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Flintknapping a stone tool Knapping is the shaping of flint , chert , obsidian , or other conchoidal fracturing stone through the process of lithic reduction to manufacture stone tools , strikers for flintlock firearms, or to produce flat-faced stones for building or facing walls, and flushwork decoration.
The Levallois technique of flint-knapping. In archaeology, in particular of the Stone Age, lithic reduction is the process of fashioning stones or rocks from their natural state into tools or weapons by removing some parts.
Israel Museum The Levallois technique of flint-knapping The Levallois technique ( IPA: [lÉ™.va.lwa] ) is a name given by archaeologists to a distinctive type of stone knapping developed around 250,000 to 400,000 [ 1 ] years ago during the Middle Palaeolithic period.
Stone tools have been used throughout human history but are most closely associated with prehistoric cultures and in particular those of the Stone Age.Stone tools may be made of either ground stone or knapped stone, the latter fashioned by a craftsman called a flintknapper.
A flint flake tool from the Neolithic, found in Hertfordshire, England. In archaeology, a flake tool is a type of stone tool that was used during the Stone Age that was created by striking a flake from a prepared stone core.
The prepared-core technique is a means of producing stone tools by first preparing common stone cores into shapes that lend themselves to knapping off flakes that closely resemble the desired tool and require only minor touch-ups to be usable.
In archaeology, a tranchet flake is a characteristic type of flake removed by a flintknapper during lithic reduction.Known as one of the major categories in core-trimming flakes, the making of a tranchet flake involves removing a flake parallel to the final intended cutting edge of the tool which creates a single straight edge as wide as the tool itself.
Archaeologists use this process of flintknapping to analyze blades and observe their technological uses for historical purposes. Blades are defined as being flakes that are at least twice as long as they are wide and that have parallel or subparallel sides and at least two ridges on the dorsal (outer) side.