Main Body
The Plate Tectonics Theory put forth by geographers like Harry Hess explain the differential positions or shapes of continents.
Plate Tectonics Theory — Major Targets:
The granite is divided/fragmented into several plates.
ex: Nazca Coles, Pacific
These plates have movement driven by convective currents in the chamber
ex: [illegible] cells.
The relative movement of the plates ensure creation of landforms
ex: Ring of Fire
(ocean-continent convergence)
Theories of seafloor spreading with proof such as similar age of equidistant deposits is support Plate Tectonics.
Different types of Plate Boundaries:
Convergent Plate Boundary: Here two plates collide with each other with denser plates subducting under the lighter.
ex: Continent - Continent: Block/Fold Mountains
ocean - continent: Pacific Ring of Roe.
Divergent Plate Boundary: Here, two plates diverge away from each other due to diverging limbs of convective cells.
ex: Mid-Atlantic Ridge - chain of mountain arcs has formed due to divergent boundaries.
Transform Boundary: Here, while there is no subduction, there is release of tension between plates - sliding past each other.
ex: Gujarat Earthquake was due to a transform boundary.
Understanding of Plate Tectonics has led to:
Thus the development of the theory has imparted a scientific movement to the geological shift through Earth's history.
- Covers major aspects of Plate Tectonics Theory
- Provides examples (Nazca, Coles, Pacific, Ring of Fire)
- Explains mechanism of plate movement via convective currents
- Links plate movement to landform creation
Amrit Mahapatra
World Physical Geography
Phenomena
Plate Tectonics Theory
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