Blue Bell Hill and Culand Pits

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Blue Bell Hill picnic site is a stunning viewpoint that looks out across the Medway valley and to the Weald.

Maidstone

Open dawn to dusk

Free

Viewpoint

Facilities

  • Car parking
  • Picnic area
  • Visitor information available

Geosite details

Blue Bell Hill picnic site is a stunning viewpoint that looks out across the Medway valley and to the Weald, when you stand here you are standing on relatively younger rocks and looking out over older rocks stretching back to over 100 million years old.  

The Medway valley that you can see from here has been hugely important to the cement industry since around 1850, and many of the villages and towns in this area developed because of the industry.

As you look out from Blue Bell Hill, in the foreground you can see some large excavated areas, these are the Culand Pits. The Culand Pits are great examples of sites connected to the cement industry, once upon a time clay was extracted for bricks and this was followed by chalk for the cement industry. The pits are now recognised for their geological significance as part of a Site of Special Scientific Interest (SSSI), in particular due to the marine and reptile fossils that have been found here. 

Managed by Kent Wildlife Trust, this site also includes Burham Down, which is home to special chalk grassland species. This Geosite encapsulates much of what is important in the Cross-Channel Geopark, as it is a great place to understand how the landscape evolved and was formed over millions of years, and how humans have interacted with this geodiversity. Nowadays we can see how these former industrial sites can be important for protecting and restoring biodiversity thanks in part to the unique geology that can be found here.  

The 'Big Bang'

13.8 billion years ago

Earth formed

4.6 billion years ago

 

540 million years ago

The Cambrian explosion of life: animals evolved and diversified as never before on Earth.

Devonian

419 million years ago

390 million years ago the oldest rocks you can see in the Geopark date back to the Middle Devonian. They are still quarried today in the Marquise basin in France.

Carboniferous

359 million years ago

Around 325 million years ago the Geopark was near the equator. The swamp forests from that period are preserved as coal, which was formerly mined in the Marquise basin in France as well as in East Kent and the Nord-Pas-de-Calais.

Permian

299 million years ago

Triassic

252 million years ago

210 million years ago the Geopark was in the centre of the Pangaea supercontinent, and dinosaurs roamed the land!

Jurassic

201 million years ago

150 million years ago the Geopark was submerged under the sea, the sands, clays, limestones, and sandstones that compose the Boulonnais region in France were deposited.

Cretaceous

145 million years ago

Over about 40 million years from 100-60 million years ago, Chalk formed at the bottom of a warm, shallow sea where the Geopark is located today. This was the first step towards the formation of our distinctive chalk landscape, which defines much of the Geopark.

Palaeogene

66 million years ago

Tectonic activity around 40 million years ago uplifted the territory of the Geopark by dozens of metres, creating an extensive chalk landscape that connected France and Great Britain.

Neogene

23 million years ago

Quaternary

2.6 million years ago

450,000 years ago, a megaflood destroyed the chalk ridge connecting Calais and Dover, creating the iconic white cliffs of the Geopark we see today

Getting here

Blue Bell Hill and Culand Pits

Common Road,
Blue Bell Hill,
Aylesford,
Kent,
ME5 9RG

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