Factors That Influence Soil Formation in Indian Conditions: Parent Material

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Soil formation in Indian Conditions – Factors that influence soil formation: Parent Material
– Gondwana rocks & Deccan basalts, Relief, Climate & Natural Vegetation.
Factors that influence soil formation in Indian Conditions
 Parent Material
 Relief
 Climate
 Natural Vegetation
Parent Material
 The rocks from which soils are formed are called parent materials.
 In most of the cases, the parent material determines the colouration, mineral
composition and texture of the soil.
 In some cases, the soil formed may or may not have the same physical properties of
the parent rock.
 Climatic factors induce chemical changes which also affect physical properties of the
soil.
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 The surface rocks are exposed to the process of weathering. In this process, the rocks
are converted into fine grains and provide a base for the soil formation.
 In Indian Conditions, parent material is generally categorized into:
1. Ancient crystalline and metamorphic rocks
2. Cuddapah and Vindhyan rocks
3. Gondwana rocks
4. Deccan basalts
5. Tertiary and Mesozoic sedimentary rocks of extra peninsular India {Rock
System}
Ancient crystalline and metamorphic rocks
 They are the Oldest rocks [(pre-Cambrian era)(formed due to solidification of molten
magma about 4billion years ago)].
 They form the ‘Basement Complex’ of peninsular India.
 They are basically granites, gniesses and schists.
 These rocks are rich in ferromagnetic materials and give rise to red soils on
weathering.
 The red colour of these soils is due to the presence of iron oxide.
Cuddapah and Vindhyan rocks
 They are ancient sedimentary rocks (4000 m thick).

 On weathering they give calcareous [containing calcium carbonate; chalky ] and argillaceous
[consisting of or containing clay] soils.
 The soil is mostly devoid of metalliferous minerals.
Gondwana rocks
 These rocks are also sedimentary in nature and they are much younger.
 On weathering they give rise to comparatively less mature soils.
 The soil is more or less of uniform character but of low fertility.
Deccan basalts
 Volcanic outburst over a vast area of the Peninsular India many hundred million
years ago gave rise to Deccan Traps.
 Basaltic lava flowed out of fissures covering a vast area of about ten lakh sq km.
 Basalts are rich in titanium, magnetite, aluminium and magnesium.

 Consequently the weathering of these rocks has given rise to soils of darker colour.
 The is fertile with high moisture holding capacity and is popularly known as
‘regur’ or black cotton soil.
Tertiary and Mesozoic sedimentary rocks
 Rocks of extra peninsular (plains and Himalayas) India have given rise to soils with
high porosity.
 These soils are generally immature recent and sub recent rocks, result in alluvial
soils on weathering.
 Alluvial fertile soils consist of fine silts and clay. These soils have little relation with
the original rocks.
 On the other hand, the soils of peninsular plateau are generally coarse-grained and
are closely related to the parent rocks. The peninsular soils are generally less fertile.
Relief
 The relief is the most important factor for soil formation in places with steep slopes
like the hilly regions, edges of plateaus etc.
 Soil erosion on barren slopes is rampant and it hinders soil formation. Example:
Chambal ravines, higher reaches of Himalayas where there is minimal or no forest
cover (most on the steep southern slopes) etc.
 The areas of low relief or gentle slope generally experience deposition and have deep
soils. Example: Indo-Gangetic plain.
 The exceptions in the plateau are river basins where the soil layers are sufficiently
deep.
Climate
 Temperature and rainfall are the most important factors in soil formation.
 They determine the effectiveness of weathering of the parent material, the quantity of
water seeping through the soil and the type of micro-organisms present therein.
 Two different parent materials may develop the same soil in the same type of climate.
Similarly, the same parent material may produce two different types of soils in two
different types of climates.
 The crystalline granites produce laterite soil in relatively moist parts of the
monsoonal region and non-laterite soil in drier areas.
 Hot summer and low rainfall develops black soil as is found in some parts of
Tamil Nadu irrespective of the parent rock.
 In Rajasthan, both granite and sandstone give birth to sandy soil under arid
climate.
 In arid and semi-arid regions, evaporation always exceeds precipitation. There is little
vegetation and the soils badly lack humus content. Hence the soils are invariably of
light colour.
 In Rajasthan and the adjoining arid and semi-arid regions, excess of evaporation
makes soils lime accumulating. Hence the soil is pedocal in nature [Pedocal is a
subdivision of the zonal soil order. It is a class of soil which forms in semiarid and
arid regions. It is rich in calcium carbonate and has low soil organic matter].
 In cold climates of the Himalayan region, the process of vegetation decay is very
slow and the soils are acidic in nature.
In areas of heavy rainfall and high temperature, the soils are red or lateritic. Why?
 Torrential rainfall during the rainy season washes the upper soil and leaches the
materials into deeper horizon.
 During the dry summer season the evaporation exceeds precipitation and through
capillary action iron and aluminium oxides are transported to the surface making
the soil red.
 In areas of alternate wet and dry climate, the leached material which goes deep down
in the horizon is brought up and the blazing sun bakes the top soil so hard that it
resembles a brick. Therefore, this soil is called lateritic which literally means
brick.
Natural Vegetation
 Natural vegetation reflects the combined effects of relief and climate.
 The formation and development of soil is very much influenced by the growth of
vegetation.
 The decayed leaf material adds much needed humus to soil thereby increasing its
fertility.
 The densely forested areas contain some of the best soils in India. There is a close
relationship between the vegetation types and soil types in India.

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Factors that influence soil formation in Indian Conditions

Ancient crystalline and metamorphic rocks

Cuddapah and Vindhyan rocks

 They are ancient sedimentary rocks (4000 m thick).

 Basalts are rich in titanium, magnetite, aluminium and magnesium.

Tertiary and Mesozoic sedimentary rocks

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