Hot air pour into the lower pressure area and hit head on, rise up, condense and rain.
The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).
generally in mountain ranges
No, Teide is not formed on a convergent plate boundary. It is a volcano located on the island of Tenerife, which is part of the Canary Islands, formed by a hotspot beneath the Earth's crust, creating a volcanic hotspot.
A rain shadow.
Convergent boundaries are typically found where mountain ranges are created. This is where two tectonic plates move towards each other, causing the crust to buckle and push upwards, forming mountain ranges.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
At convergent boundaries plates come together. In other words, they converge.
Convergent precipitation occurs when air masses with different temperatures and moisture levels collide, causing the air to rise rapidly and form thunderstorms. This can lead to severe weather events like heavy rain, hail, strong winds, and tornadoes.
Convergent.
A convergent boundary causes compressional stress.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
Convergent boundary.
They form on convergent boundaries.
Convergent boundry
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.