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New homes The wider regeneration. Lyme Regis, in Dorset, which is known for its ammonites, has around 40 different species.

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Chalk gives you the most diverse habitat. Take a bottle of water with you to help you on your way back to the top!

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They then crashed down like a massive waterfall over the cliffs we have and plummeted into the sea. The landbridge between Britain and France was much more recent, in geologic terms, being in existence aboutyears ago. You can have up to 40 to 50 different species of plants per square metre in chalky grassland.

The Warren holds around ammonite species as they were evolving at such a rate. This category only includes cookies that ensures basic functionalities and security features of the website. What the team found were these huge plunge pools under the sea.

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But opting out of some of these cookies may have an effect on your browsing experience. There are paths leading down, through the metre high cliffs to the sea front. The Victorians were big collectors and this is when you start seeing people becoming interested in visiting all these places. These cookies do not store any personal information.

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Out of these cookies, the cookies that are categorized as necessary are stored on your browser as they are essential for the working of basic functionalities of the website. Toggle Search.

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On top of that we have the Gault Clay which is a bit younger, and sitting on top of that is the chalk. When they died, they dropped to the bottom of the sea forming a porridge-like sediment that got compacted over time and formed the chalk.

It is mandatory to procure user consent prior to running these cookies on your website. I love these plants. When they died, they would have fallen to the seabed as well, and once compressed we find ourselves with flint rocks! And so, at the end of the last ice age, around 10 to 12, years ago, the first lands to be cleared of forests were around chalky areas as Stone Age man learned how to nap flints, making tools to cut down the trees.

The Warren is a wonderful place to walk dogs, and, importantly, they are allowed here all year round. And what was happening at this time was the organisms were evolving so quickly that you can see their development happening in the fossils you find here.

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The zig-zag path draws you up into the tumbling fauna of the cliffs. So, at the time the chalk was being formed, there was runaway climate warming.

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It keeps the the more vigorous species that would swamp everything else out. The greenhouse effect had melted the polar ice caps, so there was no ice at either pole. You can find the curly Ammonites, and the Belemnite fossils which are the bone-type structure you find inside little squid-like creatures. And what was creating all those greenhouse gasses were lo of volcanoes going off. Close Privacy Overview This website uses cookies to improve your experience while you navigate through the website.


The rocks at The Warren indicate an ancient constantly changing sea level. They might look quite weedy to some, but actually, during the Cretaceous period they were as huge as trees! The sequence of fossils that the area holds is so complete that you can use it to date other sediment of a similar age from around the world.

You can unsubscribe at any time by following the steps contained in the particular message. Foraging in Folkestone — Living in our Environment. Across the country you will find important collections of fossils taken from The Warren in regional museums. We also use third-party cookies that help us analyze and understand how you use this website. Necessary Necessary. Up until this point, the creation of the English Channel had been up for debate.

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The White Cliffs country continues from Dover into Folkestone but here, the bedrock is Lower Greensand and Gault clay with the white cliffs at the back. This website uses cookies to improve your experience.

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In these warm seas, along with the Coccoliths are lots of zooplankton or animal plankton. The fossils are marine animals and pieces of driftwood. Fossils get washed out of the clay by the sea and can be found easily on the beach.

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When the Channel Tunnel was being built, they needed to re-direct the route of the tunnel to avoid some of these huge shafts going right down into the sea. Non Necessary non-necessary.

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And so the more delicate species like the herbs and the orchids can survive. The rocks at The Warren are about to 90 million years old. So now, we can walk around this terrain and find rather small examples of what animals much larger than us would have found to eat. Now, their skeletons are made up of silica, a glass-like substance.

You also have the option to opt-out of these cookies. You can see Samphire Hoe in the distance; this is the landmass created by the spoil from the Channel Tunnel in Wild samphire grows here, as does wild cabbage and rock sea lavender. Imagine a layer cake, and at the bottom we have the Lower Green Sand, and then the sticky Gault Clay, now, what happens next is the chalky layer forms. Take your binoculars to find over species of native birds, and there are some impressive butterflies to spot too. Accept. The dinosaurs loved eating them. The Warren certainly is an incredibly important geological area.

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The highest sea level ever on planet Earth. Any cookies that may not be particularly necessary for the website to function and is used specifically to collect user personal data via analytics,other embedded contents are termed as non-necessary cookies. This has formed the undulating, undercliff landscape. This clay was formed in a deep-sea environment a long way from land. At the end of the last Ice Age, when the glaciers were melting, there were channels of water flowing at great speed across the land.

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Necessary cookies are absolutely essential for the website to function properly. These cookies will be stored in your browser only with your consent. You can see lots of examples of local flint tools in the Folkestone Museumalong with lots of fossils found from The Warren, and evidence of dinosaurs. Those continental plates meet, folding down underneath the next plate they reach and this is where you get earthquakes. Their skeletons are what makes the chalk.

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