The oceanic crust is mostly made up of different types of basalt which extends how many kilometres beneath the ocean floor?

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  1. 5-10 km
  2. 15-22 km
  3. 2-5 km
  4. 10-17 km

Answer (Detailed Solution Below)

Option 1 : 5-10 km
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The correct answer is 5-10 km.

Key Points

  • The oceanic crust is primarily composed of basalt, a dense, dark volcanic rock.
  • The thickness of the oceanic crust ranges from 5 to 10 kilometers beneath the ocean floor, depending on its age and location.
  • New oceanic crust is formed at mid-ocean ridges due to volcanic activity and spreads outward over time.
  • It is thinner and denser than the continental crust, which is mostly composed of granite and is around 30-50 km thick.
  • The oceanic crust is a crucial part of the Earth's lithosphere and plays a significant role in the plate tectonic cycle.

Additional Information

  • Basalt
    • Basalt is a volcanic igneous rock that makes up the majority of the oceanic crust.
    • It is rich in minerals like pyroxene, plagioclase, and olivine, and has a high density compared to continental crust rocks.
  • Mid-Ocean Ridges
    • These are underwater mountain ranges where new oceanic crust is formed due to tectonic plate divergence.
    • Examples include the Mid-Atlantic Ridge and the East Pacific Rise.
  • Plate Tectonics
    • The oceanic crust is part of the Earth's lithosphere, which is divided into tectonic plates.
    • Plates interact at boundaries, leading to processes like subduction, where oceanic crust is pushed beneath continental crust, recycling it into the mantle.
  • Oceanic vs. Continental Crust
    • Oceanic crust is thinner (5-10 km) but denser, while continental crust is thicker (30-50 km) but less dense.
    • The differences in composition and density play a key role in tectonic processes like subduction and mountain building.
  • Seafloor Spreading
    • The process by which new oceanic crust is created at mid-ocean ridges and spreads outward.
    • This phenomenon provides evidence for the theory of plate tectonics, as observed through magnetic patterns on the seafloor.
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