Geographical range | Great Britain |
---|---|
Period | Upper Paleolithic |
Dates | between 13,000–11,800 BP [1] |
Type site | Creswell Crags |
Major sites | Gough's Cave, Kents Cavern |
The Creswellian is a British Upper Palaeolithic culture named after the type site of Creswell Crags in Derbyshire by Dorothy Garrod in 1926. [3] It is also known as the British Late Magdalenian. [4] According to Andreas Maier: "In current research, the Creswellian and Hamburgian are considered to be independent but closely related entities which are rooted in the Magdalenian." [5] The Creswellian is dated between 13,000 and 11,800 BP [1] and was followed by the most recent ice age, the Younger Dryas, when Britain was at times unoccupied by humans. [6]
The term Creswellian appeared for the first time in 1926 in Dorothy Garrod's The Upper Palaeolithic Age in Britain. This was the first academic publication [7] by the woman who in 1939 became the first woman ever to be elected as a professor at Cambridge. [8] It is also the first monograph about the Upper Paleolithic of Britain at the national level and it remained the only one on the subject for half a century. Garrod suggested that the British variant of the Magdalenian industry is different enough to create a specific name: [7]
"I propose tentatively "Creswellian", since Creswell Crags is the station in which it is found in greatest abundance and variety."
— Dorothy Garrod, The Upper Palaeolithic Age in Britain, Oxford, Clarendon Press, 1926, p. 194.
The definition of Creswellian was refined since then and now refers exclusively, in the British context, to the Late Magdalenian-style industry.
Diagnostic tools used to identify the period include trapezoidal backed blades called Cheddar points, variant forms known as Creswell points, and smaller bladelets. Other tool types include end scrapers made from long, straight blades. A special preparation technique was employed to remove blades from a core through striking in a single direction, leaving a distinct 'spur' on the platform. The tools were made using a soft hammerstone or an antler hammer.[ citation needed ]
Other finds include Baltic amber, mammoth ivory and animal teeth and bone. These were used to make harpoons, awls, beads and needles. Unusual bevelled ivory rods, known as sagaies have been found at Gough's Cave in Somerset and Kent's Cavern in Devon.
Twenty eight sites producing Cheddar points are known in England and Wales though none have so far been found in Scotland or Ireland, regions which it is thought were not colonised by humans until later. Most sites are caves but there is increasing evidence for open air activity and that preferred sources of flint were exploited and that tools travelled distances of up to 100 miles from their sources. Some of the flint at Gough's Cave came from the Vale of Pewsey [ citation needed ] in Wiltshire whilst non-local seashells and amber from the North Sea coast also indicate a highly mobile population. This matches evidence from the Magdelanian cultures elsewhere in Europe and may suggest that exchange of goods and the sending out of specialised expeditions seeking raw materials may have been practised. Analysis of debitage at occupation sites suggests that flint nodules were reduced in size at source and the lighter blades carried by Creswellian groups as 'toolkits' in order to reduce the weight carried.
Comparison of flint from Kent's Cavern and Creswell Crags has led some archaeologists to believe that they were made by the same group.[ citation needed ]
Food species eaten by Creswellian hunters focused on the wild horse ( Equus ferus ) or the red deer (Cervus elaphus), probably depending on the season, although the Arctic hare, reindeer, mammoth, Saiga antelope, wild cow, brown bear, lynx, Arctic fox and wolf were also exploited.
Highly fragmentary fossil bones were found in Gough's Cave at Cheddar. They had marks that suggested actions of skinning, dismembering, defleshing and marrow extraction. The excavations of 1986-1987 noted that human and animal remains were mixed, with no particular distribution or arrangement of the human bones. They also show the signs of the same treatments as the animal bones. These findings were interpreted in the sense of a nutritional cannibalism. However, slight differences from other sites in skull treatment leave open the possibility of elements of ritual cannibalism. [9]
The Red "Lady" of Paviland is an Upper Paleolithic partial male skeleton dyed in red ochre and buried in Wales 33,000 BP. The bones were discovered in 1823 by William Buckland in an archaeological dig at Goat's Hole Cave which is a limestone cave between Port Eynon and Rhossili on the Gower Peninsula, near Swansea in south Wales. Buckland believed the skeleton was a Roman era female. Later, William Solace examined Goat's Cave Paviland in 1912. There, Solace found flint arrow heads and tools and correctly concluded that the skeleton was in fact a male hunter-gatherer or warrior during the last Ice Age.
