The Archaeology of Britain: An introduction from ... - waughfamily.ca
The Archaeology of Britain: An introduction from ... - waughfamily.ca The Archaeology of Britain: An introduction from ... - waughfamily.ca
The Lateglacial colonization of Britain • 17 • Church Hole (Creswell Crags, Derbyshire). Products on unidentified antler include parts of three barbed harpoons from Kent’s Cavern, while leg bones of arctic hare (Lepus timidus) modified for use as pointed awls (poinçons) have been recovered at Gough’s Cave and Robin Hood Cave (Creswell Crags, Derbyshire). Other organic items include bone needles at Gough’s Cave, Church Hole and Kent’s Cavern, plus an awl—though not of hare bone—from the latter site. Several fox tooth beads have also been found at Gough’s Cave. Evidence for the method of antler working technology is restricted to a single fragment of antler from Gough’s Cave that shows groove and splinter modification. Grooves and cuts on the bones of Whooper swan (Cygnus cygnus) from Gough’s Cave show how needles were manufactured from bone cores. Radiocarbon dating Until recently, efforts to date the Creswellian have been greatly hampered by the limitations of the conventional methods of Figure 2.3 Distribution of Creswellian findspots: 1. Kent’s Cavern; 2. Three Holes Cave; 3. Sun Hole; 4. Gough’s Cave; 5. King Arthur’s Cave; 6. Robin Hood Cave; 7. Pin Hole; 8. Church Hole. Hachuring indicates potential source of flint raw materials. Source: After Jacobi in Barton et al. 1991 determining radiocarbon ages (Campbell 1977). However, since the 1980s, with the advent of AMS (Accelerator Mass Spectrometry) dating which can use extremely small sample sizes, the position has been considerably improved, and it is now possible to outline with greater confidence a basic chronological scheme for the Lateglacial settlement of Britain (Housley et al. 1997). The record is based on directly dated human bone, cut-marked bone and teeth, and bone, antler and ivory artefacts. AMS radiocarbon dates are presented (Table 2.2) for a selection of sites for which reliable associations with Creswellian artefacts exist. Nearly all of them fall between 12,500 and 12,000 BP, and are thus certainly part of the pre-woodland phase of the Interstadial. One of the sites deliberately omitted is Gough’s Cave, as this spans a greater number of radiocarbon years and includes artefactual material of clearly later type (see below). Equally problematic, for the moment, is the earliest date on modified bone from Gough’s Cave (12,800±150 BP), since it is so far the only date for a Creswellian site that could be significantly older than 12,500 BP. If the date is genuine, it might suggest a potentially earlier phase of occupation in south-west Britain than has hitherto been recognized. Taken as a whole, the AMS dates confirm that human presence
• 18 • Nicholas Barton Table 2.2 Radiocarbon accelerator dates from British Lateglacial findspots. in Britain probably lagged 500 radiocarbon years or more behind the main phase of Magdalenian settlement of the north-west European mainland. Raw material and mobility The 28 findspots with evidence of Creswellian activity consist mainly of collections from cave sites in the west and mid-central limestone areas of England and Wales, but there is increasing evidence for open-air activity both in these regions and in flatter areas further east (Figure 2.3). In cases where such evidence has been searched for, the preferred raw materials seem to have been good quality flints capable of producing long, straight blades, rather than local rocks of mixed or unpredictable quality.
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<strong>The</strong> Lateglacial colonization <strong>of</strong> <strong>Britain</strong><br />
• 17 •<br />
Church Hole (Creswell Crags,<br />
Derbyshire). Products on<br />
unidentified antler include parts <strong>of</strong><br />
three barbed harpoons <strong>from</strong> Kent’s<br />
Cavern, while leg bones <strong>of</strong> arctic<br />
hare (Lepus timidus) modified for use<br />
as pointed awls (poinçons) have been<br />
recovered at Gough’s Cave and<br />
Robin Hood Cave (Creswell Crags,<br />
Derbyshire). Other organic items<br />
include bone needles at Gough’s<br />
Cave, Church Hole and Kent’s<br />
Cavern, plus an awl—though not <strong>of</strong><br />
hare bone—<strong>from</strong> the latter site.<br />
Several fox tooth beads have also<br />
been found at Gough’s Cave.<br />
Evidence for the method <strong>of</strong><br />
antler working technology is<br />
restricted to a single fragment <strong>of</strong><br />
antler <strong>from</strong> Gough’s Cave that<br />
shows groove and splinter<br />
modifi<strong>ca</strong>tion. Grooves and cuts on<br />
the bones <strong>of</strong> Whooper swan (Cygnus<br />
cygnus) <strong>from</strong> Gough’s Cave show how<br />
needles were manufactured <strong>from</strong><br />
bone cores.<br />
Radio<strong>ca</strong>rbon dating<br />
Until recently, efforts to date the<br />
Creswellian have been greatly<br />
hampered by the limitations <strong>of</strong> the<br />
conventional methods <strong>of</strong><br />
Figure 2.3 Distribution <strong>of</strong> Creswellian findspots: 1. Kent’s Cavern; 2. Three<br />
Holes Cave; 3. Sun Hole; 4. Gough’s Cave; 5. King Arthur’s Cave; 6. Robin<br />
Hood Cave; 7. Pin Hole; 8. Church Hole. Hachuring indi<strong>ca</strong>tes potential<br />
source <strong>of</strong> flint raw materials.<br />
Source: After Jacobi in Barton et al. 1991<br />
determining radio<strong>ca</strong>rbon ages (Campbell 1977). However, since the 1980s, with the advent <strong>of</strong><br />
AMS (Accelerator Mass Spectrometry) dating which <strong>ca</strong>n use extremely small sample sizes, the<br />
position has been considerably improved, and it is now possible to outline with greater confidence<br />
a basic chronologi<strong>ca</strong>l scheme for the Lateglacial settlement <strong>of</strong> <strong>Britain</strong> (Housley et al. 1997). <strong>The</strong><br />
record is based on directly dated human bone, cut-marked bone and teeth, and bone, antler and<br />
ivory artefacts.<br />
AMS radio<strong>ca</strong>rbon dates are presented (Table 2.2) for a selection <strong>of</strong> sites for which reliable<br />
associations with Creswellian artefacts exist. Nearly all <strong>of</strong> them fall between 12,500 and 12,000<br />
BP, and are thus certainly part <strong>of</strong> the pre-woodland phase <strong>of</strong> the Interstadial. One <strong>of</strong> the sites<br />
deliberately omitted is Gough’s Cave, as this spans a greater number <strong>of</strong> radio<strong>ca</strong>rbon years and<br />
includes artefactual material <strong>of</strong> clearly later type (see below). Equally problematic, for the moment,<br />
is the earliest date on modified bone <strong>from</strong> Gough’s Cave (12,800±150 BP), since it is so far the<br />
only date for a Creswellian site that could be signifi<strong>ca</strong>ntly older than 12,500 BP. If the date is<br />
genuine, it might suggest a potentially earlier phase <strong>of</strong> occupation in south-west <strong>Britain</strong> than<br />
has hitherto been recognized. Taken as a whole, the AMS dates confirm that human presence