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As mountains rose overhead, the Indian plate slid underneath Asia.
The Himalayas were formed some time after the Indian Plate collided with the Eurasian Plate.
East of the Alpine region, the Indian Plate was moving northward approaching the Asian Plate.
The ridge then subsided as it rode north on the Indian Plate.
For example, Mr. Wyman quit smoking after stubbing out a cigarette on an American Indian plate that Mr. Land grimly informed him was irreplaceable.
What enabled the Indian plate to move so fast?
It was caused by a collision of the Indian Plate beneath the Eurasian Plate.
(Inset) Indian plate boundaries are highlighted to realize the geographical location of Kachchh peninsula.
The northward drift of Indian Plate during Cretaceous to Eocene period is shown in Fig. 1a.
The cold lithosphere in the Indian Plate exhibits a high Pn velocity.
In the northern region (25°N), the strike of the subducting Indian Plate is N20°E.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com