A subduction zone can be a result of a convergent plate boundary, but the terms are not synonymous. If the two convergent plates are continental, neither of them will subduct.
Islands can form at various types of plate boundaries, including divergent boundaries where tectonic plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past each other. Island formation is often influenced by volcanic activity associated with plate boundaries.
They are the same size
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
No, faults are not the same as plate boundaries, though they are related. Faults are fractures in the Earth's crust where rocks have moved past each other, while plate boundaries are the edges where tectonic plates interact. Plate boundaries can give rise to faults due to the stress and movement of the plates, but not all faults are located at plate boundaries. Faults can also occur within tectonic plates away from these boundaries.
mount Kilimanjaro sits on a divergent plate boundry
No, subducting plate and oceanic plate are not the same. An oceanic plate is a type of tectonic plate that lies beneath the ocean, while a subducting plate refers to an oceanic plate that is descending beneath another tectonic plate at a convergent boundary. Subducting plates are a specific category of oceanic plates.
Convergent boundaries are boundaries where tectonic plates are moving together. Since the edges of both can't be in the same place, one plate will be forced under another plate (and the other above). The plate going 'down' will thus go deeper into the earth - allowing deeper earthquakes to occur.
Islands can form at various types of plate boundaries, including divergent boundaries where tectonic plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past each other. Island formation is often influenced by volcanic activity associated with plate boundaries.
I think there 1)Destructive (convergent) 2)collision(convergent) 3)constructive(divergent) 4)conservative(transform) the brackets are the same words
They are the same size
No, some are convergent (against each other), some are divergent (away from each other), and most boundaries are transform (horizontal grinding) at some point.
Convergent boundaries are boundaries where tectonic plates are moving together. Since the edges of both can't be in the same place, one plate will be forced under another plate (and the other above). The plate going 'down' will thus go deeper into the earth - allowing deeper earthquakes to occur.
No. Not all plate boundaries are at the edges of continents, nor do all edges of continents correspond with plate boundaries. Many plate boundaries are found in the middle of oceans, while the continent of Africa is being torn apart by a developing plate boundary. Some edges of continents, such as the west coast of South America are near plate boundaries. These are called active continental margins. Others, such as the east coast of North America, are nowhere near plate boundaries. These are called passive continental margins.
there the same
Yes
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
An equal amount of oceanic crust is being subducted at the convergent plate boundaries as is being created at the mid-oceanic ridge.