Continental Margins Quiz
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Questions and Answers

What is the primary composition of the Earth's core?

  • Largely composed of lithosphere and asthenosphere.
  • Predominantly solid rock and magma.
  • Primarily basalt and granite.
  • Mainly iron and nickel. (correct)

Which layer of the Earth constitutes the largest percentage of its volume?

  • The inner core.
  • The outer core.
  • The crust.
  • The mantle. (correct)

What type of rock primarily makes up oceanic plates?

  • Limestone.
  • Basalt. (correct)
  • Granite.
  • Sandstone.

The movement of tectonic plates is LEAST likely to directly cause which of the following?

<p>Changes in atmospheric pressure. (A)</p> Signup and view all the answers

Continental margins are best described as areas where:

<p>Continental crust meets oceanic crust. (D)</p> Signup and view all the answers

Which geological process is primarily responsible for the formation of deep ocean trenches at active continental margins?

<p>Subduction of oceanic plates beneath continental plates. (C)</p> Signup and view all the answers

What is a distinguishing feature of passive continental margins in terms of their continental shelves?

<p>Wide and gradually sloping away from the coastline. (C)</p> Signup and view all the answers

How do sea canyons found at passive margins primarily differ in their formation from ocean trenches at active margins?

<p>Sea canyons are results of underwater erosion, while ocean trenches are from tectonic subduction. (B)</p> Signup and view all the answers

The Andes Mountains, located along the west coast of South America, are a direct result of which type of continental margin?

<p>Active continental margin, due to the subduction of the Pacific Plate. (C)</p> Signup and view all the answers

What is the primary reason for the relatively uniform and flat inland geography associated with passive continental margins?

<p>Absence of significant tectonic uplift, allowing erosion to flatten the land over time. (A)</p> Signup and view all the answers

Flashcards

Continental Margins

The area where the Earth's continents meet the ocean floor, a boundary between different types of rocks.

Earth's Crust

The outermost layer of the Earth, made up of tectonic plates.

Tectonic Plates

Large, rigid pieces of the Earth's lithosphere that move slowly over the surface, causing tectonic activity.

Active Continental Margins

Continental margins characterized by active geological processes such as earthquakes and volcanic activity.

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Passive Continental Margins

Continental margins where tectonic plates are not interacting, resulting in less geological activity.

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Subduction Zone

A zone where an oceanic plate slides beneath a continental plate, causing volcanic activity and earthquakes.

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Oceanic Trench

A deep, narrow depression in the ocean floor formed at the boundary of an active continental margin.

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Continental Shelf

A shallow, submerged area extending from the coastline towards the ocean, typically wider and shallower at passive margins.

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Study Notes

Continental Margins

  • Continental margins are where continental rocks meet oceanic rocks at the edges of tectonic plates.
  • Earth's layers include the core (inner and outer), mantle, and crust.
  • The crust consists of the lithosphere (tectonic plates) and asthenosphere.
  • Tectonic plates move slowly, causing earthquakes, volcanoes, mountain building, and ocean formation.
  • Two types of plates exist:
    • Oceanic plates: dense, young, composed of basalt.
    • Continental plates: less dense, older, composed of granite.
  • Plate movements (convergent, divergent, parallel) influence continental margin types.

Active Continental Margins

  • Occur where continental and oceanic plates collide.
  • Oceanic plates are denser, subducting beneath continental plates.
  • Features of active margins:
    • Varied inland geography: mountain ranges, sea cliffs, short rivers.
    • Subduction zones: oceanic crust melts, creating magma.
    • Narrow continental shelf.
    • Ocean trenches.
    • Volcanic and earthquake activity.
  • Examples:
    • Western coasts of North and South America (e.g. Andes Mountains, Cascades).
    • East and Southeast Asia (e.g. Marianas Trench).
    • Ring of Fire: high volcanic activity around the Pacific.

Passive Continental Margins

  • Occur where continental and oceanic plates don't collide.
  • Lack of significant tectonic activity.
  • Features of passive margins:
    • More uniform inland geography: flat plains, long rivers, estuaries.
    • Wide continental shelf.
    • Estuaries where rivers meet the ocean.
    • Sea canyons: underwater erosion perpendicular to the coast.
  • Examples:
    • Eastern coast of North and South America.
    • Africa, Antarctica, Australia (lack of seismic activity).
    • Amazon, Congo, Nile, and Ganges Rivers.

Emergent and Submergent Coasts

  • Emergent coasts: formed when the crust rises (active margins, rocky coastlines).
  • Submergent coasts: formed when sea levels rise or crust sinks (wider river valleys).
  • Both types relate to isostatic equilibrium (balance between the Earth’s lithosphere and asthenosphere).

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Test your knowledge on continental margins, including the characteristics and differences between active and passive margins. Explore how tectonic plate movements shape our planet's geography and features like ocean trenches and subduction zones.

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