The Taal Volcano in the philippines. And more.
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
The Himalayas formed :]
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
India has it's own tectonic plate. It is not tectonically connected to the Eurasian plate. When the India plate crashed into the Eurasian plate, this formed the Himalayan Mountains. India is still moving closer to into the Eurasian plate today, and this is how the Himalayas are still growing.
The Eurasian and Australian plates. Krakatau was formed by the Australian plate subducting under the Eurasian plate.
Examples of collision mountain ranges include the Himalayas (formed by the collision of the Indian Plate with the Eurasian Plate), the Alps (formed by the collision of the African Plate with the Eurasian Plate), and the Andes (formed by the collision of the South American Plate with the Nazca Plate).
The Himalayas were formed by the convergence of the Indian and Eurasian tectonic plates, with the Indian plate pushing against the Eurasian plate, causing the land to rise and form the mountain range.
Mount Fuji, which is found in Japan is a type of island-arc volcano. It was formed by three plates, the Philippine plate, Eurasian plate and Okhotsk plate.
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.
They were formed when the African Plate and the Eurasian plate collided. The crust buckeld and thickend creating the mountains. They were formed when the African Plate and the Eurasian plate collided. The crust buckeld and thickend creating the mountains.
It has several! For example the Himalayas are formed due to the collision of the Indian and Eurasian tectonic plates.
Mount Stromboli is located on the Eurasian Plate due to tectonic forces that have pushed the plate boundary close to the area where the volcano formed. The volcano lies at a convergence zone where the African Plate is subducting beneath the Eurasian Plate, leading to volcanic activity in the region.