Lulworth Cove and Crumple - A Geography Pilgrimage

lulworth-cove-250Location: Lulworth

Rock Type: Limestone, clay, sandstone and chalk

Age: 140 - 70 million years old

Look out for: the hard rocks at the mouth of the cove erode much more slowly than the rocks behind giving the cove its horseshoe shape.

The geology in detail

The rock layers on this part of the coast have been folded so that the layers appear almost vertical. Hard Portland and Purbeck Stone forms the cliffs with much softer Wealdon Clay, Gault and Greensand behind with the chalk forming the back of the cove. This is an internationally renowned place for the study of different rates of erosion in the formation of bayes and headlands. Below is a brief description of these various rock sequences.

Portland Stone - Oolitic limestone that formed at the end of the Jurassic in warm shallow water very much like the Bahamas.

Purbeck Stone - A series of thin layers of limestone and clay that formed in swamps.

Wealdon Clay - Clay and sandstone layers that were layed down in rivers flowing from the west (the sandstone layers contain quartz grains eroded from Dartmoor Granite over 120 million years ago)

Gault - A soft clay formed in a still marine environment. It is rarely exposed well because it is so soft.

Greensand - Generally quite soft sandstone containing the green mineral glauconte. It formed in a shallow sea and often contins abundant trace fossils (burrows)

Chalk - An almost pure limestone that formed at the end of the Cretaceous in a warm 200 - 300m deep sea. It is made up almost entirely of the microscopic skeletons of plankton. 

The formation of the Cove

The attractive form of Lulworth Cove formed due to the effect of the erosive power of the sea on the vertical layers of different types of rock. At some point in the past the river would have punched a hole in the hard Portland Limestone that formed the cliffs. Once the sea could breach those rocks it quickly eroded the much softer rocks behind, widening the gap and creating the rounded cove. This process has happened in several places along the coast here and is still happening. At Man ‘O War Cove to the west of Lulworth, two old coves have been eroded to form one with only a string of reefs showing where the Portland Stone once was. And Stair Hole just next to Lulworth is a new cove in the making. Eventually it will join up with Lulworth Cove.

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Dorset and East Devon's World Heritage Coast

 
 
 
 
  • Triassic250-200 million years old
  • Jurassic200-145 million years old
  • Cretaceous145-65 million years old