Jurassic Coast

Durdle Door - The natural arch

durdle_door-250Location: Durdle Door near Lulworth

Rock Type: Limestone

Age: Jurassic 140 million years old

Features of Note: Natural rock arch, ripple marks and Fossil Forest remnants.

The geology in detail

Hard layers of Portland Limestone have been folded on this part of the coast so that they appear almost vertical and these form the seaward edge of the small promontory here that includes the arch known as Durdle Door. The type of rock is known as an Oolitic Limestone and is made up of tiny balls of calcium carbonate and is famously quarried on Portland. On parts of the vertical face of the landward side of the arch there are preserved ripple marks, formed where the water was shallow enough so that the sea bed was disturbed by the waves. There are also holes that would have once contained fossil wood.

The ancient environment

Oolitic limestones are known to form in shallow warm seas very like those found in the Bahamas today, where modern oolitic sand forms on the sea bed.

The rock arch

The impressive arch of Durdle Door 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 sea would have begun to breach the hard Portland Limestone and form a string of caves along the coast. The much softer rocks behind would have quickly been eroded away creating caves and natural arches. Eventually the arches collapsed leaving stacks, which would in turn be broken and washed away by the power of the waves. And so, the Portland stone was slowly stripped from the coast, Durdle Door is part of only a small strip that is left here. The remnants of old arches can still be seen in the form of ‘stumps' of limestone only just visible in the waves. One day that is all that will remain of Durdle Door.
Geo highlights

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