|
World Class Geology in North-East Yorkshire
North and East Yorkshire have some of the best Jurassic and Cretaceous geology in the world.
Erosion of the massive cliffs reveals an array of spectacular fossils.
The deep valleys formed during the last Ice Age give many inland exposures and spectacular beauty spots.
The wide range of fossils provides evidence for the changing environment of tropical seas, rivers and swamps in the region’s ancient past. |
 |
 |
Scarborough Museums & Gallery
Scarborough Museums and Gallery has one of the foremost collections of Jurassic geology on the Yorkshire Coast.
With over 5500 fossils and 3000 minerals, the strengths of the collection include: numerous type specimens, which were the first of their kind ever to be described and one finest collections of Middle Jurassic fossil plants in the country. |
The collection also includes a large selection of Cretaceous fossils from the Speeton Clay and the Chalk, a wide variety of Upper and Lower Jurassic specimens, specimens from the Ice Age such as mammoth teeth and fossils from the Kirkdale Cave and a pristine Carboniferous plant collection.
Currently, the collection is being catalogued and conserved in preparation for redisplay in the Rotunda Museum, where William Smith (The Father of English Geology) originally envisaged their home.
Spectacular specimens have been chosen from the collection to go on temporary display in Wood End Museum and on this website. This gives a taste of the quality and range of our fossils and minerals that due to limited exhibition space, are often in storage. |
 |

 |
Whitby Museum
Whitby Museum has one of the foremost collections of Jurassic geology on the Yorkshire Coast.
The unique collection focusing on material local to Whitby, contains over 6500 fossils and minerals.
The museum is famous for the spectacular marine reptiles (including Plesiosaurs and Ichthyosaurs) set into the museum walls. |
The geology is currently being redisplayed and now takes you on a journey through the tropical seas of the Lower Jurassic, onto the lush deltas of the Middle Jurassic and into the warm seas of the Upper Jurassic. Also explored, are the animals and landscape of the last Ice Age, the geology of Whitby today, the alum industry and local geology pioneers.
The main strengths of the collection are: a wide selection of internationally important Lower Jurassic fossils, ranging from large marine reptiles, such as Plesiosaurs, Ichthyosaurs and a crocodile, to ammonites, belemnites and fish; an extensive collection of Middle Jurassic plants; a collection of minerals from the alum mining industry; material from the last Ice Age. Unusually, many type fossils, which are the first of their kind ever to be described, are on display. |
 |
Spectacular specimens have been chosen from the collection to go on temporary display in the museum and on this website. This gives a taste of the quality and range of our fossils and minerals that due to limited exhibition space, are often in storage.
 |
Geology sites
This area is very important for looking at geology because there is so much to see compared to other places.
The rugged coastline provides slices through the rocks that are often more than a hundred metres thick and are much more complete and extensive than elsewhere.
This means it is easy to see how the fossils change as the rocks get older or younger. In the rest of the UK, the same rocks are usually hidden deep beneath the ground. Smaller exposures complete the picture inland.
Clues to the more recent geological past are seen in the spectacular landscape of valleys and hills formed in the Last Ice Age. |
The last Ice Age (over 10 000 years ago)
During the last Ice Age the North Sea was covered by ice (often hundreds of metres thick), leaving much of Yorkshire as a frozen wasteland. Many creatures thrived in these harsh conditions, living off the stunted vegetation and preying on other animals. The evidence for this period of change is mostly seen in the carved landscape, but also in extensive deposits of boulder clay and other glacial debris.

|
Scarborough Museum
The collection provides evidence of the wide range of the animals that roamed this harsh environment.Specimens include massive mammoth teeth and Hyena bones. |

|
Whitby Museum
The collection contains a wide range of erratic rocks brought to Whitby by the ice, often over vast distances. Massive mammoth teeth, antlers and bison bones provide evidence for the wide diversity of life at this time. |
Where can I find this geology?
There are many examples in North and East Yorkshire of how the landscape that has been altered during the Last Ice Age. Spectacular valleys such as Newton Dale and Forge Valley cut through the landscape. These were formed when glacial lakes dammed by the ice, escaped through geological weak points to release massive torrents.
The boulder clay dumped by the retreating ice can be seen mostly between Scarborough and the River Humber, but good examples are at Filey Brigg and Holbeck Hall landslip (on the south side of Scarborough) where the unstable boulder clay has slipped into the sea.
Numerous erratic boulders litter the landscape, giving a glimpse of the massive power of the ice. These boulders, which are often very large, have been brought in the ice from as far a field as Scotland, the Lake District and even Scandinavia. They were then dumped when the ice melted. A large example can be seen near the entrance to Seamer station, near Scarborough, smaller examples litter the coast and are
easily picked out at places such as Robin Hood’s Bay. |
 |

The Cretaceous (about 65 to 135 million years ago)
During the Cretaceous millions of micro-organisms swarmed in the warm sub-tropical seas. They died and gradually sank to the sea floor, creating the chalk that now forms the towering cliffs at Flamborough Head. The seafloor was covered in abundant life, ranging from sea urchins (echinoids) to corals, whilst sharks and marine reptiles swam above. The soft white chalk forms towering white cliffs and rolling countryside.

