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You are currently here: Home > Fossil Locations > South East > Folkestone |
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Introduction
Folkestone if one of the best places on the south coast for fossils. The range and quality and volume of fossils make this an excellent destination. Access to the beach is convenient, with plenty of parking and facilities, including toilets.
If the weather has been wet, be sure to bring wellies or walking boots, as the clay is both wet and muddy.
The earliest rocks at Folkestone consist of Lower Greensand exposed to the north of the town and run through a sequence of Lower Greensand, Gault Clay (phasing into Upper Greensand) and Chalk, the whole sequence dating from approximately 120 to 80 million years old. The chalk increases in thickness to the north culminating with the famous white cliffs of Dover before dipping off to the north approaching Deal.
It is the Gault Clay that is of particular interest; it is a dark blue-grey colour and has been extensively studied. The clay consists of mudstones with layers of phosphate nodules that delineate the margins of some of the clay beds, the whole Gault sequence achieves a thickness of 40m in places. The clay has been sub-divided into thirteen individual beds, each containing diagnostic fossil species and dates from the Middle to the Late Albian of the Cretaceous period, approximately 108-97.5mya. The clay from the Middle Albian is known as the Lower Gault and the beds from the Late Albian are known as the Upper Gault. The Upper Gault is more calcareous than the Lower Gault mudstones and is somewhat lighter in colour. Although both the greensands and chalk all contain fossils including ammonites, the preservation is by far the best in the clay.
Where to look for fossils?
Fossils can be found all year round, but the best finds are made following periods of wet weather when the clay is soft. However, during the summer months visitors can still find a large number of fossils within the boulders and rock pools.
(Left) Searching for fossils among the boulders and rock pools. (Right) Paul examining cliff face
Searching for fossils on the foreshore requires a hands on approach! The fossils here have been washed out from the cliff and are often buried by shingle and soft clay. A small trowel is a great tool for uncovering the fossils, while some people prefer to dig with their hands! Either way, a large number of fossil fragments and complete specimens can be found this way.
A bottle of tap water is also advisable to wash finds on the spot if one is curious and wishes to wash the clay off there and then. One is advised to take a bag and newspaper to keep the specimens safe and free from knocking into each other.
For more information about the features and processes controlling coastal fossil collecting locations click here.
What fossils might you find?
The Gault contains the fossils of many forms of marine creature; ammonites, belemnites, nautilus, bivalves, crinoids, gastropods, fish remains, and scaphopods are quite common along with rare finds of reptilia. Ichthyosaur vertebrae have been found in association with the smaller fauna though by far the most common fossils are the small shelly forms. In some of the clay bed sequences the fossils are preserved in phosphate; they tend to be dark, frequently broken and are often in concreted masses. The best preserved fossils are those that are pyritised, the preservation of these pyritised animal remains in the some of the Lower Gault beds is exceptional, shells tend to be preserved in their original proportions and are generally not crushed. Sometimes a beautiful coating of iridescent mother-of-pearl is to be found though this is usually partial or flaked off entirely. They do require careful preservation (more on that subject later).
Two excellent ammonite specimens from the foreshore (Left - Anahoplites planus) (Right - Euhoplites aspasia).
Special
finds
(Left) Protosphyraena tooth. (Right) Artist impression of Protosphyraena - Fig 1, and actual skull example - Fig 2
Protosphyraena
is believed to have grown up to twice the size of an average man. They
were armed with a long, strong weapon at the extremity of the upper jaw, something like that of a sword-fish, but round and pointed and composed of strong
fibres. The jaws are provided with three kinds of teeth. On the outer edge is a row of large, flat, cutting teeth, somewhat resembling those of a shark. Inside, and placed irregularly, are small, blunt teeth; while in the back portion of the palate is the third set- small, sharp and needle-like in shape, forming a
pavement.
Two small ammonites found within the cliff face.
(Left) Tiny ammonite found in a rock pool - Hysteroceras. (Right) well preserved pyrite ammonite - Hoplites dentatus.
(Left) Small Belemnite - Neohibolites. (Right) Small Shark tooth
(Left) Hamites - hetromorph ammonite. (Right) Small bi-valve.
(Left) Fish jaw including several teeth. (Right) Small fish vertebrae.
(Left) Robert's ammonite Hoplites spathi. (Right) Close-up of Hoplites spathi crystals.
Protecting your finds
It's important to spend some time considering the best way to protect your finds onsite, in transit, on display and in storage. Prior to your visit, consider the equipment and accessories you're likely to need, as these will differ depending on the type of rock, terrain and prevailing weather conditions.
(Left) Fossil wrapped in newspaper, ready for transport. (Right) A small compartment box containing cotton wool is ideal for separating delicate specimens.
When you discover a fossil, examine the surrounding matrix (rock) and consider how best to remove the specimen without breaking it; patience and consideration are key. The aim of extraction is to remove the specimen with some of the matrix attached, as this will provide added protection during transit and future handling; sometimes breaks are unavoidable, but with care you should be able to extract most specimens intact. In the event of breakage, carefully gather all the pieces together, as in most cases repairs can be made at a later time...continued.
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