Answer:
Convergent boundary is formed
when two plates move toward each other.
This boundary has three types: Oceanic-
Continental plate boundary, Two Oceanic
plate boundary, and Two Continental
plate boundary. In Oceanic-Continental
plate boundary and two oceanic plate
boundary, the oceanic plate bends down
into the mantle through the process called
subduction. The leading edge of the
subducted plate melts in the mantle andmagma rises forming a continental volcanic arc in oceanic-continental plate
boundary, which is parallel to the trench that is formed due to subduction while in
two oceanic plate boundary, island volcanic arc is formed parallel to the trench. An
earthquake occurs at this boundary. Since the oceanic plate is destroyed at the
convergent boundary, this boundary is also called a destructive boundary. Examples
are boundaries between the Eurasian plate and the Philippine plate, Nazca Plate and
South American Plate, and Pacific Plate and Australian Plate. With two continental
plates converging, a tension zone is formed. Both plates collide and buckle up
causing mountain ranges such as the Himalayas mountain ranges. There is no
subduction, no trench, and no volcanoes formed in this type of convergent boundary.
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Answers & Comments
Answer:
Convergent boundary is formed
when two plates move toward each other.
This boundary has three types: Oceanic-
Continental plate boundary, Two Oceanic
plate boundary, and Two Continental
plate boundary. In Oceanic-Continental
plate boundary and two oceanic plate
boundary, the oceanic plate bends down
into the mantle through the process called
subduction. The leading edge of the
subducted plate melts in the mantle andmagma rises forming a continental volcanic arc in oceanic-continental plate
boundary, which is parallel to the trench that is formed due to subduction while in
two oceanic plate boundary, island volcanic arc is formed parallel to the trench. An
earthquake occurs at this boundary. Since the oceanic plate is destroyed at the
convergent boundary, this boundary is also called a destructive boundary. Examples
are boundaries between the Eurasian plate and the Philippine plate, Nazca Plate and
South American Plate, and Pacific Plate and Australian Plate. With two continental
plates converging, a tension zone is formed. Both plates collide and buckle up
causing mountain ranges such as the Himalayas mountain ranges. There is no
subduction, no trench, and no volcanoes formed in this type of convergent boundary.