Creswell Crags

Information about Creswell Crags

Map sources for Creswell Crags at grid reference SK536741
Creswell Crags is a limestone gorge in North East Derbyshire, England near the villages of Creswell and Whitwell. The cliffs of the ravine contain several caves that were occupied during the last ice age, between around 43,000 and 10,000 years ago.

The caves contain occupation layers with evidence of flint tools from the Mousterian, proto-Solutrean, Creswellian and Maglemosian cultures. They were seasonally occupied by nomadic groups of people during the Upper Palaeolithic and Mesolithic periods. Evidence of Neolithic, Bronze Age, Roman and post-medieval activity has also been found there. The main phases of stone age occupation were at around 43,000 BC then in a period between 30,000 and 28,000 BC and then again around 10,000 BC.

A bone engraved with a horse's head and other worked bone items along with the remains of a wide variety of prehistoric animals have been found in excavations from 1875 to the present day. Early excavations were carried out by Professor Sir William Boyd Dawkins, who wrote several papers on his findings.The site is open to the public and there is a visitor's centre.

In April 2003, engravings and bas-reliefs were found on the walls and ceilings of some of the caves; an important find as it had previously been thought that no British cave art existed. To this day the finds at Creswell Crags represent the only known examples of Palaeolithic cave art in Britain, the most northerly finds in Europe and the most extensive collection of prehistoric bas-reliefs in the world. Their subject matter includes representations of animals including bison and several different bird species. The engravers seem to have made use of the naturally uneven cave surface in their carvings and it is likely that they relied on the early morning sunlight entering the caves to illuminate the art. Thin layers of calcium carbonate flowstone overlaying some of the engravings were dated using the uranium-series disequilibrium method, which showed the oldest of these flowstones to have formed 12,800 years ago. This provides a minimum age for the underlying engraving. The scientists and archaeologists concluded it was most likely the engravings were contemporary with evidence for occupation at the site during the late glacial interstadial at around 13,000-15,000 years ago.

The most occupied caves were:
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Church Hole Cave, home to Palaeolithic etchings.
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Other caves at Creswell Crags.
  • Mother Grundy's Parlour, which has produced numerous flint tools and split bones and was occupied until the Mesolithic;
  • Robin Hood's Cave, from which was recovered the horse head-engraved bone and also evidence that its occupants were hunting and trapping woolly rhinoceroses and arctic hares;
  • The Pin Hole, a prehistoric hyena den and also occupied by Neandertals. Finds include a bone engraved with a human figure and an ivory pin with etched lines;
  • Church Hole, which has more than 80 engravings on its walls and was occupied intermittently until Roman times.
As a result of its unique features, Creswell Crags has been designated as a Site of Special Scientific Interest (SSSI).

It is the subject of BBC radio 4 documentaries, Unearthing Mysteries and Nature, which can both be listened to using the links section below. Creswell Crags also featured in the 2005 TV programme Seven Natural Wonders as one of the wonders of the Midlands.

References

  • Dawkins W.B, (1877) On mammal fauna of the caves of Cresswell Crags. Quarterly Journal of the Geological Society, 33, pp589 – 612
  • Dawkins W.B and Mello J.M., (1879), Further discoveries in the Cresswell Crags. Quarterly Journal of the Geological Society, 35, pp724 – 735

External links

Coordinates:

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The Ordnance Survey (OS) devised the national grid reference system, and it is heavily used in their survey data,
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Limestone is a sedimentary rock composed largely of the mineral calcite (calcium carbonate: CaCO3). Limestone often contains variable amounts of silica in the form of chert or flint, as well as varying amounts of clay, silt and sand as disseminations, nodules, or layers
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canyon (rarely cañon) or gorge is a deep valley between cliffs often carved from the landscape by a river. Most canyons were formed by a process of long-time erosion from a plateau level.
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Derbyshire (pronounced "dar-bee-sher" /ˈdɑːbɪʃə/, as opposed to "dar-bee-shire") is a county in the East Midlands of England. A substantial portion of the Peak District National Park lies within Derbyshire.
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Creswell

Creswell, Derbyshire ()
|240px|Creswell, Derbyshire (

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Whitwell

Whitwell, Derbyshire ()
|240px|Whitwell, Derbyshire (

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cliff or bluff is a significant vertical, or near vertical, rock exposure. Cliffs are categorized as erosion landforms due to the processes of erosion and weathering that produce them. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers.
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A ravine is a very small valley, which is often the product of streamcutting erosion. Often found in urban areas, ravines are typically classified as larger in scale than gullies, although smaller than valleys.
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cave is a natural underground void large enough for a human to enter. Some people suggest that the term 'cave' should only apply to cavities that have some part which does not receive daylight; however, in popular usage, the term includes smaller spaces like sea caves, rock
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ice age is a period of long-term reduction in the temperature of Earth's climate, resulting in an expansion of the continental ice sheets, polar ice sheets and mountain glaciers.
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Flint tools were made by stone age peoples worldwide. Paleolithic tools were relatively simple, repeated small flakes being struck or pressed from a flint until the required shape was achieved.
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Mousterian is a name given by archaeologists to a style of predominantly flint tools (or industry) associated primarily with Homo neanderthalensis and dating to the Middle Paleolithic, the middle part of the Old Stone Age.
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Solutrean industry was a relatively advanced flint tool making style of the Upper Palaeolithic.

It is named after the type-site of Solutré in the Mâcon district, Saône-et-Loire, eastern France and appeared around 19,000 BCE.
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The Creswellian is a British Upper Palaeolithic culture named after the type site of Creswell Crags in Derbyshire by Dorothy Garrod in 1926. It dates to between c. 12,500 and 12,000 BP and was replaced by the Mesolithic Maglemosian culture.
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Maglemosian (ca 7500 BC- ca 6000 BC) is the name given to a culture of the early Mesolithic period in Northern Europe. In Scandinavia, the culture is succeeded by the Kongemose culture.
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