|
Scarborough Museum
The collection includes some fantastic examples of sponges, echinoids, sharks teeth, lobsters and ammonites, often preserved in spectacular detail. |
|
Whitby Museum
There is a small collection of Cretaceous fossils at the Museum. This includes sponges and echinoids from the Chalk and various other fossils such as ammonites from the Speeton Clay. |
 |
Where can I find this geology?
The best place to see the chalk in East Yorkshire is Flamborough Head and Bempton (there are no exposures in North Yorkshire). Here, the chalk forms towering cliffs several hundred metres high and is eroded into sea stacks and arches.
Inland, the soft rocks are quickly covered by vegetation, forming the low rolling countryside of the Yorkshire Wolds, around Bridlington and Driffield. |
The Upper Jurassic (about 135 to 152 million years ago)
During the Upper Jurassic Yorkshire was covered by warm shallow seas. Many large marine reptiles, such as Plesiosaurs swam through the water above a seabed rich in animal life. Corals, sea snails and shellfish covered the sea floor, whilst a rich community of ammonites, belemnites and other animals swam above.
The Upper Jurassic rocks are mostly limestones and sandstones. These come in a rich creamy colour, which can be seen in many of the North Yorkshire towns and villages such as Ayton, Helmsley and Pickering. Particularly distinctive are the oolite rocks that are made up of many millions of tiny bead shaped grains of limestone.
|
Scarborough Museum
The collection illustrates this rich environment with spectacular fossils such as ammonites, echinoids, starfish, bivalves and corals. |

|
Whitby Museum
Whitby Museum has a small collection of Upper Jurassic fossils, including bivalves and echinoids. |
Where can I find this geology?
This geology forms the distinctive Tabular Hills inland from Scarborough and Whitby. The hills are flat topped and have very steep sides where the hard rocks such as the Lower Calcareous Grit, come to the surface.
Particularly good exposures can be seen in Forge Valley, at Cayton Bay and at Castle Headland, Scarborough. |
 |
The Middle Jurassic (about 152 to 180 million years ago)
The Middle Jurassic was dominated by ever changing river channels that snaked across the landscape, occasionally flooding to bury the plant and animal life. Lush sub-tropical vegetation flanked the rivers and numerous dinosaurs roamed the banks feeding on the plants and stalking prey.
The Middle Jurassic rocks are dominated by sandstones, often showing well developed cross-bedding. These rocks contain casts of dinosaur footprints, but few delicate fossils. Thinner deposits of mudstone contain several plant beds, which preserve leaves, seeds and flowers in amazing detail.
|
Scarborough Museum
The spectacular plants from this period are one of the stars of the collection. Slabs full of Gingko
leaves, ferns and cycads, are complimented by a range of dinosaur footprints and spectacular bones. These fossils make the collection one of the most important of its type in the country. |

|
Whitby Museum
The collection contains a fantastic array of plant fossils. The imprints of ferns, cycads and Ginkgos give a glimpse of the lush tropical vegetation. The vegetation supported numerous dinosaurs, shown by the footprints in the collection. |
 |
Where can I find this geology?
One of the best places to find this geology is on the coast, between Scalby Mills and Ravenscar and at Whitby.
Here the cliffs are made up of massive sandstones, sometimes containing dinosaur footprints.
Inland, the Middle Jurassic rocks can be found under much of the heather moorland. |
The Lower Jurassic (about 180 to 205 million years ago)
The Lower Jurassic was covered by a warm moderately deep sea. Large marine reptiles, such as Plesiosaurs and Ichthyosaurs glided through water chasing prey such as ammonites and belemnites. The rich sea-floor life included crinoids and shellfish.
These rocks form dark coloured shales and limestones, they are often quite soft and preserve very fine details of the fossils. They tend to form towering cliffs, which are slowly eroded away by the North Sea.

|
Scarborough Museum
The Lower Jurassic collection includes some of the best-preserved ammonites, belemnites, fish and marine reptile bones from the area. Unusual specimens such as lobsters and echinoids are also represented. |

|
Whitby Museum
Whitby Museum is famous for its collection of Lower Jurassic fossils, which includes some of the best-preserved large marine reptiles from the area. A wide range of ammonites, belemnites and fish are also displayed.
|
| The spectacular ammonite fossils can be used to show the evolutionary changes that took place at this time. Unusual specimens such as lobsters and echinoids are also represented. These fossils make the collection one of the most important of its type in the country. |
 |
Where can I find this geology?
Some of the best places to see these rocks are around Whitby and Robin Hood’s Bay.
The large quarries at Ravenscar are an excellent place to visit the remains of the alum industry that exploited these rocks. |
Enquiries
 |
If you have a fossil that you want us to identify, please contact Dave Gelsthorpe and bring it along to Scarborough or Whitby Museum. |
 |
If you live outside the Dinosaur Coast, your local museum will be able to direct you to someone who can help. |
 |
If you have a scientific enquiry about the collections, please contact Dave Gelsthorpe with specific details. |
 |
If you have an enquiry about the Dinosaur Coast contact Will Watts. |
|
 |
Safe and responsible collecting coming soon!
|