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Technology and Terminology of Knapped Stone - IRIT

Technology and Terminology of Knapped Stone - IRIT

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1. Observation o f surface condition s<br />

Any reading <strong>of</strong> an object must begin with the careful examination <strong>of</strong> the surface<br />

condition(s), bearing in mind that:<br />

- by the word "cortex" we underst<strong>and</strong> a natural surface;<br />

- by the word "patina" we underst<strong>and</strong> an alteration <strong>of</strong> an intentionally worked (or used)<br />

surface;<br />

- by the word "neocortex" we underst<strong>and</strong> a surface <strong>of</strong> original cortex that has been<br />

altered by natural causes, such as fluvial transport. The presence <strong>of</strong> neocortex is therefore<br />

indicative <strong>of</strong> a secondary deposit <strong>of</strong> raw material.<br />

Once the specimens showing only cortical surfaces have been set aside, technological<br />

analysis entails examining the entire appearance <strong>of</strong> a tool as it has come down to us. The indelible<br />

marks <strong>of</strong> its history must be deciphered according to their chronology.<br />

Take the case <strong>of</strong> a core whose removal negatives have fresh arrises <strong>and</strong> ridges, others<br />

being blunted <strong>and</strong> striated as if by fluvial transport. Such a core carries several informations : it<br />

was first used as an "active" core, then rolled around, subsequently picked up (away from the<br />

point where it was found) <strong>and</strong> then flaked again before being discarded for good. There are even<br />

documented examples <strong>of</strong> tools having undergone three series <strong>of</strong> retouches, each showing a<br />

different patina.<br />

Further sorting out may be necessary, in order to set aside "pseudo-tools". Amongst<br />

others, these are most frequently pseudo-bifaces or "pebble-tools" fractured by frost or by a wide<br />

variation in temperature <strong>and</strong> humidity (the latter being common in desert settings); also, cobbles<br />

"knapped" by surf or glacial compression, <strong>and</strong> the (sometimes prehistoric) pieces crushed by<br />

cryoturbation or by mechanical devices ("denticulates", "scrapers", "raclettes", "borers", etc.).<br />

For any assemblage studied, it is therefore absolutely necessary to know the exact<br />

physical context <strong>of</strong> the site <strong>of</strong> origin :<br />

- surface site;<br />

- buried site;<br />

- thickness <strong>and</strong> lithology <strong>of</strong> the archaeological layer;<br />

- angle <strong>of</strong> dip;<br />

- origin <strong>of</strong> the sediments (volcanic, metamorphic, sedimentary - aeolian or fluvial,<br />

glacial);<br />

- cliff-base, talus slope, etc.<br />

It should be kept in mind that, even in a living zone, trampling is far from negligible; it<br />

can become quite intense around springs where large animals have come to drink.<br />

In all instances the accumulation <strong>of</strong> observations is essential.<br />

2. Types o f surface condition s<br />

The following examples are intended simply as an indicative list.<br />

2.1. Natural alteration s<br />

• Cortex is an integral part <strong>of</strong> the raw material in its natural condition, before being<br />

knapped. Its presence or absence on flakes provides information about the management <strong>and</strong><br />

origin <strong>of</strong> the raw material.<br />

• Patina, due to physical <strong>and</strong> chemical interactions, consists <strong>of</strong> a modification <strong>of</strong> the<br />

surface, which does not notably change its morphology. The degree <strong>of</strong> modification is eminently<br />

variable : it entails a change in colour - with or without modification <strong>of</strong> the granularity <strong>of</strong> the<br />

texture - either solely on the surface (film) or more deeply, sometimes throughout the body <strong>of</strong><br />

the piece, which can then become considerably lighter. The causes are so numerous <strong>and</strong> varied<br />

(even within a single layer), <strong>and</strong> their study so complex that no chronological classification based<br />

on patina has yet been successfully developed, even when only one site is involved.<br />

• Wind gloss is less glassy than that due to the swirling <strong>of</strong> s<strong>and</strong> in artesian springs. Both<br />

weathering phenomena can wear down an artefact to the point where its morphology is<br />

substantially modified, so that all traces <strong>of</strong> knapping may be obliterated.<br />

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