Tectonic plates and their boundaries
The Earth's crust is broken into large pieces called tectonic plates that move slowly over the mantle below. Most earthquakes and volcanoes occur at plate boundaries where these plates meet.
Three types of boundary
- Convergent boundary: two plates collide. An oceanic plate sinks beneath a continental plate, producing volcanoes, earthquakes and fold mountains such as the Himalayas.
- Divergent boundary: two plates move apart. Magma rises to fill the gap, forming mid-ocean ridges and new volcanoes.
- Transform boundary: two plates slide horizontally past each other, causing strong earthquakes.
Key idea
Plate boundaries = zones of earthquakes and volcanoes. Convergent → fold mountains; divergent → ridges; transform → earthquakes.
The effects of plate movement include earthquakes that can trigger tsunamis, volcanic eruptions, and the building of mountain ranges. Malaysia lies a little away from active plate boundaries, but neighbouring countries such as Indonesia and the Philippines, on the "Pacific Ring of Fire", often suffer these hazards.