There are three main types of plate boundaries:
An example of a continental to continental crust collision is the collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayan mountain range. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
Great Britain and Ireland, along with continental Europe, are entirely on the Eurasian Plate.
The plates that have continental crust include the North American Plate, South American Plate, Eurasian Plate, African Plate, Australian Plate, and Antarctic Plate. These plates contain mostly granitic rock, which is characteristic of continental crust.
Eyjafjallajökull is located on the boundary between the Eurasian Plate and the North American Plate in Iceland.
eurasian plate
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
Ireland is located on the Eurasian Plate, which covers Europe and parts of Asia.
Mount Vesuvius is located on a continental plate, specifically the Eurasian Plate. It is within the boundaries of the subduction zone where the African Plate is being subducted beneath the Eurasian Plate, leading to volcanic activity in the region.
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
An example of a continental to continental crust collision is the collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayan mountain range. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
eurasian plate
The Himalayas and the Tibetan Plateau are formed by a continental-continental boundary where the Indian continental plate is moving north against the Eurasian continental plate.
The Eurasian Plate is largely considered to be a continental plate. It does, however, lay claim to some oceanic crusts, most notably extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge.
No It is considered a continental plate although it does cover some ocean
Great Britain and Ireland, along with continental Europe, are entirely on the Eurasian Plate.
Where the Indian-Australian Plate Meets the Eurasian Plate. This is along the Himalayan Mountains.
The tectonic plate under parts of Europe and Asia is a continental crustal plate.