convergent boundary
The volcanic and earthquake activity in a region is usually caused by the movement of tectonic plates. When tectonic plates shift and collide, it can create volcanic eruptions and earthquakes due to the buildup of pressure and release of energy. The specific type of activity depends on the type of plate boundary present in the region.
A convergent boundary is where two plates collide. This can lead to the formation of mountains, earthquakes, and volcanic activity.
A mountain range forms when two of Earth's plates collide. The intense pressure and forces created by the collision push the Earth's crust upwards, creating towering peaks and ranges. Examples include the Himalayas formed by the collision of the Indian Plate and the Eurasian Plate.
The region where tectonic plates move is known as the lithosphere, which is the outermost shell of the Earth comprising the crust and upper mantle. Tectonic plate movement occurs at plate boundaries, where plates collide, move apart, or slide past each other, causing geological phenomena like earthquakes and volcanic activity.
When two plates collide, it can form different geological features such as mountain ranges, deep-sea trenches, and volcanic arcs. The exact formations that occur depend on the type of collision, whether it's a convergent boundary where plates collide, or a transform boundary where plates slide past each other.
When two continental plates collide,fold mountains are formed.
an earthquake
an earthquake
sinks
When plates collide it is called a convergent boundary.newtest3
earth plates can and do collide, even though the earth rotates around the sun
The volcanic and earthquake activity in a region is usually caused by the movement of tectonic plates. When tectonic plates shift and collide, it can create volcanic eruptions and earthquakes due to the buildup of pressure and release of energy. The specific type of activity depends on the type of plate boundary present in the region.
Mountains
Trolled
The answer is the Convergent Boundary.
a fault
earthquakes