Anthracite coal was discovered by Philip Ginder in 1791 on Sharp Mountain,
an area nine mile west of the Lehigh River and forty miles north of
Allentown. The Lehigh Coal Mine Company was formed in 1792, but eventually
business began to falter because of the cost of transportation for anthracite
coal to Philadelphia. The company could not compete with the bituminous
coal that was being shipped over from England. The company briefly increased
its sales under the control of Jacob Cist during the War of 1812 because
bituminous coal could no longer be shipped over from England. Unfortunately,
sales plummeted once again when the war was over (Hugh Moore Historical
Park and Museums).
Two men in Philadelphia, Josiah White and Erksine Hazard, had purchased
some of the anthracite coal from Cist and discovered that it was an
excellent industrial fuel. They decided to lease, and then eventually
purchase, the lands of the Lehigh Coal Mine Company. They began their
efforts in the present day Mauch Chunk and formed two separate companies:
the Lehigh Coal Company and the Lehigh Navigation Company. Shortly after,
they merged to become the Lehigh Coal & Navigation Company, know
as LC & N (Campion et al., 1997). Through the LC & N, a wagon
trail was built in 1818 from the Summit mines to Mauch Chunk. This wagon
trail transformed into a gravity railroad later in order to minimize
the time needed for coal to get down the hill. In 1829, the Lehigh Navigation
was completed as well (Hugh Moore Historical Park and Museums).
The easier transport of coal due to the gravity railroad and the completion
of the Upper Grand Section of the Lehigh Navigation made it possible
to open more coal mines. New companies began to open in the Lehigh region,
although they all transported their coal via the LC & N (Hugh Moore
Historical Park and Museums).
During the early years of the anthracite coal industry at Summit Hill,
deep mining was not necessary because the coal was located relatively
near the surface. It was dug out by workers with a simple pick and shovel.
The coal was not always located at the same location on different mountains.
When Cist had begun his coal mine operations, his mine was located at
Room Run. In 1830, White reopened the Room Run mines located near Nesquehoning
Creek. There were pros and cons to this location since coal at Room
Run was located closer to the river than the coal at Summit Hill. It
was, however, deeper in the surface of the earth (Campion et al., 1997).
This coal was retrieved by drilling tunnels until the coal was reached
(Hugh Moore Historical Park and Museums).
Ethnic diversity was extremely prominent in the industry. Some of these
new immigrants faced harsh treatment, partly because many of them could
not speak English. Ironically, much of this discrimination was lead
by the Irish, who too, had been previously discriminated against. However,
his was partly due to economic fears (Campion 1997).
Strong ties were formed by men and boys who worked in the mines since
they were expected to aid each other in the event of disaster. Mining
accidents were very common for anthracite coal workers. During mining,
coal gave off methane (also known as firedamp). This gas was explosive
and a constant threat to the well being of those in the mines. Fans
were utilized to circulate the air, but the methane remained a threat.
There are numerous explosions in the record books due to firedamp explosions.
The worst in history occurred in the Avondale coal fields near Wilkes-Barre
in 1869. One hundred and eight men and boys were killed when a match
was lit following a strike, igniting the circulating air and causing
a fatal explosion. The mine collapsed, trapping the unfortunate people
and taking their lives. This, however, is only one of the many tragic
accidents that occurred (Campion et al., 1997).
Working in the coalfields began as early as the age of nine. These "breaker
boys" had the job of picking slate out of the tons of coal. This
was hard work and would often would lead to bleeding fingers at days
end. When machinery started to become more popular, some of these young
boys were mangled to death in the blades of the machinery (Campion et
al., 1997).
Drinking alcohol also became a way of life for the miners due to the
danger and hard work. This was the case for those who worked on the
canal as well, although LC & N looked down upon this. The work on
the canal was not as dangerous as it was in the mines. It was important
to have a level head when coal mining because of the technical difficulty.
However, the drinking continued because it was just the way of life
(Campion et al., 1997).
The anthracite coal industry began to dramatically change during the
1850s and 1860s. This was directly related to the changing
transportation systems in the area. Railroads began to be a much faster
means of transportation. They were also operable in the winter months
when the canal froze over. In the 1870s and 1880s, the industry
was growing quickly but unfortunately, the market was growing at a much
slower rate. This created competition between coal companies as well
as the transportation companies (Hugh Moore Historical Park and Museums).
In the beginning of the twentieth century, the coal industry began to
decline. Alternative fuels such as oil and natural gas were becoming
more popular energy sources. There were also continuous problems between
the workers and the management resulting in numerous strikes that were
also extremely detrimental to the industry. The number of jobs was also
decreasing due to increased in technology and the implementation of
strip mining. The Great Depression also caused the coal industry to
decline further. By 1954, the LC&N stopped mining coal altogether
(Campion et al., 1997).
The anthracite coal industry has had a major impact on the quality of
the water in the Lehigh River. Over the past thirty years, the quality
of the water has drastically increased. Coal silt deposits in the Lehigh
River used to increase the acidity of the waters. Much of this silt
was swept away by hurricanes and floods. In addition, the average pH
of the river has changed from approximately 4.5 to 6.0 in the 1950s
to the present range of 6.9 to 9.2 (Miller, 2000).
Today, abandoned coal mines are a major cause of the decrease in water
quality in the Lehigh River. Abandoned mine drainage is the "single
largest source of water pollution in Pennsylvania" according to
the Wildlands Conservancy in Emmaus, PA. The tributaries that lead into
the Lehigh River, including Nesquehoning and Buck Mountain Creeks, are
affected by the acid mine drainage from eight coal mines. This decreases
the quality of water in the river. Drainage from the mines also causes
various changes to the water including lowering alkalinity levels, decreasing
the natural buffering capacity, and introducing high concentrations
of sediment, iron, sulfate, aluminum, zinc, and acidity (Urban, 1998).
Efforts are being made by the Wildlands Conservancy to decrease the
effects of this acid mine drainage. They have received a grant to construct
a 1.5 acre artificial wetland to remove acid mine drainage pollutants
from the Lausanne Tunnel discharge. Hopefully, this will be another
step towards increasing the water quality of the Lehigh River (Miller,
2000).