Review of evidence for thermal fracture as the primary cause...
"...all the objects on your web site appear to be purely natural. They mainly appear to have been produced through frost shattering... ...Such objects can only be produced through freezing and thawing over a long period time and by pure chance superficially resemble the images you suggest."
Dr. Nicholas Ashton, September 2006
Clearly, from even a cursory examination of the assemblage (a sample of which is pictured on this web site) we can ascertain that the majority of the fracture planes do _not_ exhibit the features which are characteristic of frost shattering, including either irregular (angular) planes or differentiated patination. In fact, patination of comparable materials differs little throughout the assemblage indicating that the majority of fractures took place within a relatively short window of opportunity that is not consistent with a drawn out geological process such as freezing and thawing over a long period of time.
Fractures typically show traits compatible with mechanical percussion such as a bulb of percussion, point of detatchment, a relatively smooth plane, possibly with percussion "ripples", errailure scar and in the case of bipolar reduction, fractures emanating from the distal end. Platforms (the plane receiving the impact blow) when present are both "simple" and "complex" (Andrefsky).
Is it possible that the assemblage is glacial till, most likely from the Anglian glaciation?
The excavation site sits on the Colne valley, formerly the course of the proto-Thames before the Anglian glaciation diverted the path toward the present course around 475,000 years ago. The arrival of the glaciation caused a lake to form north east from the site around the Vale of St. Albans causing the Thames to eventually divert through Staines. The southern most extent of the glaciation is said to have ended at Bricket Wood. Figure 1 shown below derives from publically available information held by the British Geological Survey (BGS) in addition to represented Ordance Survey topographical data. The map shows the bedrock and superficial deposits - the white area is mapped by the BGS as glacial till (TILL-DMTN). The deposits from whence the assemblage presented derives (location marked A1 in Figure 1 and 2) are mapped as a sand and gravel layer (GSG-SAGR). The sand and gravel layer from whence the artefacts derive does not have a chalky appearance which is a characteristic of the Anglian glacial deposits (Catt, 2009).
There is a steep incline a little further from the excavation site (SE) from approximately 90 to 80 metres signifying a geological phase which created a distinct terrace. Indeed, an adjoining road is called "The Brow" and also nearby "Valley Rise". In Figure 2, the proto-Thames is depicted at a hypothetical level assuming that this event had passed and the flow receeded. It should be noted that the excavation site (A1), is located on the "warm" side of the valley (protected from Northerly winds), and considerably further up the valley than the maximum extent (70 metres) of the glacial till as mapped by the BGS. The hypothetical mapping of the Thames would place the site in a potentially strategically advantageous position.
 
Figure 1 (left), topographical and geographical map. Figure 2 (right) hypothesised extent of proto-Thames.
Age of deposits
The superficial deposits mapped as GSG-SAGR above may range in age. Until secure dating can be realised at the excavation site (e.g. OSL) we are reliant on visual inspections of the layer. There is the possibility that the sand and gravel layer was "plateau drift", where the clay has dissolved through solution. However, this would indicate an even older age for the layer which is not really consistent with what is known in the area.
The Gerrards Cross gravels, which this layer appears to be contemporaneous with, are dated to between MIS 22 and 23, or approximately 860,000 to 900,000 years old (Bridgland 1994). Ages in excess of that known for human occupation in the UK range from 0.86 Mya and 1.7 Mya across Europe (Azarello et al, Carbonell et al, Cauche, Toro-Moyano). Typically these occupation sites reveal lithic industries which are firmly classed as Mode 1 and are usually mostly unifacial.
Review of evidence for a glacial origin for the assemblage
The available data does not support the excavation site being in the vicinity of glacial till from the Anglian glaciation. However, this does not rule out an earlier glacial event being the cause of the fracturing.
During a private meeting where a small selection of the assemblage was briefly viewed by both Dr. Nicholas Ashton and Dr. Roger Jacobi it was proposed that the assemblage was largely glacial till. An earlier proposal by both was that the patination of flake scars was "too old" to be associated with human agency. Without being able to define how a patination could be interpreted to be "too old" this remark lacks any meaningful reference; an "authenticated" lithic was presented during the same meeting - also sourced from the Colne (about 8 Km away from A1 approximately in the left hand corner of Figures 1 and 2) by Jacobi himself, which had directly comparable patination. Further more, there are plentiful examples of recognised lithics with many shared qualities in the media. Indeed the two hypotheses are contradictory, the Anglian glaciation occurred many thousands of years after established human occupation at the Pakefield site (Parfitt et al).
Other archaeologists have claimed that the assemblage is resultant from a "dynamic fluvial environment" without being anymore specific. For the sake of argument, the Anglian glacial episode is considered here as one likely dynamic environment capable of creating sufficient forces and opportunity required to fracture large nodules (or cobbles) and large pebbles (this aspect is explored further in the next section). In this event, there are several characteristics of the assemblage that need to be accounted for when considering the plausability of this hypothesis, including the existence of delicate blades and even large nodules which have been split laterally but not fractured across the most "prone" areas. Indeed, the characteristics of the material presented typically show a range of features such as sequential or unifacial removal of flakes which are not at all compatible with a dynamic environment causing random, unselective fracturing and rolling during the transport which is inevitable with this type of event. Before considering further whether a glacial origin could satisfactorily account for the origin and features of the assemblage these matters need to be addressed.
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