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Understanding Volcanoes, Earthquakes, and Mountains

Apr 23, 2025

Volcanoes, Earthquakes, and Mountain Ranges

Introduction

  • Welcome to the lesson on volcanoes, earthquakes, and mountain ranges.
  • The goal is to describe and relate the distribution of active volcanoes, earthquake epicenters, and major mountain belts to plate tectonics.

Earth's Structure

  • Earth is composed of four layers:
    • Crust
    • Mantle
    • Outer Core
    • Inner Core
  • Two main types of Earth's crust:
    • Continental Crust: Thick (30-50 km), forms continents.
    • Oceanic Crust: Thin (5-10 km), denser, forms ocean floors.

Lithosphere and Tectonic Plates

  • Lithosphere: Outermost layer including the crust and upper mantle.
  • Lithosphere broken into tectonic plates, akin to a cracked eggshell.
  • Tectonic plates are in constant, slow motion:
    • Move apart
    • Push together
    • Slide past each other
  • Plate movement caused by mantle heat currents.

Geological Features and Events

  • Mountains: Form when plates collide.
  • Volcanoes: Created through subduction, when one plate dives under another.
  • Earthquakes: Result from plates sliding past or colliding.

Plate Tectonics

  • Drives the movement of Earth's plates, shaping Earth's surface and causing geological events.
  • Ring of Fire: A major area in the Pacific with frequent earthquakes and volcanic eruptions.

Philippines and Tectonic Plates

  • Philippines located in a tectonically active region (Ring of Fire).
  • Influenced by several tectonic plates:
    • Philippine Sea Plate: East, causes earthquakes and volcanoes.
    • Eurasian Plate: Northwest, interacts with Philippine Sea Plate.
    • Pacific Plate: Further east, influences seismic activity.
    • Sunda Plate: Southwest, affects southern Philippines.

Conclusion

  • Summary of key ideas:
    • Lithosphere consists of crust and upper mantle, divided into plates.
    • Two crust types: continental (thicker) and oceanic (denser).
    • Plate tectonics theory explains Earth's crust movement, causing earthquakes, volcanoes, and mountains.
    • Plate interactions are concentrated near edges of continents, leading to seismic and volcanic activity.
  • Upcoming topic: Plate boundaries.