I’m not sure
Yes, a subduction zone is a type of convergent boundary where one tectonic plate is forced beneath another plate.
Convergent boundary Convergent boundary
This occurs at a convergent plate boundary, specifically at a subduction zone where one plate is forced beneath another due to differences in density.
This type of plate boundary is called a convergent boundary or subduction zone. It occurs when two tectonic plates collide, with the denser oceanic plate being forced beneath the less dense continental plate. This process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
Subduction is a convergent boundary where one tectonic plate moves beneath another plate into the Earth's mantle. This process occurs at plate boundaries where two plates are moving towards each other.
I’m not sure
The plate boundary for Unzen volcano is the subduction zone where the Philippine Sea Plate is being subducted beneath the Eurasian Plate. This subduction zone is part of the larger convergent boundary between the Philippine Sea Plate and the Eurasian Plate.
Yes, subduction occurs at a convergent boundary—but specifically when an oceanic plate converges with another plate. Here’s how it works: 🔁 Convergent Boundary Types: Oceanic-Continental Convergence The denser oceanic plate subducts beneath the lighter continental plate. 🌋 Example: Andes Mountains (South America) Oceanic-Oceanic Convergence One oceanic plate subducts beneath the other, forming island arcs. 🌋 Example: Japan, Mariana Trench Continental-Continental Convergence No subduction occurs here—both plates are too buoyant. Instead, they collide and crumple, forming large mountain ranges. 🏔️ Example: Himalayas ✅ Summary: Subduction = Yes → Oceanic-continental & oceanic-oceanic boundaries Subduction = No → Continental-continental boundaries #JAIDIXIT
Yes, a subduction zone is a type of convergent boundary where one tectonic plate is forced beneath another plate.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
A Transform Fault ZoneIn the textbook Earth Science and the Environment (4th Edition) by Thompson and Turk. Located on page 163, it shows that Tonga has a Convergent Boundary. A convergent boundary is where two lithospheic plates collide head on.
Subduction takes place at a convergent plate boundary, where two tectonic plates collide and one plate is forced beneath the other into the Earth's mantle. This process is associated with the formation of deep ocean trenches and volcanic arcs.
Convergent boundary Convergent boundary
A convergent boundary forms when an oceanic plate is pushed under a continental plate. This process, known as subduction, can result in the formation of deep ocean trenches, volcanic arcs, and earthquakes.
Paricutin is located on a convergent boundary. The volcano formed as a result of the subduction of the Cocos Plate beneath the North American Plate in Mexico.
This occurs at a convergent plate boundary, specifically at a subduction zone where one plate is forced beneath another due to differences in density.
Mt. Fuji is a result of subduction at a convergent plate margin.