Lithosphere -- Environmental Sciences


Internal structure of the Earth

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Internal Structure of the Earth

The Earth's internal structure is divided into several layers:

  1. Crust:

    • Continental Crust: Thicker and less dense, composed mostly of granite.
    • Oceanic Crust: Thinner and more dense, composed mostly of basalt.
    • The crust is the outermost layer and is where we live. It varies in thickness from about 5 km (under the oceans) to about 70 km (under continents).
  2. Mantle:

    • Comprises about 84% of Earth's volume.
    • Divided into the upper mantle and lower mantle.
    • Composed of silicate minerals that are rich in magnesium and iron.
    • The upper mantle includes the asthenosphere, which is semi-fluid and allows tectonic plates to move.
  3. Core:

    • Outer Core: Liquid layer composed mainly of iron and nickel. It creates Earth's magnetic field through its movement.
    • Inner Core: Solid, due to the immense pressures, composed primarily of iron and nickel. It is the hottest part of the Earth.

Rock Types

Rocks are classified based on their formation processes:

  1. Igneous Rocks:

    • Formed from the cooling and solidification of magma or lava.
    • Intrusive Igneous Rocks: Formed from magma that cools slowly beneath the Earth’s surface (e.g., granite).
    • Extrusive Igneous Rocks: Formed from lava that cools quickly on the Earth’s surface (e.g., basalt).
  2. Sedimentary Rocks:

    • Formed from the accumulation and lithification of sediments.
    • Often contain fossils and are usually layered.
    • Examples include sandstone, limestone, and shale.
  3. Metamorphic Rocks:

    • Formed from existing rocks that are subjected to heat and pressure, causing physical and chemical changes.
    • Examples include slate (from shale), marble (from limestone), and gneiss (from granite).

Soil

Soil is a natural resource composed of mineral particles, organic matter, water, and air. It forms through the weathering of rocks and the decay of organic material over time. Key aspects of soil include:

  1. Soil Horizons:

    • O Horizon: Organic layer composed of decomposed leaves and organic material.
    • A Horizon (Topsoil): Rich in organic material and minerals, crucial for plant growth.
    • B Horizon (Subsoil): Accumulates minerals leached from the topsoil and contains more clay.
    • C Horizon: Consists of weathered parent material.
    • R Horizon: Unweathered bedrock.
  2. Soil Composition:

    • Mineral Particles: Derived from the breakdown of rocks; classified into sand, silt, and clay based on size.
    • Organic Matter: Decomposed plant and animal material that enriches the soil.
    • Water and Air: Fill the spaces between soil particles and are essential for soil health and plant growth.
  3. Soil Types:

    • Sandy Soil: Drains quickly but has low nutrient retention.
    • Clay Soil: High nutrient content but poor drainage.
    • Loamy Soil: Balanced mixture of sand, silt, and clay; ideal for agriculture.

Solid Waste

What is solid waste?

Solid waste is the type of waste which is, well, solid in nature (duh).

Types of solid wastes


Recovery and Disposal methods


Solid Waste Management and Control