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Indonesia is located near the borders of the Eurasian and Indo-Australian Tectonic Plate zones. Subduction will happen from the plates rubbing together causing earthquakes in Indonesia
Indonesia is located near the borders of the Eurasian and Indo-Australian Tectonic Plate zones. Subduction will happen from the plates rubbing together causing earthquakes in Indonesia
Indonesian volcanoes like mt rinjani are formed due to subduction zones between the Eurasian plate and the Indo-Australian plate
Yes. Some volcanoes on the Eurasian Plate include: Mount Etna in Sicily, Mount Vesuvius in Italy, Santorini off the coast of Greece, Mount Baekdu on the border of China and North Korea, Mount Unzen in Japan, and many others.
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.
Cinder cone volcanoes have formed in all of the major land-based settings for volcanoes: subduction zones, hot spots, and rifts.
There is a subduction zone under Krakatoa where the Indian Ocean seafloor is being pushed eastwards under Indonesia. (The Australian plate is moving under the Eurasian plate here.) When the seafloor is pushed into the earth it melts due to increases in pressure and temperature. The hot, melted seafloor material (now known as magma) rises up and creates volcanoes like Krakatoa.
Japan is an arc caused by subduction of the Pacific and Phillipine plates beneath the Eurasian plate. The subduction plates lose water to the mantle rocks as they go down, which causes the mantle rock to melt. This is the magma that forms the volcanoes. The earthquakes are caused by the plates scraping against each other- a subduction zone is basically a reverse fault.
The Himalayas were lifted by the subduction of the Indian tectonic plate under the Eurasian Plate,
The two plates that caused the formation of Vesuvius were the African and Eurasian plates. Its resting on a compressional/destructive plate boundary.
The Himalayas were lifted by the subduction of the Indian tectonic plate under the Eurasian Plate,