Hawkes Tor, Bodmin - by Martin Hunt Engine House, Crows nest, Bodmin - by Pat Sargeant Cape Cornwall - by Beth Tonkin
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COASTLINE

Cornwall's spectacular coastline stretches for over 400 miles - the longest of any county. And what a variety we have!

Boscastle Coastline, North Cornwall - by Pat Sargeant

See the Coastline geological timeline >>

Logan Rock, W Penwith - by Pat SargeantHow about taking on the challenge of 731 feet high cliffs between Bude and Boscastle; across the sandy beaches and golden dunes of Penhale, Perranporth and Gwithian; around the granite peninsula of Land's End; past Lizard Point, the most southerly place on mainland Britain; then meander around the beautiful south coast estuaries and headlands from the Fal to the Tamar. Every mile controlled by the rocks under your feet and the continual action of the sea, wind, time and tide.



Helford river - by Pat SargeantThe coast is probably our most dramatic and dynamic environment and therehave been some amazing changes since the end ofthe last Ice Age only 12,000 years ago. Sea level has fluctuated like a see-saw. Imagine being able to walk to France when the English Channel was an enormous river valley. You could have done this as recently as 8,000 years ago because much of the Earth's sea water was still locked up in the polar ice sheets. At the height of the last Ice Age sea level was about 400 feet lower than today and all of Cornwall's rivers cut long deep valleys. As the ice sheets melted sea level rose again submerging woodlands and forests that became fossilised. Our estuaries were flooded to form the deep water rias that now provide the sheltered harbours and anchorages along the south Cornwall coast.

by Beth TonkinRaised beaches provide evidence of even higher sea levels, some dating back to pre-glacial times. We even have curious glacial debris or erratics left behind from the Ice Age. Then Cornwall had a climate similar to present day Siberia or northern Canada. Rocks were shattered by the freezing conditions and ice-bergs floated offshore. On land the frost shattered debris, known as Head, accumulated on coastal and valley slopes, and massive dust storms deposited layers of fine sand or loess across much of the county.

Experts tell us that sea level is still rising, the climate is changing and Cornwall is still sinking. Parts of Cornwall even bounce by about 4 inches everytime the tide comes in and out twice a day, making Cornwall one of the bounciest places in Britain - honest!

So where should you go to see the best geological features that the Cornish coastline has to offer? Well what a choice!

Cliffs
by Pat Sargeant
Between Bude and Boscastle
by Pat Sargeant
The Land's End Peninsula
by Pat Sargeant
The Lizard
 
Shingle Bar
Collapsed Caves & Blowholes
by Peter Ealey
Loe Bar near Porthleven
by Peter Ealey
Lion's Den and The Devil's Frying Pan on The Lizard
 
Sand Dunes
by Pat Sargeant
Rock Dunes
by Pat Sargeant
Holywell Bay
by Pat Sargeant
Gwithian Dunes
by Pat Sargeant
St. Martin's on the Isles of Scilly
Rias
by Pat Sargeant
Fal and Helford Estuaries
by Pat Sargeant
Fowey Estuary
 

Raised Beaches

by Peter Ealey
Godrevy
by John Macadam
Pendower guide
by Peter Ealey
Porthallow
 
Tombolo

by Pat Sargeant

The Tombolo linking Gugh to St. Agnes, Isles of Scilly
* A World apart from Tombola, I promise!
Glacial Erratics

by Beth Tonkin

The Giant's Rock, Porthleven
 

Submerged Forests & Landscapes

from the Royal Cornwall Museum
Mount's Bay, Penzance

by Pat Sargeant
Samson Flats, Isles of Scilly
 

Remember that all of these amazing locations (except for those on the Isles of Scilly) can be reached from the South West Coast Path that traverses the whole coastline. And with links inland you can make some spectacular round walks. Let me suggest one of my favourites to you.

Click here for a list of Photograph credits

Granites | The Lizard | Killas | Coastline


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