Description
Genuine Neolithic Flint Working Flake from Grimes Graves
This carefully selected archaeological artefact is a genuine Neolithic white flint working flake recorded as originating from Grimes Graves in Norfolk, England, and attributed to approximately 2500 BC. It comes from an old collection and represents waste produced during the extraction, preparation or manufacture of flint tools within one of Britain’s most celebrated prehistoric flint-mining landscapes.
Rather than being a finished implement, this specimen is a working flake: a piece deliberately detached from a larger flint nodule, core, rough-out or developing tool during knapping. Such flakes are important archaeological evidence because they preserve the individual actions involved in prehistoric stone-working and help illustrate how raw flint was transformed into functional axes, cutting tools and other implements.
The photographs show the actual carefully chosen specimen you will receive. This is not a stock image or a representative example from a group. Please examine the photographs for its complete outline, fracture surfaces, geological colour, patination, flake scars and condition. Full sizing is shown in the photo.
Grimes Graves Neolithic Flint-Mining Landscape
Grimes Graves is an internationally important prehistoric flint-mining complex situated in the Breckland landscape of Norfolk. The site is renowned for its numerous mine shafts, quarry hollows and underground galleries created by Neolithic communities seeking high-quality flint embedded within the chalk.
The name “Grimes Graves” is much later than the prehistoric workings. The visible hollows across the landscape are the remains of filled-in mining shafts rather than graves. Beneath the surface, miners excavated through chalk deposits to reach particularly desirable seams of flint.
A working flake attributed to this location represents more than an isolated piece of stone. It is connected with an organised process of raw-material extraction, selection and tool production that required geological knowledge, physical labour and skilled craftsmanship.
The attribution to circa 2500 BC places the specimen within the later Neolithic, a period associated with established farming communities, extensive exchange networks, monument construction and sophisticated stone-tool industries.
White Flint Geology and Patination
Flint is a hard, compact siliceous rock composed predominantly of microscopic quartz crystals. It commonly occurs as nodules, lenses and irregular bands within chalk formed from ancient marine sediments.
The chalk deposits of Norfolk date to the Cretaceous period, when the region lay beneath a warm sea. Silica derived partly from marine organisms, including sponges and other siliceous life forms, was redistributed through the soft carbonate sediment and concentrated into dense flint nodules.
Flint may be naturally dark grey, black, brown or mottled when freshly fractured. The white or pale appearance of an archaeological specimen can result from its original mineral characteristics, chalky surface deposits or long-term patination.
Patination develops as the outer surface of flint undergoes chemical and physical alteration during burial or exposure. Pale grey, cream and white surfaces are frequently associated with prehistoric flint from chalk landscapes. The degree and distribution of this colour can vary across a single artefact, especially where different surfaces were exposed at different times.
Please refer to the listing photographs for the precise colour, texture, translucency and surface condition of this individual flake.
Neolithic Working Flake Artefact Type
A working flake is produced when force is directed into a prepared area of flint, causing a controlled fragment to detach. The resulting flake normally has two principal faces.
The ventral face is the inner fracture surface created at the moment of removal. It may preserve a striking platform, bulb of percussion, ripples or other features indicating the direction in which force travelled through the stone.
The dorsal face is the outer surface of the flake. It may carry cortex, previous flake scars or areas that once formed part of a core or developing implement.
Working flakes can be generated during several stages of production. Larger removals may establish the initial shape of a tool, while smaller flakes refine its outline, thin its body or prepare a cutting edge. This specimen therefore represents a surviving fragment of a wider technological process.
Conchoidal Fracture and Flint-Knapping Skill
Flint was highly valued during the Neolithic because it fractures predictably through conchoidal fracture. Unlike rocks that split along regular crystal planes, flint can produce curved fracture surfaces and extremely sharp edges when struck correctly.
A prehistoric knapper needed to assess the quality and shape of the raw nodule before selecting a suitable striking platform. The angle, location and strength of each blow influenced the direction, thickness and termination of the detached flake.
Hard-hammer percussion using a stone percussor could remove substantial flakes during early shaping. Finer work might involve softer hammers made from antler, bone or dense wood, allowing thinner and more controlled removals.
The surfaces preserved on this flake record one stage in that reduction sequence. Its ridges, scars and fracture features provide direct evidence of deliberate human action rather than natural breakage.
Flint Mining and Tool Production
The Neolithic miners at Grimes Graves excavated shafts through the chalk to reach selected seams of flint. Mining underground allowed access to material that had not been damaged by surface weathering, glacial movement or repeated natural impacts.
Tools made from antler, bone, wood and stone were used to break and remove chalk. Red-deer antler picks are particularly associated with prehistoric flint mining because their strong tines could loosen the surrounding deposits.
Once extracted, flint nodules could be tested and reduced close to the mining area. Unwanted cortex, flawed sections and excess material were removed, producing working flakes and other manufacturing debris.
Some flint may have left the site as prepared rough-outs rather than finished tools. Reducing the nodules near the source removed unnecessary weight and allowed unsuitable pieces to be identified before transportation.
Neolithic Flint Axes and Exchange
Grimes Graves is especially associated with the production of high-quality flint suitable for large tools, including Neolithic axe heads. Flint axes were used for woodworking, forest clearance and the preparation of structural timber.
Axe manufacture involved several stages. A selected nodule was first shaped through bifacial flaking, with material removed from both faces to establish the outline and cutting end. The surface might then be ground or polished, particularly around the blade, to strengthen and regularise the working edge.
Flint and completed tools could move beyond their original geological sources through exchange, travel and social relationships. High-quality raw material therefore had practical importance as well as potential social value.
Working flakes are essential to understanding these production systems. They reveal where tools were made, how the raw material was reduced and which manufacturing techniques were employed.
Archaeological Significance of Knapping Waste
Manufacturing waste can be as archaeologically informative as a complete polished axe. Every deliberately detached flake represents a decision made by a prehistoric craftsperson.
Groups of flakes can allow archaeologists to reconstruct the stages of tool production, identify specialised working areas and assess the skill of individual knappers. Refitting studies may even join separate flakes back together, partially reconstructing a core or tool-making sequence.
This specimen captures a single moment within that process. The knapper selected a platform, positioned the stone and applied force to remove material in a controlled direction.
Its survival provides a tangible connection with the people who mined and worked flint in Norfolk more than four thousand years ago.
Ex Old Collection Provenance
The artefact comes from an old collection and retains its recorded identification as a Neolithic white flint working flake from Grimes Graves, Norfolk, dating to approximately 2500 BC.
Old collection provenance forms part of an object’s modern history following its discovery. Earlier collecting associations can preserve valuable information concerning its locality, classification and archaeological interpretation.
The Grimes Graves attribution, Neolithic identification and old collection association will accompany the actual specimen shown in the photographs.
Actual Specimen and Condition
The photographs show the exact carefully selected flint working flake supplied with this listing. Please use the images to assess its full dimensions, thickness, profile, fracture features, white patination, geological texture and overall condition.
The specimen may display chalky deposits, mineral staining, weathered flake ridges, ancient edge losses or variations in surface colour. These characteristics contribute to its individual appearance and reflect its geological, archaeological and collection history.
Certificate of Authenticity
This is a genuine physical artefact and includes a generic Certificate of Authenticity card supported by a lifetime authenticity guarantee.
The certificate accompanies the actual specimen pictured, making this Grimes Graves Neolithic working flake suitable for a British archaeology collection, prehistoric mining display, lithic reference set, educational collection or museum-style cabinet.
Reviews
There are no reviews yet.