Notes For All Chapters – Geography Class 7
Soils
1. Introduction to Soil
- Soil is the uppermost layer of the Earth’s crust and is essential for plant growth.
- It is a mixture of weathered rock particles, minerals, organic matter (humus), air, and water.
- Soil formation is a long and slow natural process.
- Various factors influence soil formation, leading to different soil types across regions.
2. Factors Necessary for Soil Formation
Several factors contribute to soil formation:
(a) Parent Rock
The type of rock in a region determines the soil’s characteristics.
Rocks break down into smaller particles due to weathering.
Different parent rocks result in different soils:
- Basalt rock (found in Deccan Plateau) → Forms black soil (regur soil).
- Granite or gneiss rock (found in South India) → Forms red soil.
(b) Regional Climate
The climate (temperature, rainfall, humidity) affects weathering intensity and soil formation.
Example:
- Basalt rock in dry Deccan Plateau → Forms black soil.
- Basalt rock in humid Western Ghats → Forms lateritic soil due to heavy rainfall.
(c) Biotic Material (Organic Matter)
- Decomposed remains of plants and animals mix with weathered rock to form humus.
- Humus improves soil fertility.
- Microorganisms play a role in decomposing organic matter into nutrients.
- Organic composting techniques like vermicomposting help maintain soil health.
(d) Time
- Soil formation is a slow process and takes thousands of years.
- 2.5 cm of topsoil takes thousands of years to develop.
- Soil formation is faster in humid and warm regions compared to cold and dry areas.
3. Importance of Soil for Plants
Soil is essential for plant growth and provides:
- Nutrients for growth.
- Anchorage (support) for roots.
- Water retention for plant hydration.
Vegetation and soil fertility are interconnected:
- Equatorial regions (high rainfall) → Fertile soil → Dense forests.
- Deserts (dry regions) → Infertile soil → Sparse vegetation.
- Polar regions → Almost no soil → No vegetation.
4. Different Types of Soil in Maharashtra
Maharashtra has five major types of soil based on color, texture, formation process, and fertility.
(a) Coarse Soil
- Found in hilly areas like Ajanta, Balaghat, Mahadeo hills.
- Formed due to weathering and low rainfall.
- Contains low humus, making it less fertile.
(b) Black Soil (Regur Soil)
Found in Deccan Plateau and river valleys.
Two types:
- Dark black soil (Western Maharashtra) – Retains moisture well.
- Medium black soil (Vidarbha) – Less organic content.
Best for cotton, jowar, bajra cultivation.
(c) Laterite Soil
- Found in Konkan region & Vidarbha (high rainfall areas).
- Iron reacts with oxygen, giving it a red-orange color.
- Suitable for tea, coffee, and cashew nuts.
(d) Alluvial Soil (Coastal Region)
- Found near river mouths in Konkan.
- Formed by river deposits (sediments).
- Fertile and used for rice cultivation.
(e) Yellow-Brown Soil
- Found in Chandrapur, Bhandara, and Sahyadri mountains.
- Not very fertile, mainly used for forestry.
5. Soil Erosion and Degradation
(a) Soil Erosion
Definition: Removal of the top fertile layer of soil by wind or water.
Causes of soil erosion:
- Deforestation – Cutting down trees exposes soil to erosion.
- Overgrazing – Animals eat vegetation, leaving soil unprotected.
- Heavy rainfall and floods – Wash away the topsoil.
- Strong winds – Blow away loose soil particles.
(b) Soil Degradation
Definition: Reduction in soil fertility and productivity due to human activities.
Causes of soil degradation:
- Excessive use of chemical fertilizers & pesticides – Kills soil microorganisms.
- Over-irrigation – Leads to salinization (increased salt levels).
- Loss of organic matter – Reduces soil nutrients and humus content.
Effects of soil degradation:
- Reduced crop production.
- Decline in soil health.
6. Soil Conservation Methods
(a) Government Initiatives for Soil Conservation
- Watershed Development Programs – Construct embankments and trenches to stop erosion.
- Jalayukt Shivar Scheme – Water conservation and soil retention projects.
(b) Measures for Soil Conservation
- Afforestation (Tree Plantation) – Prevents wind erosion and holds soil in place.
- Contour Farming – Plowing across slopes to slow water runoff.
- Gully Plugging – Stopping small streams to prevent deep erosion.
- Organic Farming – Using natural manure instead of chemicals.
- Crop Rotation – Alternating crops to maintain soil fertility.
7. Geographic Indication (GI) of Soil-Based Crops
Some regions have specialized crops due to soil suitability.
Examples of GI Crops in Maharashtra:
- Hapus Mango (Sindhudurg)
- Nagpur Oranges
- Custard Apple (Beed)
- Basmati Rice (Dehradun)
8. Important Questions from the Chapter
(a) Why do the following occur?
- Laterite soil forms in the Western Ghats due to heavy rainfall.
- Humus content increases when organic material decomposes in soil.
- Soil formation is faster in equatorial climates due to high rainfall.
- Soil salinity increases due to over-irrigation.
- Rice is the staple diet in Konkan because of alluvial soil and heavy rainfall.
(b) Give information on:
- Measures of soil conservation (tree plantation, contour farming).
- Organic manures (compost, vermicompost).
- Finding soil suitability for crops (agriculture research centers).
- Importance of soil for plant growth (nutrients, support, water retention).
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