Stone as a material

print Print
Please select which sections you would like to print:
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

External Websites

The Stone Age is divided into two contrasting periods: the Old Stone Age, a long era of stagnation; and the New Stone Age, a brief period of swift progress.

The Paleolithic Period, or Old Stone Age, endured until about 10,000 years ago and was characterized by tools of chipped stone, cutting tools with rough and pock-marked surfaces and generally serrated cutting edges. The later Paleolithic was also an era of wood, horn (antler), and bone. These three materials, all softer than rock but nevertheless intractable, could not be worked successfully without the aid of harder rock tools, such as serrated blades and gravers, or burins, small scrapers with either pointed or narrow, chisel-like ends. Bone was a particularly useful material, for its toughness made feasible barbed fishhooks, eyed needles, and small leatherworking awls.

The term Neolithic Period, or New Stone Age, defines the second period, at the beginning of which ground and usually polished rock tools, notably axes, came into widespread use after the adoption of a new technique of stoneworking. The beginning of the Neolithic, the retreat of the last glaciers, and the invention of food crops, involving agriculture and animal domestication, were more or less contemporary events. The period terminated with the discovery of metals.

The revolutionary art that created the definitive ground and polished tools of Neolithic man was essentially a finishing operation that slicked a chipped tool by rubbing it on or with an abrasive rock to remove the scars of the chipping process that had produced the rough tool. Not only was the edge keener than ever before, but the smooth sides of the edge also promoted deeper penetration and, hence, greater effectiveness, with the added advantage of easier tool extraction from a deep and wedging cut.

As a tool material, the term rock covers a wide variety of rocks, ranging from the dense and grainless flint and obsidian to coarse-grained granite and quartzite. Each kind of rock has certain unique properties that are further influenced by temperature and humidity. Stone of any kind is difficult to manipulate. It has been noted, for example, that the indigenous peoples of Australia reject as unsuitable a great many of the flints they have worked on, sometimes in the ratio of 300 rejects to one accepted tool. This high discard rate may help explain the thousands upon thousands of rock artifacts that have been found.

Flint, homogeneous and isotropic (having equal properties in all directions), is the rock of first choice for toolmaking. Reasonably well distributed over much of the world, it is an impure quartz, a form of silica, usually opaque and commonly of gray or smoky-brown colour. It is harder than most steels, having no cleavage planes, but displaying the conchoidal, or shell-like, fracture of a brittle material that leaves a sharp edge when flakes are detached. (Glass, which may be considered an artificial quartz, also exhibits the conchoidal fracture.) Obsidian, a volcanic glass of rather limited distribution, is usually black or very dark and, because of its conchoidal fracture, was used like flint. Most edged rock tools, however, were of flint. Flint was once an object of trade, and flint mines were in Neolithic time what iron mines became at a later age.

Types of stone tools

Three principal types of tools appeared in the long Paleolithic Period, with substantial variations occurring within each type. The types are distinguished principally by workmanship but also vary in size and appearance and are known as core, flake, and blade tools. The core tools are the largest; the earliest and most primitive were made by working on a fist-sized piece of rock (core) with a similar rock (hammerstone) and knocking off several large flakes on one side to produce a jagged but sharp crest. This was a general-purpose implement for the roughest work, such as hacking, pounding, or cutting. The angle of the cutting edge was rather large because of the sphericity of the stone. In time, thinner, sharper, and more versatile core tools were developed.

Although large flakes with sharp edges of small angle were a by-product of core tool manufacture and were well suited for slitting and scraping, they were not flake tools in the proper sense. True flake tools derived from an advanced technique practiced more than 2 million years later that sought the flake and discarded the core from which it had been detached; flake tools were made deliberately to serve a certain function and were not the casual spin-off of another operation. Finally, there were blade tools, longish slivers of rock with keen unserrated edges, directly useful as knives or as stock from which other pieces might be skillfully broken to serve numerous purposes. While flake and blade tools were developing, core tools were refined by overall chipping to create thinner and more efficient forms.

Techniques for making stone tools

Archaeologists have noted three different techniques for working rock to successive stages of refinement in the Paleolithic Period. The first and always basic method employed the hammerrock to fashion either a large and rude core tool such as the chopper, whose form persisted for perhaps 2 million years, or to rough out (block in) large tool blanks that would be brought to final form by removing small flakes. The hammerrock technique produced short and deep flake scars. A variation employed the anvil stone, a large stationary rock against which the workpiece was swung to batter off large flakes.

The second method was the soft-hammer, or baton, technique, based on a discovery of perhaps 500,000 years ago that hard rock (flint in particular) could be chipped by striking it with a softer material. The baton was a light “hammer,” an almost foot-long piece of bone, antler, or even wood, whose gentler blows detached only quite small flakes that left smooth, shallow scars. Such small flakes, when removed from the large scars left by the hammerstone, reduced the coarse and jagged edge to many small serrations, giving a straighter and more uniform cutting edge whose angle was also more acute than formerly and, hence, sharper.

Pressure flaking was the third technique. In this, a short pointed instrument of bone, antler, or wood was used to pry, not strike, off tiny flakes in order to leave the smallest scars. As the least violent and most advanced of the methods of working stone, it gave the craftsperson the ultimate in control for the removal of materials in the shaping of an implement.

To judge from the few remaining hand-tool-making societies, it is likely that every early human was adept at making new tools quickly and easily and on the spot, as fast as the old ones were blunted or broken. The earliest simple tools, made by taking convenient hand-sized stones and giving them sharp crests by a few well-placed blows, were evidently discarded after use, for their widespread dispersal suggests that they were made at the place of use and abandoned after serving their purpose. Tens of thousands of prehistoric rock tools survive, compared with only very few bits and pieces of the skeletal remains of the makers. Stone, of course, is imperishable, whereas bone is not, and one individual might have made several hundred tools.