One
mid-morning after a 12-hour night shift I was woken up by a phone call. The man
on the line was looking for a geologist, someone who knows about building
stones in Northeast Ohio. I asked him if it was the Berea Sandstone. He said he
thought that is what it was. He owned what he called a mine, but really meant a
quarry of the stone and was in some kind of dispute about its boundaries and
depth. He needed to know its thickness. Not being an expert in this area I
referred him to the Ohio Geological Survey in Columbus, knowing that they had some
old reports about the Berea Grit, as the sandstone is called in its building and
grindstone manifestation.
Since some of
my blog posts are related to personal experience, I thought I would research
and write a bit about the Berea Grit and its history and qualities as a
building stone. The sand is indeed thick in Northeast Ohio and Western
Pennsylvania. It outcrops in Northeast Ohio, near Cleveland, where it has been
extensively quarried and milled.
As an oil and
gas geologist from Ohio I am well aware of the Berea Sandstone, having mapped
it in Southern Ohio and studied oil and gas production from it. It was once thought
to be of the Early Mississippian period but now is assigned to Late Devonian. The
sand made several river channels through West Virginia and deltas in Western
West Virginia and Ohio. Many of these produce natural gas and oil. I even
mapped one section I interpreted as an ebb tide delta with a single well of
prolific gas production (by Berea standards). A little further in Ohio there is
an older sandstone just below it, known as the Second Berea, that makes up
offshore marine bars. An equivalent sandstone in Western Pennsylvania is known
as the Murrysville Sandstone. The Berea Sandstone is also present as a lower
permeability rock in Kentucky where it produces oil and there is an equivalent but
likely slightly younger sandstone in Michigan. The sediment source of the sand was
the highlands of Eastern Canada.
The qualities of
the sand lend themselves well to being a building and grinding stone. Berea Grit
has a high silica content, composed mainly of quartz grains with silica cement.
An old book/magazine from 1896 notes that quarrying of Berea Sandstone began in
1830. First, until around 1840 or 1845, only grindstones were produced. Then flagstones
and building stones were produced. By 1893 the dozen or so companies producing
the stone consolidated into the Cleveland Stone Company, which was the largest
sandstone producer in the United States at the time. As a building stone the
Berea faces several large courthouses and buildings in the U.S. and Canada.
The sandstone
is named after the town of Berea, along the Rocky River, twelve miles southwest
of Cleveland and six miles from Lake Erie. There is an annual Berea Grindstone
festival in the town.
“The requirements for a good, natural grinding stone
are that it be sharp sand, clean—free from clay or other impurities—and
strongly cemented together. However, when this ideal condition is reached, any
further cement is objection-able, since it reduces the grit. The coarser the
stone the faster the cutting. The Berea grit is composed of about 4 percent
super hard aluminum oxide (corundum) bonded with about 93 percent silicon
dioxide (quartz), the remainder being iron, magnesium, and calcium oxide. Near
perfect in grain, the sandstone was ideal, cutting evenly and efficiently.”
The Berea is
also quarried in South Central Ohio as the Waverly Stone but there it is of
lower quality, having a higher clay content. The high-quality Berea Grit in
northern Ohio was easy to cut and milling the stone into shapes resulted in
very little waste. It was used extensively as a grindstone and as a whetstone. In
1915, about 85% of the grindstones in the U.S. were made from Berea Grit.
Unfortunately,
there were some tragedies regarding the stone’s production. Towns with quarries
were jagged and uneven with rock strewn about. The workers, particularly in the
mills where the stone was turned to make grinding wheels, developed silicosis
as the fine silica dust entered and accumulated in their lungs. Many workers
died from it. Incidentally, the more recent increase in black lung disease from
coal mines (after falling somewhat when better safety measures came) is really
attributable to silicosis as mining machines tear through adjacent sandstones to
get to other coal seams. The average time a worker spent in Berea Grit quarries
and mills was just 5 years.
Precision
grinding machines made of alloy steel began to replace grinding stones at the turn
of the century. The steel machines used new synthetic materials for grinding: vitrified
emery, carborundum (silicon carbide), and alundum (artificial corundum) became
the abrasives of choice for grinding wheels. These materials replaced sandstone.
Cheaper concrete and cement replaced the sandstone for use in sidewalks, curbs,
and foundations.
The Berea
Sandstone is also used in the petroleum industry as a standard for testing
cores. “For the past 30 years, Berea Sandstone core samples have been widely
recognized by the petroleum industry as the best stone for testing the
efficiency of chemical surfactants.” A company called Cleveland Quarries supplies
Berea for this purpose as well as for Berea Patio company and other uses. The high
permeability of the sand lends it well for use as a testing standard. Cleveland
Quarries’ Berea Sandstone Cores markets the rock for this use and describes
three grades based on permeability and other features:
“Split Rock has visible laminations but
can be classified as homogeneous. These samples typically yield mD ratings
between 100-300.
Liver Rock has little top no visible
laminations and is homogenous. These samples typically have mD ratings above
500 and can be found with mD ratings up to 900 when measured with air.
Dundee samples are from the Massilon
Formation. While having consistent porosities and densities to our Berea
Sandstone™, our Ohio Sandstone samples are not considered homogeneous. Its
laminations do not run parallel to each other and is very porous, therefore
yielding the higher ratings of 900mD-2500mD.”
References:
Wikipedia: Berea Sandstone. Berea Sandstone - Wikipedia
Rowley, Ira P. (1893). "Sandstone Interests of Northern Ohio - IV". Stone; an Illustrated Magazine. D. H. Ranck Publishing Company. pp. 200–203. Stone; an Illustrated Magazine - Google Books
Ohio’s Sandstone: Once
the source of the World’s Finest Grinding Stones. Dana Martin Batory. Early
American Industries Association. Excerpted from The Chronicle Vol. 60 No. 1,
March 2007. Ohio’s
Sandstone: Once the Source of the World’s Finest Grinding Stones – EAIA
(eaiainfo.org)
Berea Sandstone Patio. Website. Berea Sandstone - Patio stone, sandstone, Cleveland, Ohio (sandstonepatio.com)
Berea Sandstone
Cores. Website. Berea Sandstone
Cores | Cleveland Quarries
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