Tees Valley Geology Details
The Tees Valley is blessed with some of the most spectacular geology and industrial archaeology in the British Isles, ranging from:
|
Upland Moors and Escarpments The North York Moors and Cleveland Hills tower over the Tees Valley providing a rugged horizon. The underlying geology outcrops creating spectacular exposures at places like High Cliff Nab and Eston Hills. |
![]() |
![]() |
|
Deep River Gorges Draining from upland areas such as East Durham and the North York Moors rivers have cut deep gorges creating amazing exposures and landscapes. Rivers like Crimdon Dene and Skelton Beck are excellent examples. |
![]() |
![]() |
|
Coastal Scar and Cliffs The coastline from Redcar to Staithes provides us with some outstanding exposures and breathtaking scenery. Cliffs such as Huntcliff at Saltburn and the scar at Redcar stand proud dominating the view south from Hartlepool Headland. |
![]() |
![]() |
|
Industrial Archaeology Mineral extraction has been a major driving force behind the Tees Valley’s development. Salt extraction, Ironstone mining, Jet mining, and the Alum trade have all left behind scars on the landscape, creating features such as Boulby Cliff and Eston Hills. |
|
|
Geological Heritage of the Tees Valley
|
|
Quaternary: 10,000 Years ago We were underneath 300m of ice during the last Ice Age. Exposed all over the Tees Valley as clays, sands and gravels. |
|
Jurassic: 200 Million Years ago We were underneath a shallow tropical ocean similar to the Caribbean Sea. Jurassic rocks exposed in cliffs and inland throughout upland areas. |
|
|
Triassic: 245 Million Years ago We were on the edge of a desert similar to the Sahara Desert today. Triassic rocks exposed at Seaton Carew beach and at Ingleby Barwick. |
|
|
Permian: 290 Million Years ago Underneath a very shallow and salty tropical ocean with massive coral reefs. Permian rocks exposed at Hartlepool Headland. |
The Geodiversity Action Plan is a project delivered by the Tees Valley Wildlife Trust, enabled by funding from the Heritage Lottery Fund. The GAP aims to document, conserve, manage and promote the geological heritage of the Tees Valley. The project is run in direct co-operation with the Tees Valley RIGS Group.
The project achieves its objectives by raising awareness amongst, and encouraging practical action by local communities and schools, through education and volunteering opportunities. The project specifically offers an extensive guided walk programme for the general public and offers local schools & colleges the chance to take part in site visits and classroom based geological activities.
|
Volunteering Opportunities The project offers the chance to get really involved and help protect some fragile or neglected sites of geological interest. |
![]() |
|
Guided Walk Activities Free of Charge Taking the general public out to see the spectacular geology of the Tees Valley raises awareness and gets people fit! |
![]() |
|
Education Sessions Free of Charge Education sessions are being offered to involve local schools and raise geological awareness at the grass roots. |
![]() |
|
If you want to get involved with the GAP project then contact Beth Andrews at the Tees Valley Wildlife Trust. |
|
The spectacular “ironstone rush” during the 1800’s was responsible for the rapid expansion of our area.
The rocks in the Tees Valley are up to 250 million years old.
The area is an internationally important place for Jurassic plant fossils.
The remains of large reptiles and dinosaur footprints can be found throughout the Jurassic rocks in the area.
Coal was once mined at Danby.
Salt extraction at Billingham gave birth to the chemical industry boom on Teesside today.
The first public toilets in Hull were built to collect urine used in the production of Alum throughout Cleveland and North Yorkshire.
Only 10,000 years ago the Tees Valley was in the grip of the last ice age and was buried under hundreds of metres of ice.
Jet was mined all over Cleveland in places like Guisborough, Carlton and Eston, not just at Whitby.
A surge of molten rock ripped through the area leaving behind the Cleveland Dyke, resulting in the Langbaurgh Ridge feature at Great Ayton.
Geological Survey Details
As part of the Tees Valley Geodiversity Action Plan the Tees Valley Wildlife Trust and the Tees Valley RIGS group surveyed the geology of the Tees Valley. As a result of this year long survey nearly all exposures have been logged and compiled on the GAP Database. The database illustrates where people can go to access the geology of the Tees Valley and also explains what they are observing.
The GAP Database is available to view online or at every public library throughout the Tees Valley.
Click here to access the GAP database
(The database will open in a new window, simply close the GAP window to return to this site)