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The continental crust is less dense than the oceanic crust. That's the reason we find that the oceanic crust sinks (subducts) beneath the continental crust.
Continental crust is less dense than oceanic crust and so cannot sink below it.

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The two types of convergent boundaries are -?

The two types of convergent boundaries are oceanic-continental and continental-continental. At oceanic-continental convergent boundaries, an oceanic plate subducts beneath a continental plate, leading to volcanic activity and the formation of mountain ranges. In contrast, at continental-continental convergent boundaries, two continental plates collide, resulting in the uplift of mountain ranges without significant subduction. These interactions are responsible for significant geological features and seismic activity.


What are the three different setting of convergent boundaries?

Oceanic-continental: Oceanic plate is subducted beneath continental plate, creating volcanic arcs and mountain ranges. Oceanic-oceanic: One oceanic plate is subducted beneath another, forming deep ocean trenches and volcanic island arcs. Continental-continental: Collision of two continental plates, leading to intense folding and faulting, creating high mountain ranges.


Which event is the most common at oceanic-continental convergent boundaries?

Rift Valleys are the most common at oceanic-continental convergent boundaries.


Why are continental volcanoes associated with oceanic continental convergent boundaries?

Continental volcanoes form at oceanic-continental convergent boundaries because as oceanic plates are subducted beneath continental plates, the subducted oceanic crust melts due to the high temperatures and pressures deep within the Earth. This molten rock then rises to the surface, resulting in volcanic eruptions on the continental plate.


What are the 3 subtypes of convergent plate boundaries?

1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.

Related Questions

What are the three types of convergent plate boundries?

The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries


What are the three sub-types of convergent plate boundaries?

if i thing if gago abno yudipota ka


The two types of convergent boundaries are -?

The two types of convergent boundaries are oceanic-continental and continental-continental. At oceanic-continental convergent boundaries, an oceanic plate subducts beneath a continental plate, leading to volcanic activity and the formation of mountain ranges. In contrast, at continental-continental convergent boundaries, two continental plates collide, resulting in the uplift of mountain ranges without significant subduction. These interactions are responsible for significant geological features and seismic activity.


Convergent continental oceanic definition?

Convergent continental-oceanic boundaries are locations where a continental plate collides with an oceanic plate, resulting in subduction of the denser oceanic plate beneath the less dense continental plate. This collision can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes. The Andes Mountains in South America and the Cascades in North America are examples of convergent continental-oceanic boundaries.


What are the three different setting of convergent boundaries?

Oceanic-continental: Oceanic plate is subducted beneath continental plate, creating volcanic arcs and mountain ranges. Oceanic-oceanic: One oceanic plate is subducted beneath another, forming deep ocean trenches and volcanic island arcs. Continental-continental: Collision of two continental plates, leading to intense folding and faulting, creating high mountain ranges.


Which event is the most common at oceanic-continental convergent boundaries?

Rift Valleys are the most common at oceanic-continental convergent boundaries.


What does a convergant boundary form?

There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges. Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range. Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.


What are the types of convergent boundary?

There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.


What are the three different types of convergent plat boundaries?

The three different types of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental. In an oceanic-continental boundary, the denser oceanic plate subducts beneath the less dense continental plate. In an oceanic-oceanic boundary, one oceanic plate subducts beneath another. In a continental-continental boundary, the plates collide and uplift, forming mountain ranges.


Convergent boundaries can be divided into 3 categories what are these categories and what geological feature are created by each?

The categories are a continental and a continental plate colliding, continental and oceanic plates colliding, and oceanic and oceanic plates colliding. The two continental plates form mountains. The continental and oceanic plated colliding cause subduction zones and volcanoes. Oceanic and oceanic plates colliding form a trench.


What are the types of convergence?

There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.


What are three sub-types of convergent plate?

Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.