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. It 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 silicious 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.
A Preferred Material for Making Tools
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, spear points, arrowheads, scrapers, axes, drills and other sharp tools using a method
known as flintknapping. If these tools were broken or damaged in use they were often reshaped into smaller tools
of similar function.
|Prehistoric people became highly skilled at flintknapping, a method of shaping
flint into useful objects such as drills, arrowheads, knife blades and spearheads. National Park Service image.
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. 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. 
|The Vanport Flint has been quarried by people for at least 12,000 years. It outcrops in a layer between one
and twelve feet thick along Flint Ridge in eastern Ohio. Native Americans produced the flint from hundreds of quarries
along the ridge. Some of these people travelled hundreds of miles to collect the flint, used it to make a variety of
tools and weapons, and traded it widely throughout what is now the eastern United States.
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. Over 400 of these
shafts were sunk over an area of about 100 acres. 
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
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.
Close-up of a French flintlock rifle showing a flint ready to strike the steel frizzen, which will produce the spark needed to ignite the powder. Photo © Michael Westhoff, iStockphoto.|
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.
Flint is often cut into dome-shaped stones known as cabochons. These can be set into pins, belt buckles, pendants, bolos and other jewelry items.
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 portion of a wall of a medieval building in Suffolk, UK built with split flints. Photo © John Woodcock, iStockphoto.|
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" for this material.
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 another similar material. It has a sedimentary origin that is similar to 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.
Contributor: Hobart King
Find it on Geology.com
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|One of the most common uses of flint by prehistoric people was in the making of arrowheads. They were hard, tough and very sharp. Image by mcleandesign.com.
A lithic knife made from flint. Photo © Martin Vallière, iStockphoto.|
The Alibates Flint has been used by people of southwestern North America for about 13,000 years. The quarries used by these
people have been preserved as part of the Alibates Flint Quarry National Monument.  National Park Service image.|
Heavily quarried landscape at the Alibates Flint Quarry National Monument. Over 700 quarries can still be seen today. These
were all dug by hand without metal tools. National Park Service image.|
Shown in this satellite view are the remains of mining pits at the Grimes Graves flint mining complex, near Brandon,
England. Neolithic people constructed vertical shafts down through the Cretaceous chalk to a layer of flint about 40 feet
below the surface. Each shaft required the removal of about 2000 tonnes of chalk and required a team of workers several
months to construct. About 60 tons of flint could be removed from each of these pits and 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.  View Larger Map|
Flint is a variety of microcrystalline or cryptocrystalline quartz. It occurs as nodules and concretionary masses and less
frequently as a layered deposit. It breaks consistently with a conchoidal fracture and was one of the first materials used
to make tools by early people. They used it to make cutting tools. After thousands of years, people continue to use it. It
is presently used as the cutting edge in some of the finest surgical tools. This specimen is about four inches (ten centimeters)
across and is from Dover Cliffs, England.|
Chalk cliffs can be an excellent place to find flint. As the soft chalk weathers away, flint nodules fall to the beach below. Image of chalk cliffs along the
Baltic Sea, photo © hsvrs, iStockphoto.|
 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.
 The Neolithic Flint Mines of Sussex: Britain's Earliest Monuments, website article, Bournemouth University Archaeology Group, 2011.
 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.