Ocean Basins: Formation and Features
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Questions and Answers

Which geological process is primarily responsible for the creation of mid-ocean ridges?

  • Seafloor spreading at plate boundaries (correct)
  • Subduction of tectonic plates
  • Volcanic activity from mantle plumes
  • Continental weathering and erosion
  • In what order are the five major ocean basins typically listed, from largest to smallest?

  • Atlantic, Pacific, Indian, Arctic, Southern
  • Atlantic, Indian, Pacific, Southern, Arctic
  • Pacific, Indian, Atlantic, Arctic, Southern
  • Pacific, Atlantic, Indian, Southern, Arctic (correct)
  • What term describes the comprehensive mapping and study of the ocean floor's shape and features?

  • Oceanography
  • Bathymetry (correct)
  • Hydrology
  • Topography
  • Which of the following is NOT considered a primary feature found on the abyssal plain of an ocean basin?

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

    Besides seafloor spreading, what is another major plate tectonic activity responsible for the formation of many ocean basins?

    <p>Subduction (D)</p> Signup and view all the answers

    What geological process is primarily responsible for the initial formation of the Atlantic Ocean?

    <p>Tectonic plates pulling apart from each other. (B)</p> Signup and view all the answers

    Which characteristic primarily distinguishes an active continental margin from an inactive continental margin?

    <p>The presence of convergent plate boundaries and tectonic activity. (A)</p> Signup and view all the answers

    Abyssal plains in inactive ocean basins are largely formed due to the accumulation of which type of material?

    <p>Sedimentary deposits from continental drainage and marine organisms. (C)</p> Signup and view all the answers

    How does the rate of seafloor spreading affect the topography of an oceanic ridge?

    <p>Faster spreading results in gentler slopes and no rift valley. (C)</p> Signup and view all the answers

    What is the primary difference between a seamount and a guyot, both being types of inactive volcanoes?

    <p>Seamounts have jagged peaks, while guyots have flattened tops due to wave erosion. (D)</p> Signup and view all the answers

    Flashcards

    What is an Ocean Basin?

    A large, bowl-shaped depression in the Earth's surface that is filled with water, formed by geological processes.

    Continental Shelves

    The edges of ocean basins are called continental shelves. They are flat, shallow areas that extend from the coast.

    Continental Slope

    The steep slope that marks the transition from the continental shelf to the deep ocean floor.

    Seafloor Spreading

    A process where tectonic plates move apart, allowing magma to rise and form new ocean floor.

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    Mid-Ocean Ridges

    Large underwater mountain ranges formed by the upwelling of magma during seafloor spreading.

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    Oceanic Ridges

    A chain of underwater mountains formed by the spreading of tectonic plates. As the plates pull apart, volcanic eruptions bring basalt rock to the seafloor's surface. The Mid-Atlantic Ridge is an example of a slow-spreading ridge, with steep slopes and a rift valley. Faster spreading ridges, like the East Pacific Rise, have gentler slopes and no rift valley.

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    Abyssal Hill

    A small hill on the ocean floor, ranging in height from 985 to 3,200 feet. They are found between the abyssal plain and mid-oceanic ridge. Their size decreases with distance from the ridge due to sediment buildup.

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    Seamount

    An inactive volcano formed by lava rock solidified during past eruptions. Most seamounts are over 3,200 feet tall and remain submerged, but some can rise above the water's surface, like Mauna Kea. They play a crucial role in shaping ocean currents and provide habitats for various marine species.

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    Guyot

    A flattened, inactive volcano that once rose above the ocean's surface. Guyots have a flat top due to erosion from waves. They were eventually submerged by seafloor spreading. Guyots, like seamounts, provide habitats for marine life and influence ocean currents.

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    Ocean Trenches

    The deepest part of an active ocean basin. These steep, V-shaped trenches extend down into the Earth's mantle, trapping sediment that would otherwise cover the abyssal plain.

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    Study Notes

    Ocean Basins: Formation and Features

    • Ocean basins are bowl-shaped depressions formed by geological forces (weathering, erosion, plate tectonics)
    • Five major ocean basins: Pacific, Atlantic, Indian, Southern (Antarctic), Arctic
    • Collectively known as the world ocean, covering ~70% of Earth's surface
    • Smaller basins exist between larger ones (e.g., North Aleutian Basin)
    • Bathymetry describes the ocean floor's shape
    • Continental shelves, slopes, and rises form the basin's rim, declining to the abyssal plains
    • Abyssal plains contain oceanic ridges (abyssal hills, guyots, seamounts) and trenches
    • Oceanographers use submersibles to study deep trenches due to water pressure and cold temperatures

    Formation of Ocean Basins

    • Primarily formed by seafloor spreading and subduction
    • Seafloor spreading: Tectonic plates diverge, magma rises to form mid-ocean ridges, creating new ocean floor (e.g., Mid-Atlantic Ridge)
      • Atlantic Ocean is still expanding
    • Subduction: Tectonic plates collide, one slides under the other (forming trenches). Subduction causes ocean basins to shrink.
      • Pacific Ocean is shrinking

    Active vs. Inactive Basins

    • Active Basins: Marked by active plate tectonics, steep continental slopes, and deep trenches. Often convergent plate boundaries.
      • Example: Pacific Coast of North America
    • Inactive Basins: No convergent boundaries, passive continental margins. Transition from oceanic to continental crust. -Example: Gulf of Mexico
    • Inactive basins collect sediment from rivers, continental shelves, marine organisms, and volcanic ash, creating abyssal plains

    Ocean Basin Features

    • Oceanic Ridges: Underwater mountain chains, formed by seafloor spreading, volcanic eruptions, and basalt rock.
    • Abyssal Hills: Small hills on abyssal plains, smaller when farther from the ridge; marine life is similar to that of abyssal plains.
    • Seamounts: Inactive volcanoes rising from the seafloor, some above sea level (e.g., Mauna Kea). Habitats for various marine species.
    • Guyots: Inactive volcanoes with flattened tops due to wave erosion. Once above sea level. Homes to various marine species, and help nutrient circulation.
    • Ocean Trenches: Deepest parts of active ocean basins, V-shaped; trap sediment; highly pressured, dark environment, have specific marine life. Located along convergent plate boundaries (e.g., Marianas Trench, Challenger Deep).

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    Description

    Explore the fascinating world of ocean basins, including their formation, features, and the major oceanic divisions. This quiz delves into geological processes like seafloor spreading and subduction while highlighting the unique characteristics of each basin. Test your knowledge on how these underwater landscapes shape our planet's hydrology.

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