Creswell Crags is an enclosed limestone gorge on the border between Derbyshire and Nottinghamshire, England, near the villages of Creswell and Whitwell. The cliffs in the ravine contain several caves that were occupied during the last ice age, between around 43,000 and 10,000 years ago. Its caves contain the northernmost cave art in Europe. The evidence of occupation found in the rich series of sediments that accumulated over many thousands of years is regarded as internationally unique in demonstrating how prehistoric people managed to live at the extreme northernmost limits of their territory during the Late Pleistocene period.
Several species of humans have intermittently occupied Great Britain for almost a million years. The earliest evidence of human occupation around 900,000 years ago is at Happisburgh on the Norfolk coast, with stone tools and footprints probably made by Homo antecessor. The oldest human fossils, around 500,000 years old, are of Homo heidelbergensis at Boxgrove in Sussex. Until this time Britain had been permanently connected to the Continent by a chalk ridge between South East England and northern France called the Weald-Artois Anticline, but during the Anglian Glaciation around 425,000 years ago a megaflood broke through the ridge, and Britain became an island when sea levels rose during the following Hoxnian interglacial.
Below are notable events in archaeology that occurred in 1892.
The Solutrean industry is a relatively advanced flint tool-making style of the Upper Paleolithic of the Final Gravettian, from around 22,000 to 17,000 BP. Solutrean sites have been found in modern-day France, Spain and Portugal.
The Magdalenian cultures are later cultures of the Upper Paleolithic and Mesolithic in western Europe. They date from around 17,000 to 12,000 years ago. It is named after the type site of La Madeleine, a rock shelter located in the Vézère valley, commune of Tursac, in France's Dordogne department.
Federmesser group is an archaeological umbrella term including the late Upper Paleolithic to Mesolithic cultures of the Northern European Plain, dating to between 14,000 and 12,800 years ago. It is closely related to the Tjongerian culture, as both have been suggested. It includes the Tjongerian sites at Lochtenrek in the Frisian part of the Netherland, spanning the area of Belgium, the Netherlands, northern France, northern Germany, southern Denmark, and Poland. It is also closely related to the Creswellian culture to the west and the Azilian to the south. The name is derived from the characteristic small backed flint blades, in German termed Federmesser. It is succeeded by the Ahrensburg culture after 12,800 BP.
Gough's Cave is located in Cheddar Gorge on the Mendip Hills, in Cheddar, Somerset, England. The cave is 115 m (377 ft) deep and is 3.405 km (2.12 mi) long, and contains a variety of large chambers and rock formations. It contains the Cheddar Yeo, the largest underground river system in Britain.
The Boxgrove Palaeolithic site is an internationally important archaeological site north-east of Boxgrove in West Sussex with findings that date to the Lower Palaeolithic. The oldest human remains in Britain have been discovered on the site, fossils of Homo heidelbergensis dating to 500,000 years ago. Boxgrove is also one of the oldest sites in Europe with direct evidence of hunting and butchering by early humans. Only part of the site is protected through designation, one area being a 9.8-hectare (24-acre) geological Site of Special Scientific Interest, as well as a Geological Conservation Review site.
Aadloun, Adloun or Adlun is a coastal town in South Lebanon, 17 kilometres (11 mi) south of Sidon famous for its cultivation of watermelons. It is also the site of a Phoenician necropolis and prehistoric caves where four archaeological sites have been discovered and dated to the Stone Age. The evidence of human occupation of Abri Zumoffen has been dated as far back as 71,000 BCE with occupation of Bezez Cave dating back even further into the earlier Middle Paleolithic.
Qesem cave is a Lower Paleolithic archaeological site near the town of Kafr Qasim in Israel. Early humans were occupying the site by 400,000 until c. 200,000 years ago.
Hazar Merd is a group of Paleolithic cave sites excavated by Dorothy Garrod in 1928. The caves are located southwest of Sulaymaniyah, in the Kurdistan Region, Iraq. Garrod's soundings in two caves in the Hazar Merd group provided evidence of Middle and Epi-Paleolithic occupation. it is referred to as Ashkawty Tarik in Kurdish, which means Dark Cave, it also has a commanding view over the valley and it's close to a small spring and a village with the same name.
