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It’s located in the Indian Ocean, extending north from the South Atlantic.
It’s a mid-ocean ridge, a chain of underwater mountains formed by the separation of tectonic plates.
The Mid-Indian Ridge is a divergent boundary, where tectonic plates move apart, allowing magma to rise and cool, creating new crust.
Its existence supports the theory of continental drift and plate tectonics, where Earth’s crust is divided into large plates that move and interact.
It divides into two segments near Rodrigues Island: one northward towards the Gulf of Aden and the other southeast towards the Macquarie Ridge.
The central section of the Mid-Indian Ridge is known as the Central Indian Ridge.
The Mid-Indian Ridge is associated with earthquake activity, though it is considered a relatively slow spreading ridge.
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