Having formed as part of the Solar System around 4600 million years ago, the internal structure of the earth is composed of condensed gases and particles in concentric layers.  At extremely high temperature and pressure, the densest part of the earth is the central core, whilst the coolest, lightest and thinnest part of the earth is the outer layer, the crust. 

In between the two exists a thick layer known as the mantle, capable of movement, even though it is comprised of mostly solid rock.  The movement of the mantle is key to the changes that have occurred on the Earth’s surface since its formation. 

The earth’s crust moves across the mantle in great sections, known as plates. The plates fit together like a giant jigsaw, great sections constantly moving relative to each other at a rate of a couple of centimetres per year.  Known as plate tectonics, this process is responsible for continents colliding as they move from one side of the globe to another, oceans opening and closing, sea levels dramatically altering and mountains rising; millennia of volcanic action, earthquakes and unbelievable pressures contorting the very rock itself.

New rock is created where the plates pull apart (constructive plate margin) and old rock sinks back down into the mantle and melts where one plate slides under the other (destructive plate margin). Quite literally the Earth recycles itself! In some cases the plates do neither of the above but judder past one another. The pressure between the plates build until the forces cannot hold any longer and an earthquake occurs, sometimes creating great tears in the earth and potentially further complications from tsunami if the quake occurs under the sea.

Although much older rocks exist elsewhere in the country, the first rocks evident in Torbay are from the Devonian Period, the pre-Devonian history is uncertain.