The Earth's surface is home to spectacular and frightening sights and experiences that hint at what is happening deep within the planet. Volcanoes and earthquakes are powerful evidence of the tectonic plates that grind against one another and the magma that rises through an inner layer known as the mantle.
Plate tectonics, a theory central to modern geology, explains so much of what we see happening around us. Through this theory, we now understand how mountains form, why there are different types of volcano, and how the land surface is constantly renewed.
The pages in this section contain video clips from popular television series such as Earth: Power of the Planet, presented by Iain Stewart, Horizon, Bang Goes the Theory, and How the Earth Made Us.
Image: Lava flows from Kilauea volcano into the sea in Hawaii (credit: Doug Perrine/naturepl.com)
Composite volcanoes
Composite volcano eruptions are often the most deadly.
Erosion
Rain, wind and ice constantly wear down the Earth's surface.
Hotspots
The Hawaiian islands owe their existence to a hotspot.
Impact craters
Asteroids and comets will continue to strike the Earth.
Inside the Earth
Earthquakes help geologists understand the Earth's inner structure.
Lava
Aa is a Hawaiian name for a type of lava.
Magma
Large bodies of molten rock exist below the Earth's surface.
Mid-ocean ridges
New sections of the Earth's tectonic plates form deep in the oceans.
Minerals
There are thousands of minerals on Earth.
Mountain formation
Most mountains are formed at tectonic plate boundaries.
Plate boundaries
Earthquakes and volcanoes are common at plate boundaries.
Plate tectonics
A theory explains why many of the continents fit together.
Rocks
Rocks are a valuable record of the Earth's history.
Shield volcanoes
Shield volcanoes are huge, but less explosive.
Supercontinents
In the past the continents have been joined together.
The rock cycle
Rocks change their form over very long time periods.
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