Earth's Interior and Surface Contrasts

From the study guide

Course Outline

  1. Earth Surface Contrasts
  2. Crust Composition
  3. Continental Crust Rocks
  4. Oceanic Crust Rocks
  5. Internal Earth Structure
  6. Seismic Wave Propagation
  7. Discontinuities in Earth
  8. Thermal Structure Models
  9. Heat Transfer Modes
  10. Thermal Anomalies

1. Earth Surface Contrasts

Key Concepts & Definitions

  • Bimodal Altitude Distribution: The presence of two distinct altitude peaks representing oceanic (-4500 m average) and continental (+300 m average) domains, indicating a clear geological contrast (source content).
  • Crustal Composition (Continent vs Ocean): The continental crust primarily consists of granite (rich in SiO2 and K, with a density of ~2.7), while oceanic crust is mainly basalt and gabbro (low in SiO2 and K, dense ~2.9), reflecting different mineralogical and chemical properties (source content).
  • Discontinuity of Mohorovicic (Moho): The boundary separating the crust from the mantle, characterized by a sudden increase in seismic wave velocities, with variable depth (~7 km under oceans, ~30 km under continents) (source content).
  • Discontinuity of Gutenberg: The seismic boundary at approximately 2900 km depth, separating the mantle from the liquid outer core, evidenced by the shadow zone where P and S waves are absent or refracted (source content).
  • Low Velocity Zone (LVZ): A ductile, deformable layer in the upper mantle between 100-200 km depth where seismic wave velocities decrease,…
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Practice quiz preview

1. What does the bimodal altitude distribution of Earth's surface represent?

2. What are the main rocks that compose the oceanic crust?

3. What is the primary role of continental crust rocks like granite in Earth's geology?

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Flashcard preview

Bimodal Altitude Distribution β€” definition?

Two distinct peaks: oceanic (-4500 m) and continental (+300 m).

Crust composition β€” continental rocks?

Primarily granite, silica-rich, coarse-grained, ~2.7 density.

Crust composition β€” oceanic rocks?

Mainly basalt and gabbro, mafic, denser (~2.9), fine- to coarse-grained.

Moho discontinuity β€” role?

Separates crust from mantle, marked by seismic velocity increase.

Gutenberg discontinuity β€” depth?

Approximately 2900 km, separates mantle from outer core.

Lehmann discontinuity β€” significance?

Divides outer liquid core from inner solid core at ~5100 km.

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Frequently asked questions

What does the Earth's Interior and Surface Contrasts study guide cover?

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The practice quiz has 10 multiple-choice questions, each with an explanation. Use it to check what you know and find your gaps.

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