Iron is a silvery white, solid metal, though
when found in local ore it commonly appears brown, sometimes
nearly black. It's chemical symbol, Fe, is derived from ferrum,
the Latin word for iron. By volume, iron makes up 34.6% of
the earth, more than any other element.
What Is Salisbury Ore?
Just because we call our local iron Salisbury
ore, it doesn't mean it's only found in Salisbury! Salisbury
ore is the name given to deposits of iron found in a relatively
narrow belt extending south from Vermont along the Massachusetts/Connecticut/New
York borders. In Connecticut, we find Salisbury ore in Canaan,
Kent, Sharon, Cornwall, Salisbury, Norfolk and North Canaan.
Collier's Hut
Why and Where Do We Find
It?
In order to understand why we find abundant
iron in the Northwest Corner towns, we need to go back to
the origins of the earth - the study of Geology, which provides
the true beginning to the iron story. We find rich deposits
of iron in the Northwest corner because of the patterns of
rock formation and movement from as long ago as 570,000,000
years! The development of the Salisbury ore deposits began
in the mid-Ordovician Period when most of the region was under
water. Over time large quantities of sediments, some rich
in iron, settled in the silts and muds of the youngest bedrock
formations. Because of long-time exposure to water and the
shifting movements of the earth, iron ores were formed. Even
though the various ice ages that moved across northern Connecticut
rounded off our jagged mountain topography, and cut furrows
and valleys into the land, most Salisbury ore is still found
underground.
How Does Ore Become Pure Iron?
Since iron ore comes out of the mine mixed up with other
kinds of rocks and sediments, it must be processed to become
useful. Early in the industry's development, iron was processed
or smelted, in forges by heating the ore in a charcoal fire,
then hammering it to drive out the impurities. Bloomery forges,
named in Germany because the final product looked like a flower
or "bloom", reduced the ore directly to solid iron and liquid
slag (slag is a waste combination of iron, charcoal and sediments.)
Bloomery forges were made of stone and stood about 8 feet
high, with an opening for forced air blown from bellows powered
by a water wheel, and a chimney to allow gases to escape.
While Bloomery forges do a good job of making pure iron,
they can't make a lot of iron. In 1762, the first Blast Furnace
in Connecticut opened in Lakeville. The construction of a
blast furnace forthe manufacture of pig iron is more difficult
than the operation of a forge. A blast furnace consists of
a stack made of large stones. The stones must be built up
on a deep foundation to hold their heavy weight. A minimum
of two ground-level openings in the stack were needed; one
large opening to let the melted iron and slag (waste product)
out of the furnace, and another to let the air in so a hot
fire could be maintained. The openings to the furnace stack
were usually shaped like arches for strength. A stone hearth
was built on the bottom of the stack, leaving an opening for
a nozzle to carry in air from the blast pipe. This nozzle
was called a tuyere. The inside of the hearth had to be lined
with special heat-resistant brick called refractory fire brick.
The interior of the stack was lined with sand and rubble to
help the furnace stay hot. Once the stone work was finished,
a bridge had to be built from the top of the charging wall
to the top of the furnace stack. The charging wall was built
next to the furnace stack, as high as the top of the stack.
By building a bridge from the top of the charging wall to
the top of the furnace, workers were able to dump the ore
- or charge - directly into the top of the furnace stack.
After the charging wall was built, most of the furnace was
enclosed in wood buildings to keep the furnace safe from rain.
A building called a casting shed, with a sand floor, was built
out from the area next to the opening where the liquid iron
poured out, called the casting arch. A water wheel was used
to pump the large bellows needed to force air into the fire
was nearby. When the construction of the furnace was complete,
it was ready to be fired. A charcoal fire was built in the
hearth. The blowing mechanism was started, and workers began
dumpng charcoal from the top house (built over the top of
the furnace stack) through the tunnel head and into the furnace.
Gradually small amounts of iron ore and lime were added. Once
the furnace was heated, it was in full blast. At regular intervals,
the charge, consisting of iron ore, charcoal and limestone,
was dumped into the stack top. Temperatures were raised to
melt the metal. The charcoal served as fuel for the fire and
helped to purify the ore. The lime attached itself to ash
and other residues to form slag which floated on top of the
iron and could be easily seperated from it.
Pig Iron
Blast furnaces made Pig Iron. When the hot liquid metal was
tapped or poured from the furnace, it flowed into an indentation
in the sand bed called a sow and then into a series of smaller,
perpendicular indentations in the sand called pigs. When the
pigs had cooled enough to hold their shape, they were broken
from the sow and stacked. After that they were loaded into
wagons, weighed and taken to the foundry where they could
be used for casting or refined into wrought iron. Wrought
iron is a kind of iron made in a forge, either directly from
iron ore or from pig iron. Wrought iron is pulled or stretched
or hammered to make it into useful objects like nails, pokers
or hooks.
The Discovery of Salisbury Ore
In 1728, surveyors were sent to the western lands from Hartford.
Their main jobs were to determine borders and establish townships.
