Natural Phenomenon

Natural Phenomenon

🌍 Earthquakes

πŸ”¬ Causes of Earthquakes

  • Tectonic Activity: Most earthquakes are caused by the sudden release of energy due to the movement of tectonic plates.
  • Volcanic Activity: Earthquakes can occur due to magma movement beneath the Earth’s surface.
  • Human Activity: Induced earthquakes can result from activities like mining, reservoir-induced seismicity, and hydraulic fracturing.
  • Faulting: Earthquakes occur when stress builds up along faults and is suddenly released.

πŸ“Š Types of Earthquakes

Type Description Example
Tectonic Earthquakes Caused by movement of tectonic plates San Francisco 1906
Volcanic Earthquakes Result from magma movement Mount St. Helens 1980
Collapse Earthquakes Due to cave collapses or landslides Not commonly recorded
Induced Earthquakes Caused by human activities Oklahoma (2016)

πŸ“ Measurement of Earthquakes

  • Richter Scale: Measures the magnitude of an earthquake based on the amplitude of seismic waves.
  • Moment Magnitude Scale (Mw): More accurate for large earthquakes, measures the total energy released.
  • Mercalli Scale: Qualitative scale based on observed effects.
  • Seismographs: Instruments used to record seismic waves.

πŸ“Œ Important Facts for Exams

  • Great Earthquake of 1906 (San Francisco): Magnitude 7.8 on the Richter scale.
  • Earthquake in Japan (2011): Magnitude 9.0, caused by the Pacific Plate and Eurasian Plate.
  • Earthquake in Nepal (2015): Magnitude 7.8, killed over 9,000 people.
  • Earthquake in India (2001): Gujarat earthquake, magnitude 7.7, killed over 20,000 people.

πŸŒ‹ Volcanoes

🧱 Types of Volcanoes

Type Description Example
Shield Volcanoes Broad, gently sloping shape Mauna Loa (Hawaii)
Stratovolcanoes (Composite Volcanoes) Steep, conical shape with explosive eruptions Mount Fuji (Japan), Mount Vesuvius (Italy)
Cinder Cone Volcanoes Small, steep-sided cones made of volcanic ash and cinders ParΓ­cutin (Mexico)
Lava Dome Volcanoes Formed by viscous lava extrusion Mount St. Helens (USA)
Caldera Volcanoes Large depressions formed by collapse Yellowstone Caldera (USA)

🌍 Distribution of Volcanoes

  • Ring of Fire: A major area of volcanic and seismic activity around the Pacific Ocean.
  • Mid-Atlantic Ridge: Active volcanic zone in the Atlantic Ocean.
  • Continental Volcanoes: Found in areas like the East African Rift Valley.
  • Hotspots: Volcanic activity not related to plate boundaries, e.g., Hawaii, Iceland.

πŸ§ͺ Effects of Volcanoes

  • Positive Effects:
    • Fertile soil due to volcanic ash.
    • Geothermal energy sources.
    • Tourism and economic benefits.
  • Negative Effects:
    • Lava flows, pyroclastic flows, and ashfall.
    • Volcanic gases (e.g., sulfur dioxide) can affect climate.
    • Ashfall can damage infrastructure and agriculture.

πŸ“Œ Important Facts for Exams

  • Mount Vesuvius (Italy): Erupted in 79 AD, destroyed Pompeii and Herculaneum.
  • Mount Fuji (Japan): Active stratovolcano, last eruption in 1707.
  • Mount St. Helens (USA): Erupted in 1980, one of the most destructive eruptions of the 20th century.
  • Mount Pinatubo (Philippines): Erupted in 1991, one of the largest eruptions of the 20th century.
  • Volcanic Winter: Eruption of large volcanoes can lead to global cooling due to atmospheric ash and sulfur dioxide.

🌍 Plate Tectonics

🧠 Theory Overview

  • Plate Tectonics Theory: Explains the movement of the Earth’s lithosphere, divided into tectonic plates.
  • Key Concepts:
    • Lithosphere: The rigid outer layer of the Earth.
    • Asthenosphere: The semi-fluid layer beneath the lithosphere.
    • Convection Currents: Heat from the Earth’s core drives the movement of tectonic plates.
    • Plate Boundaries: Divergent, convergent, and transform boundaries.

πŸ“Œ Types of Plate Boundaries

Boundary Type Description Example
Divergent Boundaries Plates move apart, creating new crust Mid-Atlantic Ridge
Convergent Boundaries Plates move towards each other, leading to subduction or collision Himalayas (India-Eurasia), Andes (South America)
Transform Boundaries Plates slide past each other San Andreas Fault (USA)

πŸ“Œ Important Facts for Exams

  • Continental Drift Theory (Alfred Wegener): Proposed in 1912, suggested continents were once joined.
  • Seafloor Spreading (Harry Hess): Proposed in 1960, explained the creation of new oceanic crust.
  • Plate Tectonics Theory (1960s): Unified the concept of continental drift and seafloor spreading.
  • Mid-Atlantic Ridge: A divergent boundary where new oceanic crust is formed.
  • Himalayas Formation: Result of the collision between the Indian and Eurasian plates (started ~55 million years ago).
  • San Andreas Fault: A transform boundary in California, responsible for frequent earthquakes.

πŸ“Œ Key Terms

  • Tectonic Plates: Large sections of the Earth’s lithosphere.
  • Subduction Zone: Area where one plate is forced under another.
  • Volcanic Arcs: Form along subduction zones.
  • Isostasy: The balance between the Earth’s crust and the mantle.
  • Hotspots: Areas of volcanic activity not related to plate boundaries.

πŸ“Œ Exam-Focused Summary

  • Plate Tectonics is the unifying theory of geology.
  • Divergent boundaries create new crust.
  • Convergent boundaries lead to mountain building and subduction.
  • Transform boundaries cause earthquakes.
  • Key examples: Himalayas, Mid-Atlantic Ridge, San Andreas Fault.