convergent
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.
Dukono volcano is located on the island of Halmahera in Indonesia, which is situated on the boundary of the Indo-Australian Plate and the Eurasian Plate. This region is part of the Pacific Ring of Fire, where tectonic activity is high due to the interaction of these plates. The activity at Dukono is primarily a result of subduction processes associated with these tectonic boundaries.
Dukono is a volcano located in Indonesia that is part of the Pacific Ring of Fire, a region known for frequent seismic and volcanic activity due to the movement of tectonic plates. The volcano sits on the boundary between the Eurasian Plate and the Pacific Plate, where the Pacific Plate is subducting beneath the Eurasian Plate, leading to the volcanic activity in the region.
Dukono is located on the island of Halmahera in Indonesia, which is situated at the convergence of the Pacific, Eurasian, and Indo-Australian tectonic plates. This region experiences complex tectonic interactions, primarily characterized by subduction and volcanic activity. The convergence of these plates contributes to the formation of volcanic arcs and frequent seismic activity in the area, making Dukono an active stratovolcano.
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.
Dukono volcano is located on the island of Halmahera in Indonesia, which is situated on the boundary of the Indo-Australian Plate and the Eurasian Plate. This region is part of the Pacific Ring of Fire, where tectonic activity is high due to the interaction of these plates. The activity at Dukono is primarily a result of subduction processes associated with these tectonic boundaries.
Dukono is a volcano located in Indonesia that is part of the Pacific Ring of Fire, a region known for frequent seismic and volcanic activity due to the movement of tectonic plates. The volcano sits on the boundary between the Eurasian Plate and the Pacific Plate, where the Pacific Plate is subducting beneath the Eurasian Plate, leading to the volcanic activity in the region.
Dukono is located on the island of Halmahera in Indonesia, which is situated at the convergence of the Pacific, Eurasian, and Indo-Australian tectonic plates. This region experiences complex tectonic interactions, primarily characterized by subduction and volcanic activity. The convergence of these plates contributes to the formation of volcanic arcs and frequent seismic activity in the area, making Dukono an active stratovolcano.
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 by a collision plate boundary, meaning that the plates collided and formed the Himalayas. The Himalayas are also referred to as 'fold mountains' because of the way in which they are made.
The east coast of South America along the Atlantic Ocean is a passive continental margin. This means that it is not located along a tectonic plate boundary where significant tectonic activity such as earthquakes or volcanic eruptions occur. The passive margin formed when South America separated from Africa during the opening of the South Atlantic Ocean.
A physcadelic plate.
Pumice is formed from magma coming out of volcanoes where rhyolite would have formed, (Destructive plate margin), but has cooled so fast that it appears glassy, and almost non-crystalline.
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.