The Robin Hood Cave Horse is a fragment of a rib engraved with a horse's head, discovered in 1876, in the Robin Hood Cave in Creswell Crags, Derbyshire. It is the only piece of Upper Paleolithic portable art showing an animal to have been found in Britain. It is now in the British Museum, but normally not on display. In 2013, it was displayed in the exhibition at the British Museum Ice Age Art: Arrival of the Modern Mind. A replica of the artifact is displayed at the Creswell Crags Museum.
Kendrick's Cave on the Great Orme, Llandudno, Wales, was the site of important archaeological finds by Thomas Kendrick in 1880. The site is a small natural cavern on the south of the Great Orme Head, a limestone massif on the seaward side of Llandudno.
Cathole Cave, Cat Hole Cave or Cathole Rock Cave, is a cave near Parc Cwm long cairn at Parc le Breos, on the Gower Peninsula, Wales. It is a steep limestone outcrop, about 200 yards (180 m) north of the cromlech along the Parc le Breos Cwm valley and near the top of the gorge, about 50 feet (15 m) from the valley floor. The cave is a deep triangular fissure penetrating the hillside and narrowing towards the top. It has two entrances, with a natural platform outside the larger of the two. It is about seven 1⁄2 miles (12 km) west south–west of Swansea, Wales, in what is now known as Coed y Parc Cwm at Parc le Breos, on the Gower Peninsula.
The Pinhole Cave Man or Pin Hole Cave Man is the common name for an engraving of a human figure on a woolly rhinoceros rib bone dating to the Upper Paleolithic that is now in the British Museum. In 1926, a woolly rhinoceros rib that was broken at both ends was found in Pin Hole Cave, Creswell Crags, Derbyshire, England.
Paul Barry Pettitt, FSA is a British archaeologist and academic. He specialises in the Palaeolithic era, with particular focus on claims of art and burial practices of the Neanderthals and Pleistocene Homo sapiens, and methods of determining the age of artefacts from this time. Since 2013, he has been Professor of Archaeology at Durham University. He previously taught at Keble College, Oxford and the University of Sheffield.
The Brillenhöhle is a cave ruin, located 16 km (9.94 mi) west of Ulm on the Swabian Alb in south-western Germany, where archaeological excavations have documented human habitation since as early as 30,000 years ago. Excavated by Gustav Riek from 1955 to 1963, the cave's Upper Paleolithic layers contain a sequence of Aurignacian, Gravettian and Magdalenian artifacts. In 1956 the first human fossils were discovered within a fireplace in the center of the cave, a discovery which made important contributions to the foundational understanding of the Magdalenian culture of central Europe.
The small Sirgenstein Cave, German: Sirgensteinhöhle is situated 565 m (1,854 ft) above sea level inside the 20 m (66 ft) high Sirgenstein, a limestone rock. The cave sits 35 m (115 ft) above the Ach River valley bottom in the central Swabian Jura, southern Germany. Archaeologist R. R. Schmidt excavated the site in 1906 during which he identified indices of prehistoric human presence. He recorded the complete stratigraphic sequence of Palaeolithic and Neolithic origin. In his 1910 analysis Schmidt inspired future archaeologists with his pioneering concept of including the excavation site within its geographic region, contextualizing it within a wide scientific spectrum and demonstrated valuable results as he correlated the Sirgenstein layer structure to those of prehistoric sites in France. Mammoth ivory beads dating from 39,000 to 35,000 years ago have been uncovered at the cave. Because of its historical and cultural significance and its testimony to the development of Paleolithic art, the cave was inscribed on the UNESCO World Heritage List as part of the Caves and Ice Age Art in the Swabian Jura site in 2017.
Roger Michael Jacobi was a British archaeologist specialising in Palaeolithic and Mesolithic Britain. Known for his encyclopaedic knowledge of British prehistory, Jacobi authored several key synthetic volumes and worked to catalogue, sequence and reanalyse collections from across Britain and northwestern Europe. Sections of his extensive personal archive were posthumously published as the Palaeolithic and Mesolithic Artefact (PaMELA) database. He studied archaeology at Jesus College, Cambridge, and held positions at Lancaster University, the University of Nottingham, and the British Museum.
There are numerous radiocarbon determinations on human remains, butchered animal bones and organic artefacts which date the Creswellian to between 13,000-11.800 BP (Jacobi 2004).
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