Reinvestigation of the Sutton Hoo tars was undertaken within a wider research project examining the technology and preservation of ancient tars and pitches. The tar-like lumps were analysed by Fourier-transform infrared spectroscopy (FTIR), gas chromatography-mass spectrometry (GC-MS) and elemental analysis—isotope ratio mass spectrometry (EA-IRMS) and the surface morphology of the fragments was examined by optical microscopy and eflectance transformation imaging (RTI).
The FTIR spectra of the putative tars 1939.1010.250 and 1939.1010.251 lacked the strong carbonyl band typical of pine-tar or tree resin, instead displaying less functionalised spectra, characteristic of bitumen. Spectra obtained from the other tarry finds were markedly different... and they share some features with reference spectra of cellulose and to a lesser degree Cassel brown pigment. The latter, as a bituminous earth, may indicate that these tar-like materials also have a fossil organic component, but the possibility that the spectra arise from contamination with soil-derived organic from the burial environment cannot be ruled out.
To constrain its origin, the chemical composition of the Sutton Hoo bitumen was compared with a select group of British and Middle Eastern bitumens. Bitumen from Pitchford (Shropshire, UK) was selected because of its long history of exploitation: the location is recorded as “Piceforde” in the Domesday Book (c. 1086) and the still extant bituminous well may have been used even earlier, as Romans at nearby Wroxeter are thought to have exploited local seeps. Other localities considered, that did not yield sufficient biomarkers for correlation, include mines at Great Orme’s Head (Gwynedd, Wales) and South Crofty (Cornwall), where anciently exploited ore deposits co-occur with bitumen. Specimens from three other on-shore petroleum systems (Windy Knoll, Derbyshire; Thurso, Caithness; Mupe Bay, Dorset) with substantial inland and coastal outcrops of vein-bitumen and bituminous sandstone were also included. The Middle Eastern comparators are all known or reputed to be in active exploitation in the 1st millennium AD and earlier
A larger comparator sample base would be needed to confirm a connection with a Syrian-bitumen family as above the more general Dead Sea family of bitumen. The potential impact of more than a thousand years in the acidic burial environment of Sutton Hoo should also be considered before closer parallels can be drawn with more specific sources. Alternative sources within the Eurasian continent might also be considered; bitumen trade between the Black Sea and the Mediterranean is archaeologically attested in earlier periods and although the source of this material is not proven its location on the inland river routes linking to the Baltic and North Seas may be significant. What is clear is that the Sutton Hoo bitumen does not correlate to any of the British petroleum systems investigated in this study.
Other localities considered, that did not yield sufficient biomarkers for correlation, include ...
bitumen trade between the Black Sea and the Mediterranean is archaeologically attested in earlier periods
The possible Syrian origin of the bitumen is particularly interesting given that other items in the burial assemblage have been linked to this region. Nevertheless, the significance of the bitumen lumps among the grave goods is not clear as their morphology offers little evidence for their original form: possibly they represent surviving components of perishable objects, fragmentary small bitumen objects or, alternatively, the material may have been valued in its own right as a prestige raw material.
hvered wrote:The use of bitumen in the 12th century BC seems to be better documented than for the Sutton Hoo era.
The Kimmeridge oil shale was used for making armlets in Iron Age and Roman times and this industry was on a substantial scale. Objects of Kimmeridge oil shale have been found on the continent, as far away as Switzerland. ... The Kimmeridge oil shale was used extensively by Iron Age British tribesmen and the Romans for armlets. These were made on a primitive lathe. The residual central disks are known as Kimmeridge coal money. Large numbers have been found. With one of them is shown a beach pebble of oil shale that I polished with carborundum paper and metal polish. This gives an idea of the polished appearance. It is easy to polish and the material seems to have been much valued in antiquity.
http://www.southampton.ac.uk/~imw/Kimme ... tm#KOS-2-1
In the 17th century Sir William Clavell, owner of the land around Kimmeridge, used the Kimmeridge oil shale as fuel for glass-making, and for boiling sea-water to manufacture salt.
http://www.ukogplc.com/page.php?pID=72
John Clavell's descendant Sir William Clavell (1568–1644) earned his knighthood fighting in Ireland for Elizabeth I against the Earl of Tyrone. On his return to England he engaged in various projects to exploit the oil shale found in the cliffs near Kimmeridge. Initially he attempted the production of alum, but this infringed on a monopoly granted by James I, and his works were confiscated. He then set up works for the production of glass and salt, using the shale as fuel. The chief disadvantage of burning shale was the smell - one of Clavell's neighbours compared it to a "close stool". In order to be closer to — but upwind of — these works Sir William set about building a new house at Smedmore. However, along with the losses incurred from his alum works, this proved to be ruinously expensive and he ran up debts of some £20,000. He was therefore forced to sell much of the land he had inherited, including Barneston
Mick Harper wrote: But since earthquakes nowadays are mainly (wholly?) the result of fracking and not plates moving, (wherever both are a possibility) this causal connection is splitting apart at the seams. Not that geologists have noticed. Nor pretty much anyone else it would seem.
Poole Harbour is Britain's oldest working cross-channel port, according to new research. Archaeologists say ancient piles - wooden supports - found within a series of jetties at the harbour, date back to 250 BC. The work was carried out by experts from Bournemouth University and the Poole Bay Archaeological Research group. Two jetties have been found so far, one projecting south west from Green Island and the other north east from Cleavel Point.
Artefacts from the Iron Age settlement at Cleavel Point shows that traders sailed into Poole Harbour at the time to purchase pottery, shale jewellery and other things made locally in Dorset. Professor Tim Darvill, head of Bournemouth University's Archaeology and Historic Environment Group, said: "The scale of the facilities now revealed around Cleavel suggests that here is Britain's first really substantial cross-channel port.
http://news.bbc.co.uk/1/hi/england/2266789.stm
A series of 25cm diameter oak posts were rammed into the river bed, then infilled with hard Purbeck limestone to form a hard jetty.
There's nothing like it anywhere on the Atlantic Coast. To find anything comparable you'd really have to go to the Mediterranean world, the Greeks and the Romans. What surprises me is the amount of investment that's gone into constructing something like this.
Archaelogists believe that an iron age trading network extended all the way from Britain as far as India. The Ower peninsula has extensive evidence of iron age industry.
Why on Green Island? When we look at the trading islands in the Mediterranean occupied by the Greeks and the Phoenicians, and places like Cadiz, they're on islands.
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