The term geothermal means “heat from the Earth”. Geothermal energy comes from the natural heat stored beneath the Earth’s surface. The Earth’s crust contains a virtually limitless amount of thermal energy which is being continuously replenished by heat conduction from the mantle below it. The temperature at the base of the crust is about 1000°C and, as a result, the deeper you go underground, the hotter it gets, on average at a rate of 25°C per km.
Geothermal is normally associated with volcanic regions such as Iceland and New Zealand, as this heat is more easily accessible being closer to the surface. In volcanic areas and places where the Earth's plates meet, the underground heat is much stronger. Just a couple of kilometres below the surface, temperatures can reach several hundred degrees. In some locations this heat creates natural pockets of hot water or steam underground. By drilling into these areas, we can bring the heat to the surface and use it to generate electricity and provide heating.
But geothermal resources exist away from volcanic regions too. Most countries around the world can access geothermal, albeit at lower temperatures, and around 90 countries are now harnessing it for heat or power. Some are drilling much deeper wells in non-volcanic areas to access the temperatures they need because they recognise the environmental benefits of the technology.
Geothermal is a clean, sustainable, renewable, low carbon energy source that has a very small surface footprint and minimal environmental impact. It can be harnessed from just a few metres below the surface or from deep underground and used for heating, cooling, and electricity generation. It is already present across the UK and can be accessed using different technologies to provide low-carbon heat and power.
You can find more information about geothermal energy on the British Geological Survey website and through GeoScience Limited.
Watch the British Geological Survey’s Geothermal Energy Lesson Introductory video.