Volcanoes and Plate Tectonics

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Questions and Answers

What is a volcano?

A rupture in the Earth's crust where molten lava, ash, and gases escape into the air.

Who hypothesized the existence of the supercontinent Pangaea?

Alfred Wegener

What do the terms tectonicus and tektonikos mean?

  • To build (correct)
  • To compress
  • To separate
  • To destroy

How deep is the lithosphere?

<p>80 km deep</p> Signup and view all the answers

Which type of crust is thicker and less dense?

<p>Continental crust (A)</p> Signup and view all the answers

Majority of earthquake centers are located along plate margins.

<p>True (A)</p> Signup and view all the answers

What can cause earthquakes?

<p>Collisions, rifting, or slipping between plates.</p> Signup and view all the answers

What is the Pacific Ring of Fire known for?

<p>High volcanic activity (C)</p> Signup and view all the answers

What does the term 'volcanic arc' refer to?

<p>A series of volcanoes formed from magma.</p> Signup and view all the answers

Who led the Challenger expedition in 1872?

<p>Charles Wyville Thomson (D)</p> Signup and view all the answers

Plate tectonic theory explains the different processes that cause the formation of different geologic features and phenomena, including the formation of _____ and mountain belts.

<p>volcanoes</p> Signup and view all the answers

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Study Notes

Volcanoes and Plate Tectonics

  • Volcanoes are openings in the Earth's crust that allow molten lava, ash, and gases to escape.
  • Form at tectonic plate boundaries and hotspots, where geological activity is concentrated.

Learning Objectives

  • Define plate tectonic theory and its relationship to geological features.
  • Understand processes shaping the Earth’s crust, including volcanoes and earthquakes.
  • Explore methods to mitigate damage from geological phenomena.

Plate Tectonic Theory

  • Explains formation and movement of geologic features through tectonic processes.
  • Proposed by Alfred Wegener, who suggested all landmasses once formed a supercontinent called Pangaea.
  • Earth's lithosphere consists of tectonic plates that float and interact.

Structure of the Lithosphere

  • Lithosphere: Outermost layer combining the crust and upper mantle, approximately 80 km deep.
  • Crust: Composed of rocks and sediments, 50 km deep with a density around 2.6 g/cm³.
  • Two types of crust:
    • Continental crust: Thicker, less dense.
    • Oceanic crust: Denser, relatively thinner.

Types of Plates

  • Major Plates include North American, South American, Eurasian, Pacific, Indo-Australian, African, and Antarctic.
  • Smaller plates include Philippine, Caribbean, Cocos, Nazca, Scotia, Juan de Fuca, and Arabian plates.

Geological Processes

  • Most earthquakes occur along plate boundaries, with varying strengths from shallow to destructive.
  • Earthquakes can be triggered by plate collisions, rifting, or slip movements, releasing seismic waves.
  • Volcanoes predominantly located at plate margins and in subduction zones; categorized as active, dormant, or extinct.

Mountain Formation

  • Mountains arise from tectonic plate movements; some underwater, others on land.
  • Notable contributions from Charles Wyville Thomson, who discovered the Mid-Atlantic Ocean Ridge, and Harry H. Hess, a proponent of seafloor spreading.

Key Concepts

  • Primary and secondary seismic waves travel through Earth’s interior, while surface waves affect areas above ground.
  • Volcanic arcs formed from magma accumulation are mostly found in the Pacific Ring of Fire, highlighting the dynamic nature of Earth's surface.

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