Krakatoa is situated on the Sunda Plate in Indonesia. The Sunda Plate is a minor tectonic plate in the region, and Krakatoa is a volcanic island located within this tectonic setting.
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.
Eurasian Plate and the Indo-AustralianPlate
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
Yes, Krakatoa is a volcano located on the boundary where the Indo-Australian Plate subducts beneath the Eurasian Plate. It is not formed from a hot spot.
Krakatoa is located on a convergent plate margin, specifically where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction zone is known for producing volcanic activity due to the collision between the two plates.
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.
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Eurasian Plate and the Indo-AustralianPlate
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Yes. It is on the boundary between the Indian Plate, and the Eurasian Plate.
The Krakatoa plates moved in a convergent manner, where the Indo-Australian Plate subducted beneath the Eurasian Plate. This movement led to the intense volcanic activity and eventual eruption of Krakatoa in 1883.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
Yes, Krakatoa is a volcano located on the boundary where the Indo-Australian Plate subducts beneath the Eurasian Plate. It is not formed from a hot spot.
Yes, Krakatoa is located on a subduction zone. The island sits on the convergent boundary between the Eurasian Plate and the Indo-Australian Plate, where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction zone contributes to the volcanic activity in the region.
Krakatoa is located on a convergent plate margin, specifically where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction zone is known for producing volcanic activity due to the collision between the two plates.
Krakatoa is located on the boundary of two tectonic plates: the Eurasian Plate and the Indo-Australian Plate. This area is known as the Sunda Arc subduction zone, where the Indo-Australian Plate is subducting beneath the Eurasian Plate, leading to volcanic activity in the region.
It erupted because it couldn't hold any longer.