During that first survey trip, traces of iron were found in
fresh diggings around woodchuck holes. In 1731, John Pell
and Ezekiel Ashley began exploring the western section of
Salisbury. They were rewarded with the discovery at Old Hill
(later known as Ore Hill) that would prove to be the largest
and richest of the deposits of iron later to become known
world-wide as Salisbury iron. In 1732, a wily businessman
named Thomas Lamb came to the area from Springfield, Massachusetts.
Lured by the discovery of iron, Lamb purchased over 5,000
acres of land and water privileges on the Salmon Fell Kill
in Lime Rock. Lamb’s workers mined ore from what was originally
called “Lamb’s Three Acre Grant.” Later the mine became Hendrick’s
Ore Bed, then the Davis Ore Bed or Davis Mine. Ore from the
mine was moved 4.4 miles to Lime Rock in bags carried on horseback.
In 1735, Thomas Lamb began smelting iron at his bloomery forge
in Lime Rock’s Furnace Hollow. Although Lamb didn’t stay long
in the area, it was his success that laid the foundation for
others to follow.
Local Iron Industry
In 1740 Joseph Skinner began producing
iron at a newly completed forge located near a dam standing
just south of Mudge Pond (later the site of Benedict's Mill).
Three years later he sold the forge, tools, and stock or ore
to Jonathan and Samuel Dunham of Sharon, Thomas North of Wethersfield,
and Jonathan Fairbanks of Middletown. Jonathan Pratt was also
an early partner. Two decades later the Hutchinson brothers
constructed a forge on the east slope of Sharon Mountain,
near present Smith Hill Road. Samuel Hutchinson was from Lebanon
and served as a magistrate in Sharon. John Gray from Scotland,
Connecticut, operated yet another forge off Tanner Road. Ore
was mined on Silver Mountain and Buck Mountain in Ellsworth
and Skiff Mountain on the Sharon/Kent border.
From these humble beginnings the area
prospered as one of America's most important early mining
and refining centers. Blessed with the critical resources
of waterpower, iron ore, limestone for flux, and lumber to
provide the necessary charcoal, the industry flourished. Sharon's
iron industry, already many decades old, received a great
boost in 1822 when Leman Bradley of Falls Village obtained
land and waterpower rights in Sharon valley along Webatuck
Creek for the purpose of constructing a blast furnace, the
first in town. Beginning with an initial purchase of $7,000,
he later acquired additional land containing ore (just east
of Indian Mountain), timber, and lime. By 1825 Bradley's workers
had built a large dam, creating a ten-acre pond, along with
a 1,500-foot race with overshot wheel and pumping station
to power the blast. The furnace was built of Stockbridge marble
and fueled with charcoal.
Bradley operated the site for only a few
years, however, and by the late 1820s began selling off his
holdings. The furnace later passed to Salisbury's Horace Landon
who maintained production until 1872. In 1863, the furnace
was enlarged and converted to hot blast, a more efficient
process. In the early 1870s, the Sharon Valley Iron Company
(owned by the Barnum and Richardson Company) acquired the
furnace. Hiram Weed opened a second furnace in Sharon in 1845,
located .4 miles from the west terminus of Caulkinstown Road.
It was not long in blast after 1856.
Ultimately, the iron industry faced severe
and finally insurmountable obstacles. The close of the Civil
War brought an end to government orders, however the Sharon
Valley Iron Company continued to produce iron for railroad
car wheels. Iron for wheels alone was not enough and furnaces
began to close, including the ironworks in Sharon Valley in
1898. Introduction of the Bessemer process, expansion of the
Midwestern iron and steel industry, and the high cost of ore
and fuel all made Connecticut iron increasingly uncompetitive
in national markets. The Barnum and Richardson Company/Salisbury
Iron Company, which consolidated almost complete control over
the region's furnaces and mines during this period, struggled
against the odds finally declaring bankruptcy in 1925.
Why Did the Northwest Corner Become
the Perfect Location for a Thriving Iron Industry?
The Northwest Corner became a center of iron making because
it had the perfect combination of raw materials, people-power
and energy sources. First, there was an immense amount of
high-quality iron ore. Second, there was a readily available
power source from the many little rivers which are found throughout
the area. A good, reliable source of power was necessary to
power the forges, helve hammers, foundries, grist mills and
saw mills. A stream needed enough water flowing through it
to survive the driest seasons, and the water needed to be
moving with enough speed. Rivers such as the Salmon Kill,
Wachocasttinook Brook, Blackberry River and Macedonia Brook
were perfect resources. Lastly, there needed to be a good
source of charcoal which could be made by slow burning of
native trees; lime and marble; hearthstone, refractory brick
and molding sand. All of these materials were available nearby.
View a clip from SHS's Awarding Documentary-
Vision's of Iron: The Story of the Salisbury Iron District
The American Association for State and Local History (AASLH)
selected, Visions of Iron, as the 2009 Award of Merit winner
by the Leadership in History awards committee. The AASLH Leadership
in History Awards is the nation’s most prestigious competition
for recognition of achievement in state and local history.
Visions of Iron: The Story of the Salisbury
Iron District
Narrated by Ed Kirby
Produced by The Sharon Historical Society
Directed by JEM Films
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Sharon Historical Society, 18 Main Street,
Sharon, Connecticut
860-364-5688 | sharonhistoricalsociety@yahoo.com
Museum Hours 10AM - 4PM