Atmosphere, Lithosphere and Hydrosphere

Atmosphere, Lithosphere and Hydrosphere

1. Atmosphere

1.1 Layers of the Atmosphere
LayerAltitude Range (km)Temperature TrendKey Features
Troposphere0 - 12Decreases with heightWeather occurs, Ozone layer present
Stratosphere12 - 50Increases with heightOzone layer, commercial aircraft fly here
Mesosphere50 - 85Decreases with heightColdest layer, meteors burn up
Thermosphere85 - 600Increases with heightIonosphere, auroras occur
Exosphere600 - 10,000Very low densityOutermost layer, fades into space
1.2 Composition of the Atmosphere
  • Nitrogen (78%): Most abundant gas
  • Oxygen (21%): Essential for respiration
  • Argon (0.93%): Inert gas
  • Carbon Dioxide (0.04%): Greenhouse gas, vital for photosynthesis
  • Other Gases (0.03%): Neon, helium, methane, water vapor, ozone, etc.
1.3 Important Terms and Concepts
  • Greenhouse Effect: Trapping of heat by CO₂ and other gases
  • Ozone Layer: Absorbs UV radiation, located in the stratosphere
  • Ionosphere: Layer in thermosphere that reflects radio waves
  • Auroras: Light displays caused by solar particles interacting with Earth’s magnetic field
1.4 Key Facts for Competitive Exams
  • The troposphere is the layer where weather occurs.
  • The stratosphere contains the ozone layer.
  • The thermosphere is where auroras and ionosphere are located.
  • Water vapor is a major component of the atmosphere and plays a key role in weather and climate.

2. Lithosphere

2.1 Components of the Lithosphere
  • Crust: Outermost layer, composed of rocks and minerals
    • Continental Crust: Thicker (30-70 km), granitic, less dense
    • Oceanic Crust: Thinner (5-10 km), basaltic, denser
  • Mantle: Beneath the crust, solid but can flow over long periods
    • Upper Mantle: Includes the asthenosphere, a semi-fluid layer
    • Lower Mantle: Solid, denser, under high pressure
  • Core: Center of the Earth
    • Outer Core: Liquid, composed mostly of iron and nickel
    • Inner Core: Solid, due to extreme pressure, composed of iron
2.2 Important Terms and Concepts
  • Plate Tectonics: Theory explaining the movement of Earth’s lithospheric plates
  • Seismic Waves: Used to study the interior of the Earth
  • Isostasy: Concept of balance between crust and mantle
  • Volcanoes and Earthquakes: Result of tectonic activity
2.3 Key Facts for Competitive Exams
  • The continental crust is thicker and less dense than the oceanic crust.
  • The asthenosphere is a semi-fluid layer in the upper mantle.
  • The outer core is liquid, while the inner core is solid.
  • Plate tectonics explains the formation of mountains, volcanoes, and earthquakes.

3. Hydrosphere

3.1 Water Bodies
Type of Water BodyDescription
OceansLargest reservoir of water, covers ~71% of Earth’s surface
SeasSmaller than oceans, partially enclosed by land
RiversFlowing water bodies, part of the water cycle
LakesStill water bodies, can be natural or artificial
GlaciersFrozen water bodies, store ~68% of Earth’s freshwater
GroundwaterWater stored in underground aquifers
Ice Caps and Ice SheetsStore large amounts of freshwater in polar regions
AtmosphereContains water vapor, part of the hydrological cycle
3.2 Water Cycle
  • Evaporation: Water from oceans, lakes, and land turns into vapor
  • Condensation: Vapor cools and forms clouds
  • Precipitation: Water falls as rain, snow, sleet, or hail
  • Runoff: Water flows over land into rivers and oceans
  • Infiltration: Water seeps into the ground to become groundwater
3.3 Important Terms and Concepts
  • Hydrological Cycle: Continuous movement of water on, above, and below Earth’s surface
  • Freshwater vs. Saltwater: Freshwater is less than 3% of Earth’s total water
  • Aquifers: Underground layers of water-bearing permeable rock
  • Transpiration: Evaporation of water from plants
3.4 Key Facts for Competitive Exams
  • Oceans contain 97% of Earth’s water.
  • Glaciers store ~68% of Earth’s freshwater.
  • The hydrological cycle is crucial for climate regulation and ecosystem sustainability.
  • Groundwater is a major source of freshwater for many regions.
  • Transpiration contributes to the water cycle and influences local climates.