spreading
subduction
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A physcadelic plate.
Japan sits on top of a destructive plate margin.
Yes, Eyjafjallajökull volcano is located on the constructive plate margin between the North American Plate and the Eurasian Plate in Iceland.
No,plate margin&plate boundary are not same.plate boundaries are definite regions where tectonic occurs,while margins are surface lines.
The Himalayas were formed at a convergent plate margin where the Indian Plate collided with the Eurasian Plate. This collision resulted in the uplift of the Himalayan mountain range.
Continental crust (Eurasian Plate) and oceanic crust (pacific plate) move towards each other, oceanic crust sinks because its denser, this forms deep sea trenches and volcanoes
Krakatoa is located on a destructive plate margin where the Indo-Australian plate subducts beneath the Eurasian plate. This subduction zone has led to the formation of volcanic islands in the region, including Krakatoa.
Mount. Merapi is on the Sunda Plate, which forms a convergent margin with the Indian-Australian Plate
It's called destructive plate margin/boundary, or convergent plate margin though this term applies to all plate margins where two plates are moving towards each other (such as continental + continental or oceanic + oceanic).
The San Andreas Fault in California is an example of a transform plate margin. Here, the Pacific Plate and the North American Plate slide past each other horizontally, leading to frequent earthquakes.
Florida sits on the trailing margin of the North American tectonic plate.
active continental margin