Orcombe Point
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Orcombe Point is a coastal feature near
Exmouth Exmouth is a harbor, port town, civil parishes in England, civil parish and seaside resort situated on the east bank of the mouth of the River Exe, southeast of Exeter. In 2011 it had a population of 34,432, making Exmouth the List of settl ...
,
Devon Devon ( ; historically also known as Devonshire , ) is a ceremonial county in South West England. It is bordered by the Bristol Channel to the north, Somerset and Dorset to the east, the English Channel to the south, and Cornwall to the west ...
, on the south coast of England. It lies about south of the city of
Exeter Exeter ( ) is a City status in the United Kingdom, cathedral city and the county town of Devon in South West England. It is situated on the River Exe, approximately northeast of Plymouth and southwest of Bristol. In Roman Britain, Exeter w ...
, southeast of Exmouth town centre and about southwest of
Sidmouth Sidmouth () is a town on the English Channel in Devon, South West England, southeast of Exeter. With a population of 13,258 in 2021, it is a tourist resort and a gateway to the Jurassic Coast World Heritage Site. A large part of the town has ...
. Directly to the west lies Exmouth Beach and to the east is Sandy Bay, a holiday beach, that can be reached either along the coastal path or through the large caravan park. The two beaches are part of a long strip of sand and are connected to each other below Orcombe Point at low tide. Sited high upon the hill, Orcombe Point is marked by the "Geoneedle", which was unveiled by
Prince Charles Charles III (Charles Philip Arthur George; born 14 November 1948) is King of the United Kingdom and the 14 other Commonwealth realms. Charles was born at Buckingham Palace during the reign of his maternal grandfather, King George VI, and ...
, in 2002, at the inauguration. The artist whose conceived and designed the "Geoneedle" sculpture was Michael Fairfax. Michael Fairfax. He also conceived and designed the "Exeter Riddle" in
Exeter Exeter ( ) is a City status in the United Kingdom, cathedral city and the county town of Devon in South West England. It is situated on the River Exe, approximately northeast of Plymouth and southwest of Bristol. In Roman Britain, Exeter w ...
. The Geoneedle is constructed from a variety of different stones, representing both the major building stones to be found on the Jurassic Coast and the sequence of rocks that form this part of the coastline.


Geology

The rocks dip gently to the east. Due to this tilting and erosion the oldest exposed rocks are found here in the west, with progressively younger rocks forming the cliffs further east. The coastal exposures along the coastline provide a continuous sequence of
Triassic The Triassic ( ; sometimes symbolized šŸˆ) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is t ...
,
Jurassic The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. ...
and
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ...
rock formations spanning approximately 185 million years of the Earth's history. The localities along the Jurassic Coast includes a large range of important
fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserve ...
zones. Orcombe Point is the western end of the Jurassic CoastJurassic Coast Mini-Guide (2021 edition)
and the
South West Coast Path The South West Coast Path is England's longest waymarked Long-distance footpaths in the UK, long-distance footpath and a National Trail. It stretches for , running from Minehead in Somerset, along the coasts of Devon and Cornwall, to Poole Harb ...
includes the entire length of the site. The ascent to Orcombe Point shows the successive layers of different
sedimentary rock Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or de ...
s, which were deposited under varying
geological Geology (). is a branch of natural science concerned with the Earth and other astronomical objects, the rocks of which they are composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth s ...
conditions. At the base are
cross-bedded In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original ...
sandstone Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
s. Towards the top, the rock types are those deposited by quieter, slower-flowing waters (i.e.
siltstone Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility. Although its permeabil ...
s and
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from ''shale'' by its lack of fissility.Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, ...
s). The sediments are markedly red and this indicates that they were formed in a desert. These formations belong to the Aylesbeare Mudstone Group and date from the Triassic period 250 million years ago.


References

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