Atmosphere, Lithosphere and Hydrosphere
Atmosphere, Lithosphere and Hydrosphere
1. Atmosphere
1.1 Layers of the Atmosphere
| Layer |
Altitude Range (km) |
Temperature Trend |
Key Features |
| Troposphere |
0 - 12 |
Decreases with height |
Weather occurs, Ozone layer present |
| Stratosphere |
12 - 50 |
Increases with height |
Ozone layer, commercial aircraft fly here |
| Mesosphere |
50 - 85 |
Decreases with height |
Coldest layer, meteors burn up |
| Thermosphere |
85 - 600 |
Increases with height |
Ionosphere, auroras occur |
| Exosphere |
600 - 10,000 |
Very low density |
Outermost 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 Body |
Description |
| Oceans |
Largest reservoir of water, covers ~71% of Earth’s surface |
| Seas |
Smaller than oceans, partially enclosed by land |
| Rivers |
Flowing water bodies, part of the water cycle |
| Lakes |
Still water bodies, can be natural or artificial |
| Glaciers |
Frozen water bodies, store ~68% of Earth’s freshwater |
| Groundwater |
Water stored in underground aquifers |
| Ice Caps and Ice Sheets |
Store large amounts of freshwater in polar regions |
| Atmosphere |
Contains 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.