Seafloor Spreading: Key Process in Earth’s Crust Dynamics

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Question No. 23: The process that continually adds new crust is
(A) subduction
(B) earthquake
(C) seafloor spreading
(D) convection Correct

Answer: (C) seafloor spreading


Explanation in Simple Sentences:

  • Option (A) – Subduction: Subduction is when one tectonic plate slides under another, recycling crust into the mantle. It destroys crust, not adds it. This is incorrect.
  • Option (B) – Earthquake: Earthquakes are sudden movements of tectonic plates causing ground shaking. They don’t create new crust. This is incorrect.
  • Option (C) – Seafloor spreading: Seafloor spreading happens at mid-ocean ridges where tectonic plates move apart. Magma rises, cools, and forms new oceanic crust. This is correct.
  • Option (D) – Convection: Convection is the movement of molten material in the mantle, driving plate tectonics. It supports seafloor spreading but doesn’t directly add crust. This is incorrect.

Reason: Seafloor spreading creates new oceanic crust as magma rises at mid-ocean ridges, cools, and solidifies, continually adding to the Earth’s crust. Option (C) is the correct answer.


Key Terms Explained:

  • Crust: The Earth’s outermost solid layer, made of oceanic (thinner, denser) and continental (thicker, less dense) crust.
  • Seafloor Spreading: A process at mid-ocean ridges where tectonic plates diverge, allowing magma to rise and form new oceanic crust.
  • Subduction: The process where one tectonic plate is forced under another, sinking into the mantle, recycling crust.
  • Earthquake: A sudden release of energy in the Earth’s crust, causing ground shaking, often along plate boundaries.
  • Convection: The circular movement of molten rock in the mantle due to heat, driving tectonic plate movement.
  • Tectonic Plates: Large, rigid pieces of the Earth’s crust and upper mantle that move and interact, causing geological activity.
  • Magma: Molten rock beneath the Earth’s surface that forms new crust when it cools during seafloor spreading.
  • Mid-Ocean Ridge: An underwater mountain range where tectonic plates diverge, and new crust forms via seafloor spreading.

Five Probable Questions of Similar Difficulty

  1. Question: What forms new oceanic crust at mid-ocean ridges?
    (A) Subduction
    (B) Seafloor spreading
    (C) Earthquakes
    (D) Volcanic eruptions
    Answer: (B) Seafloor spreading
    Explanation: Seafloor spreading at mid-ocean ridges allows magma to rise and solidify, forming new oceanic crust.
  2. Question: Which process recycles Earth’s crust back into the mantle?
    (A) Seafloor spreading
    (B) Convection
    (C) Subduction
    (D) Faulting
    Answer: (C) Subduction
    Explanation: Subduction occurs when a tectonic plate sinks under another, melting into the mantle.
  3. Question: What drives the movement of tectonic plates?
    (A) Earthquakes
    (B) Magma cooling
    (C) Convection in the mantle
    (D) Crust formation
    Answer: (C) Convection in the mantle
    Explanation: Convection currents in the mantle move tectonic plates, enabling processes like seafloor spreading.
  4. Question: Where does seafloor spreading primarily occur?
    (A) Continental margins
    (B) Mid-ocean ridges
    (C) Subduction zones
    (D) Fault lines
    Answer: (B) Mid-ocean ridges
    Explanation: Mid-ocean ridges are divergent plate boundaries where new crust forms via seafloor spreading.
  5. Question: What is a result of seafloor spreading?
    (A) Destruction of crust
    (B) Formation of new crust
    (C) Increased earthquakes only
    (D) Mantle cooling
    Answer: (B) Formation of new crust
    Explanation: Seafloor spreading adds new oceanic crust as magma rises and solidifies at mid-ocean ridges.

Preparation Strategies for 71st BPSC Prelims

  • Study plate tectonics, focusing on seafloor spreading and subduction.
  • Learn key terms like crust, magma, and convection.
  • Understand the role of mid-ocean ridges in crust formation.
  • Practice questions on geological processes and their outcomes.
  • Avoid confusing seafloor spreading (creates crust) with subduction (destroys crust).


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