The Old Harry Rocks are part of a chalk band that is around 65 million years old. But the rock band has only been submerged by the sea in the last few thousand years. The current rocks known as Old Harry and his wife are a few centuries old, with Harry's original "wife" having collapsed in 1509.
The 65Ma event was the KT Boundary, the end of the Cretaceous during which the chalk was formed. The subsequent uplift that formed the uplands from that Chalk was in the Tertiary, which followed the Cretaceous. The stacks themselves are no more than thousands of years old, as the Dorset coast retreated by marine erosion in the sea-level rise following the last Ice Age.
The Old Harry rocks are simply stacks left by erosion of the chalk cliff in Purbeck, which extends under the sea all the way to the Needles on the Isle of Wight.
· Old Harry was the first one to climb the rock so they called it Old Harry· The devil was known as Old Harry and he slept on the rock· The rock was named after Harry Paye, an infamous Poole pirate, who stored his contraband nearby.Old Harry was a well known Pirate around the area. It was simply named after him.
Old harry was a stack. Old harry was an old man who drove his ships in. His wife every night stood on the end of the rock holding a lamp out so Old Harry wouldn't crash his boat. One night old harry went out in his boat and his wife was in the pub. Old Harry's wife was drunk and was walking out along the stacks and fell off and died. Along came old harry in his boat and because there was no lamp he crashed his boat in to a millions of pieces and he died to. So that is how Old Harry the stack got its name.
Old harry's wife is called Henrietta. She is a stack which collapsed in the sea 1896. She is made out of chalk and her and her husband are found in swanage dorset.
Old Harry Rocks and Anvil Point are approximately 5 miles apart along the South West Coast Path in Dorset, England. It would take around 2-3 hours to walk this distance, depending on your pace and any stops you make along the way.
Old Harry Rocks located on the Jurassic Coast in England were originally a part of a chalk formation. Over time, erosion has worn away at the softer rock layers, creating three distinct formations: Old Harry, the lower Formation, and the Wave Cut Platform. These stages represent different periods of erosion and geological processes that have shaped the landscape over millions of years.
The reason why OHR (Old Harry Rocks) are called so, is because they were named after a famous pirate, Harry Paye, known as "Old Harry." A different legend claims that Old Harry is a euphemism for the devil (Satan).
the rocks had eroded
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Old Harry was widowed in 1896 as Old Harrys Wife died
a 4 figure grid refrence of old harry rock
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· Old Harry was the first one to climb the rock so they called it Old Harry· The devil was known as Old Harry and he slept on the rock· The rock was named after Harry Paye, an infamous Poole pirate, who stored his contraband nearby.Old Harry was a well known Pirate around the area. It was simply named after him.
1896
because aliens took over the WORLD!!
The Old Harry Rocks are England, and they have a stack and a stump.
Old harry was a stack. Old harry was an old man who drove his ships in. His wife every night stood on the end of the rock holding a lamp out so Old Harry wouldn't crash his boat. One night old harry went out in his boat and his wife was in the pub. Old Harry's wife was drunk and was walking out along the stacks and fell off and died. Along came old harry in his boat and because there was no lamp he crashed his boat in to a millions of pieces and he died to. So that is how Old Harry the stack got its name.
St. Lucas' Leap is the name of the gap separating the first stack of the Old Harry Rocks from the headland. The Old Harry Rocks are at the headland between the bays of Studland and Swanage on the southern coast of England. The name is in memory of a pedigree greyhound who died when it attempted to chase a hare near the Old Harry Rocks. The gap was apparently formed after the collapse of a natural arch feature that existed at the site.