Plate tectonics - Hess's Model, Seafloor Spreading, Continental Drift

plate tectonics

Table of Contents

Introduction & Top Questions
Principles of plate tectonics
- Earth’s layers
- Plate boundaries
  - Divergent margins
    - Continental rifting
    - Seafloor spreading
  - Convergent margins
    - Subduction zones
    - Island arcs
    - Back-arc basins
    - Mountain building
      Mountains by subduction
      Mountains by terrane accretion
      Mountains by continental collision
  - Transform faults
- Hotspots
- Plate motion
  - Euler’s contributions
  - Past plate movements
Development of tectonic theory
- Precursors
- Alfred Wegener and the concept of continental drift
  - Isostasy
  - Driving forces
  - Evidence supporting the hypothesis
  - Disbelief and opposition
- Renewed interest in continental drift
  - Paleomagnetism, polar wandering, and continental drift
  - Gestation and birth of plate-tectonic theory
    - Discovery of ocean basin features
    - Hess’s seafloor-spreading model
    - The Vine-Matthews hypothesis
      Magnetic anomalies
      Reversal of Earth’s magnetic field
- Toward a unifying theory
  - Determination of plate thickness
  - Plate-driving mechanisms and the role of the mantle
    - Mantle convection
    - Seismic tomography
- Dissenting opinions and unanswered questions
  - Dissenters
  - Unanswered questions
Plate tectonics and the geologic past
- Wilson cycle
- Supercontinent cycle
- Continental reconstructions
Interactions of tectonics with other systems
- Oceans
  - Sea level
  - Composition of ocean water
- Life
  - Evolution
  - Extinction
- Climate

References & Edit History Related Topics

Images & Videos

What is the theory of continental drift?

How does plate tectonics change Earth's surface?

rift valley in Thingvellir National Park

For Students

plate tectonics summary

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The existence of these three types of large, striking seafloor features demanded a global rather than local tectonic explanation. The first comprehensive attempt at such an explanation was made by Harry H. Hess of the United States in a widely circulated manuscript written in 1960 but not formally published for several years. In this paper, Hess, drawing on Holmes’s model of convective flow in the mantle, suggested that the oceanic ridges were the surface expressions of rising and diverging convective mantle flow, while trenches and Wadati-Benioff zones, with their associated island arcs, marked descending limbs. At the ridge crests, new ...(100 of 15632 words)

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