Context: A recent study by scientists in Portugal predicts the 'Ring of Fire' subduction zone beneath the Gibraltar Strait may lead to the Atlantic Ocean's closure in 20 million years.
Subduction Zone
About:A subduction zone forms where two tectonic plates converge, leading one to descend beneath the other.
Nature of Tectonic Plates: Tectonic plates are segments of the Earth's outer shell that gradually shift across its surface over long periods.
Plate Tectonics Theory: Plate tectonics theory asserts that the Earth's shell comprises moving plates that carry continents atop the lower mantle.
Composition of the Lithosphere: The lithosphere, encompassing the crust and upper mantle, constitutes the Earth's outer layer.
Subduction Mechanism: When plates meet at a subduction zone, the denser lithosphere descends into the hot mantle, inducing curving.
Lithospheric Types and Subduction: Subduction commonly arises from the interaction of contrasting lithospheric types—continental and oceanic.
Oceanic Plate Dynamics: Older, denser oceanic lithosphere submerges beneath younger, buoyant lithosphere, a process perpetuating subduction.
Formation of Oceanic Lithosphere: New oceanic lithosphere forms at plate boundaries, cooling and densifying over time, predisposing it to subduction.
Geographical Distribution: Subduction zones encircle the Pacific Ocean in a horseshoe shape, known as the "Ring of Fire," showcasing intense seismic and volcanic activity.
Strait of Gibraltar
About: It serves as a crucial waterway, linking the Atlantic Ocean with the Mediterranean Sea and acting as the boundary between Europe and Africa.
Varied Depth: The depth of the Strait of Gibraltar varies considerably, ranging from 300 to 900 meters (980 to 2,950 feet; 160 to 490 fathoms), making it a complex and dynamic maritime environment.
Territorial Jurisdiction: The strait falls within the territorial waters of Morocco, Spain, and the British overseas territory of Gibraltar, highlighting its geopolitical significance.