The Government of India has started soil conservation schemes to reduce soil erosion and improve agricultural productivity.
  • Ravine reclamation programmes help control and reclaim ravine areas in Madhya Pradesh, Uttar Pradesh, and Rajasthan through bunding and plantation.
  • Shifting cultivation is controlled by resettling tribal people, increasing forest cover, and providing employment and food security schemes.
  • Rainwater harvesting reduces surface runoff, prevents soil erosion, raises the groundwater table, and supports multiple cropping.
  • Biofertilizers and the Integrated Watershed Management Programme (IWMP) improve soil fertility, conserve water and vegetation, and provide sustainable livelihoods.
Key Points: Alluvial Soil VS Black Soil VS Red Soil VS Laterite Soil
Soil Type Formation Main Areas Key Characteristics Major Crops
Alluvial Soil River deposits Northern Plains, coastal & delta regions Loamy, fertile, rich in potash & lime Rice, wheat, sugarcane, cotton, jute
Black Soil Weathering of lava rocks Deccan Plateau Clayey, moisture-retentive Cotton, cereals, sugarcane
Red Soil Weathering of crystalline rocks Peninsular Plateau Red due to iron, poor in nitrogen Rice, ragi, groundnut, vegetables
Laterite Soil Leaching due to heavy rainfall Western & Eastern Ghats Coarse, porous, acidic Tea, coffee, rubber, tapioca
Soils in India Vary by origin & climate Different regions Differ in fertility & texture Decide crop patterns
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