In areas getting more than 200cms of annual rainfall, which type of so...
Intensive leaching is the primary explanation for the formation of laterite soils. Owing to heavy tropical rainfall more than 200 cms and high temperatures, leaching occurs.
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In areas getting more than 200cms of annual rainfall, which type of so...
Intensive leaching is the primary explanation for the formation of laterite soils. Owing to heavy tropical rainfall more than 200 cms and high temperatures, leaching occurs. Lime and silica are leached away as a result of high precipitation, and soils rich in iron oxide and aluminium compounds are left behind. The correct answer is laterite soil.
In areas getting more than 200cms of annual rainfall, which type of so...
Type of Soil in Areas Getting More Than 200cms of Annual Rainfall
The correct answer to this question is option 'C', which is laterite soil. Let's understand why.
Definition of Laterite Soil
Laterite soil is a type of soil that is found in the tropical regions of the world. It is formed by the weathering of rocks and minerals, and it is characterized by its high iron and aluminum content.
Factors Affecting the Formation of Laterite Soil
The formation of laterite soil is influenced by several factors, including:
- High temperature and humidity
- Heavy rainfall
- Poor drainage
- High levels of iron and aluminum in the rocks and minerals
Characteristics of Laterite Soil
Laterite soil has several unique characteristics, including:
- It is rich in iron and aluminum
- It is highly porous and well-drained
- It is acidic in nature
- It is low in fertility
- It is reddish-brown in color
Distribution of Laterite Soil
Laterite soil is found in areas that receive more than 200cms of annual rainfall. It is most commonly found in the tropical regions of the world, including:
- India
- Southeast Asia
- Africa
- South America
Conclusion
In conclusion, laterite soil is the type of soil that is found in areas receiving more than 200cms of annual rainfall. It is characterized by its high iron and aluminum content, porosity, acidity, low fertility, and reddish-brown color.
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