Skip to content
Skip to main content

What's Beneath Our Feet?

Updated Tuesday, 7th September 2004
The rocks and minerals that lie beneath the surface of the UK

This page was published over 18 years ago. Please be aware that due to the passage of time, the information provided on this page may be out of date or otherwise inaccurate, and any views or opinions expressed may no longer be relevant. Some technical elements such as audio-visual and interactive media may no longer work. For more detail, see how we deal with older content.

The Yorkshire Tracks

For the past 4,000 years we humans have been making an impact on our natural landscape - whether it be exploiting our natural resources, cutting down trees for building, firewood and to expose agricultural land, or searching for precious metals like gold and silver to make weapons, jewellery and coins. We have even used our landscape to make religious and political statements, like the Cerne Abbas Giant chalk figure.

The Cerne Abbas Giant

While we can all understand ‘historical time’, like the Medieval period, the Romans, Saxons and Vikings, which takes us back to about 2,000 years ago; ‘archaeological time’ takes us back even further through the Iron, Bronze and Stone age, Neanderthals and back to the first Homo Sapiens, almost a 100 thousand years ago. But this is nothing, ‘geological time’, measured in millions of years, takes us right back to the beginning of the earth over 4,600 million years ago.

What’s beneath our feet?
Most of us have probably picked up an attractive pebble on the beach, or found an unusual rock in the garden, or maybe your house or local church is made out of a particular stone. Depending on where you live the rocks beneath your feet will be quite different, because they formed at different times and in different environments.

The rocks of Britain provide a physical record of the past and ancient history of our island and they have changed over time according to the climate and the movement of the earth’s plates. They show that the UK has been drifting like a ‘passenger’ on its tectonic plate, beginning somewhere south of the equator and ending up in the northern latitudes where we are now. On the way the UK has formed rocks and sediments typical of those environments. Going out and looking at the rocks in your local area will give you a clue to the ‘geological history’ of the UK. But how do you know what you’re looking at?

Hillside showing strata of rock

We mainly see rocks in cliffs and road cuttings, but rocks also lie below the vegetation and soil in every landscape. Some of these rocks are useful as building stones, others are the source of valuable and precious metals. Rocks can seem to be a permanent feature of our landscape, but in fact they are being created, destroyed and recreated all the time. Over millions of years, volcanoes erupt, mountains are built, these are eroded by water and ice, and the rock fragments are laid down in rivers and on the seabed, only to be crumpled up to form mountains and eroded again, in a continuous cycle of processes that goes on to the present day.


The Yorkshire Tracks

The different rocks making up the surface of the earth form in different ways, and the processes involved leave their mark on the rocks they produce.

At a basic level it’s important to be clear about what is a rock and a mineral.

A “mineral“ is a solid material, formed by natural processes and with a chemical composition that falls within certain narrow limits. Minerals are made up of atoms which are arranged in a regular pattern, so they form ‘crystals’ with characteristic shapes, like cubes, sheets or pyramids. A “rock“ is a solid collection of mineral grains. These may be fragments of crystals or whole crystals and they can be mm to cm in size. A rock may have only one type of mineral, but usually it consists of several different minerals. Look at this rock - it's made of three different kinds of minerals - black, grey and white crystals:

Three types of rock in one sample

New rocks are formed where ‘magma’ or molten rock flows out onto the surface of the earth, like lava flows on the volcanoes of Hawaii, but they can also be formed by the weathering and erosion of existing rocks. The earth is a dynamic planet and the rocks are continually being recycled. There are 3 basic types of rock which are produced by three different processes acting to form rocks on the earth.

‘Igneous rocks’ are formed from molten rock that becomes solid when it cools, either on a volcano or deep in the ground in the earth’s crust:

Molten lava

They usually contain crystals. The number and size of crystals depends on how long they took to grow. Rocks which cool slowly, deep underground, grow big crystals, like granite. Rocks which cool very quickly at the surface like lavas, have minute crystals and can even be glassy.

‘Sedimentary rocks’ are made up of grains which have been eroded from other rocks, like igneous rocks. The grains are small rock fragments or individual mineral grains, and are often rounded because they have been transported by water or wind. The grains are laid down as sediments, in layers, like sand on the beach or mud in a river. Over time they get buried, become compacted and cemented into solid rock. Sedimentary rocks can contain fossils of plants or animals which were living at the time the rock was being deposited, or in some cases they are made completely of the fossil skeletons of plants and animals, forming a rock like limestone.

‘Metamorphic rocks’ are existing rocks which have been ‘changed’ or ‘metamorphosed’ by high temperature and pressure, usually after being buried deep within the earth. These rocks are made up of crystals, and are often banded, contain veins and can be flaky or sugary. Metamorphic rocks make up some of our most useful and beautiful building materials, like slate and marble.

Slate is a metamorphic rock with very tiny crystals. It was originally laid down as a soft mud, but it has been recrystallized into a hard, water resistant rock that can be split into thin sheets, making excellent roofing tiles. Marble is formed from limestone, but unlike slate it is not flaky. Marble doesn’t break into sheets like slate, therefore it is a good material for statues, as smooth surfaces can be carved in any direction.



Out to sea: A river estuary

Igneous and metamorphic rocks give us some clues about what is happening deep within the earth, or at the surface, where magma forms new rocks. Sediments give us a record of what has been happening at the earth’s surface over the past thousands and millions of years.


Different sediments are laid down in different environments, with different climates. If we look at the rocks around us they give us a clue to the past ‘geological history’ and climate of Britain. The geology of Great Britain records the passage of our island from south of the equator to its current position.

• In the South East of Britain the rocks are mainly chalk, sandstone and clays. Chalk is a well known type of rock made up of minute skeletons of billions of tiny sea creatures.

• In the North of England, the commonest type of rock is limestone, which is also made up of the skeletons of sea creatures, shells and corals.

Both of these rocks were laid down in the warm seas of a tropical climate, imagine that England once had a climate like the Bahamas has today, with warm seas and coral reefs.

• Parts of Wales, Scotland and Ireland have rocks that indicate another period when the British climate was much hotter than it is today. Red sandstone in these areas was laid down in a hot, arid desert environment.

• At the other extreme, North Wales and the English Lake District have rocks like shales and mudstones, that were formed in deep cold water. Intruding into all these sedimentary rocks are igneous rocks like granite, and we even have ancient volcanoes and lava flows.

Of course our landscape is not only characterised by the rocks that form it, it has also been shaped by the weather. In the ice age, glaciers and great ice sheets carved out deep wide valleys in the landscape and left mounds of gravel and sheets of boulder clay when the ice melted and retreated. You can find out more in ’The Big Freeze – from Icehouse to Greenhouse’.


Become an OU student

Ratings & Comments

Share this free course

Copyright information

Skip Rate and Review

For further information, take a look at our frequently asked questions which may give you the support you need.

Have a question?