To provide an accurate answer, I would need more context about what "plate B" refers to. In geological terms, if plate B is a tectonic plate, various formations such as mountains, volcanoes, or oceanic trenches can occur due to its interactions with adjacent plates. If you have a specific context or scenario in mind, please clarify for a more precise response.
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.
Mount Tambora was formed by a convergent plate boundary. It is located on the Indonesian island of Sumbawa, where the Australian Plate converges with the Sunda Plate, causing subduction and volcanic activity in the region.
To provide an accurate answer, I would need specific details about "plate a" and "plate b," such as their characteristics or context. Generally, if plate a is an oceanic plate, it would be denser and thinner compared to plate b, which might be a continental plate, characterized by being thicker and less dense. The classification is based on geological features and tectonic activity.
Mountains.
To provide an accurate answer, I would need more context about what "plate B" refers to. In geological terms, if plate B is a tectonic plate, various formations such as mountains, volcanoes, or oceanic trenches can occur due to its interactions with adjacent plates. If you have a specific context or scenario in mind, please clarify for a more precise response.
An accretionary prism is an alternative name for an accretionary wedge, the accumulation of sediment formed by an oceanic plate and a tectonic plate, as it is scraped from the top of the oceanic plate.
The Himalayas formed :]
It was formed by the subduction of the Pacific Plate beneath the north American plate.
A subduction zone is formed.
how much does a top plate cost
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
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.
Mount Tambora was formed by a convergent plate boundary. It is located on the Indonesian island of Sumbawa, where the Australian Plate converges with the Sunda Plate, causing subduction and volcanic activity in the region.
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 most notable are the Himalayas, formed when India (on the Indo-Australian plate) drove north into Asia.