A hard, tough material, used by humans to make tools for millions of years
Article by: Hobart M. King, Ph.D., RPG
What is Flint?
Flint is a hard, tough chemical or biochemical sedimentary rock that breaks with a conchoidal fracture. It is a form of microcrystalline quartz that is typically called “chert” by geologists.
Flint often forms as nodules in sedimentary rocks such as chalk and marine limestones. The nodules can be dispersed randomly throughout the rock unit but are often concentrated in distinct layers. Some rock units form through the accumulation of siliceous skeletal material. These can recrystallize to form a layer of bedded flint.
Flint is highly resistant to weathering and is often found as pebbles or cobbles along streams and beaches. Early people who used flint to make tools often prospected these areas to find nicely shaped pieces of flint for making specific tools.
The Preferred Tool-Making Material
Flint has been used by humans to make stone tools for at least two million years.  The conchoidal fracture of flint causes it to break into sharp-edged pieces. Early people recognized this property of flint and learned how to fashion it into knife blades, projectile points, scrapers, axes, drills, and other sharp tools.
They developed a method of striking a piece of flint to produce a sharp edge known as flintknapping. Through trial, error and practice they became highly-skilled craftsmen who could manufacture tools with a few quick blows. If the tools were broken or damaged in use, they were often reshaped into smaller tools of similar function.
The value of flint for making sharp tools was discovered and utilized by Stone Age people in almost every early culture located where flint could easily be found. Where flint was not locally available, people often travelled or traded to obtain premade tools or pieces of flint for manufacturing. Their survival depended upon having a durable material that could be used to produce sharp tools.
Flint Ridge Quarries, Ohio
One of the most important localities for flint in eastern North America is Flint Ridge in eastern Ohio. Native Americans discovered this deposit and produced flint from hundreds of small quarries along the ridge.  This “Ohio Flint” occurred in distinctive colors and was treasured by Native Americans.
They travelled hundreds of miles to collect it and spread the distinctive material in trade across eastern North America. It has been found as artifacts as far south as the Gulf of Mexico and as far west as the Rocky Mountains. 
Alibates Flint Quarries
In the area that is now the Texas panhandle, Native Americans discovered an area where weathered flint littered the ground. This flint was weathering out of a dolomite beneath the thin soil cover. These people discovered that fresh, unweathered flint of high quality could be obtained by digging down a few feet.
From about 13,000 years ago into the 1800's, this area was continuously mined for the high-quality flint. The flint was used to produce projectile points, scrapers, knives, and other stone tools. In the 1800's the flint was also mined for use as gunflints. Over 700 small quarries are still visible today and have been preserved as part of the Alibates Flint National Monument.
Neolithic Flint Miners
Perhaps the most impressive story about flint is that of the ancient mining complexes that were built in what is now England during Neolithic times. These excavations began about 4000 BC and continued until the widespread use of metals about 2,000 years later. 
One flint mining complex of particular note was Grime's Graves located near Brandon, England. Here ancient miners dug shafts down through 40 feet of Cretaceous chalk to a layer of high-quality flint below. Each shaft was several feet in diameter and required the removal of about 2,000 tonnes of chalk. Most of the digging was done without metal tools, using red deer antlers as picks. Each shaft required a team of workers and took several months to construct. 
About 60 tons of flint could be removed from each of these pits and the short horizontal excavations that followed the high-quality flint layer at the base. Starting about 3000 BC until about 1900 BC, these miners built over 400 shafts over an area of about 100 acres and removed thousands of tons of flint. 
Although these mining operations were amazing feats of engineering, just as impressive was the geological understanding of the workers. They knew that the flint was below the ground even though it did not outcrop anywhere in the immediate area. They also knew that the highest quality flint layer was below lower quality zones that were encountered during the early digging.
Flint as a Source of Fire
Another important property of flint is its ability to generate sparks of hot material when it is struck against steel. This property allows flint to be used as a fire-starter. Skilled people can use a piece of flint, a piece of steel, and a little tinder to quickly start a fire.
Early firearms, such as a flintlock, had a piece of flint attached to a spring-loaded hammer that was released when the trigger was pulled. The hammer struck a piece of steel known as a "frizzen" to create a shower of sparks that ignited a small pan of powder. That touched off the primary charge which exploded to propel the ball down the barrel.
Flint as a Gemstone
Flint is a very durable material that accepts a bright polish and often occurs in attractive colors. It is occasionally cut into cabochons, beads, and baroque shapes for use as a gemstone. It is also used to produce tumbled stones in a rock tumbler.
Most people have heard of a gem material called "jasper". Jasper is an opaque variety of cryptocrystalline quartz. It obtains its color and opacity from a large amount of included mineral particles. Flint and jasper are similar materials and both are varieties of a gem material known as "chalcedony".
Flint as a Construction Material
Where flint is abundant it is sometimes used as a construction material. It is very durable and resists weathering better than almost any other natural stone. It is common to see walls, homes, and larger buildings that are built partially or entirely with flint as a facing stone in southern England and many parts of Europe.
A Confusion of Names
Flint is a microcrystalline variety of quartz. Materials of this description have been given a wide variety of names, including chert, jasper, agate, and chalcedony. Most geologists use the word "chert" instead of "flint".
Some people believe that the name "flint" should be reserved for dark-colored chert that formed as nodules in limestone or chalk. Some archaeologists believe that the name "flint" should only be used when the material has been fashioned into an artifact.
The name "flint" has been so closely associated with starting fires that man-made materials used to produce sparks in cigarette lighters and survival kits have been given the name "flints."
"Novaculite" is a metamorphic rock that is similar to flint. It has a sedimentary origin, just like flint, but diagenesis and metamorphism have increased the size of the quartz microcrystals. It has been used for thousands of years for making sharp tools and weapons. Some specimens have a texture that make them useful as a sharpening stone.
 The World’s Oldest Stone Artefacts from Gona, Ethiopia: Their Implications for Understanding Stone Technology and Patterns of Human Evolution Between 2.6 and 1.5 Million Years Ago, Sileshi Semaw, Journal of Archaeological Science, Volume 27, pages 1197-1214, February 2000.|
 Flint: Ohio’s Official Gemstone: Garry L. Getz, Educational Leaflet Number 6, Ohio Geological Survey, 2012.
 Ohio’s State Gemstone - Flint: Website article, Ohio History Central: An Online Encyclopedia of Ohio History, Ohio Historical Society, 1999.
 Emmer Green (Hanover) South Chalk Mine Site Records, Subterranea Britannica, 2003. (This reference is provided for the excellent photographs of the underground workings showing the main flint seam.)
 Grime's Graves Flint Mining Complex: Article from Wikipedia, the free encyclopedia, April 2012.
 The Neolithic Flint Mines of Sussex: Britain's Earliest Monuments, website article, Bournemouth University Archaeology Group, 2011.
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