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Geosphere (Lithosphere)
Provides minerals from weathered rock.
Atmosphere
Supplies gases (oxygen, COā, nitrogen) for soil chemistry.
Hydrosphere
Adds water for chemical reactions, transport of nutrients.
Biosphere
Contributes organic material from decomposing plants/animals.
Good Soil
Contains minerals that provide nutrients like iron, calcium, potassium.
Organic Matter
Improves fertility, structure, and moisture retention.
Water & Air
Needed for root respiration, chemical reactions, and microbial life.
Residual Soil
Forms in place, directly from weathered bedrock.
Transported Soil
Moved by wind, water, ice, or gravity before settling (e.g., floodplains, dunes).
Warm, wet climates
Lead to faster weathering and deep soils rich in clay & leached nutrients.
Cool, dry climates
Result in slower weathering and thinner soils with more organic matter accumulation.
Extreme rain (tropical climates)
Produces laterite soils, heavily leached and poor in nutrients.
O-Horizon (Organic Layer)
Contains decomposing leaves, plants, and organisms; dark and nutrient-rich.
A-Horizon (Topsoil)
Mineral-rich layer mixed with organic matter, crucial for plant growth.
E-Horizon (Eluviation/Leaching Layer)
Minerals like iron, aluminum, and clay are leached out by water; lighter in color.
B-Horizon (Subsoil/Accumulation Layer)
Clay, minerals, and nutrients accumulate from the E-horizon; denser and harder than topsoil.
C-Horizon (Weathered Parent Material)
Partially broken-down bedrock with little biological activity.
Parent Material (Bedrock or Unweathered Rock)
The original rock that the soil developed from.
Chemical weathering
Can concentrate valuable minerals, forming ore deposits.
Bauxite
An aluminum ore that forms in tropical climates.
Gold & copper deposits
Can form from hydrothermal solutions.
Soil Erosion
Loss of topsoil reduces fertility and plant growth.
Human activities
Like deforestation, overgrazing, and farming accelerate erosion.
Solutions to soil erosion
Include contour plowing, windbreaks, cover crops, and no-till farming.