Good
evening all; I am Pete Dohms, husband of Benigne who is
your regular correspondent at this e-mail address. I
am a professional geologist and this topic has landed
squarely in an area of which I have some degree of
knowledge.From direct observation and over 30 years of
professional experience, I can assure you all that
there is some degree of truth in what Bob has stated,
but there are limitations. Allow me to explain.
There are several types of "stone" that are
typically used for creating tombstones. In the early
days of America (particularly in New England), slate was
used. Slate is a dark colored rock that breaks
naturally along a very strong preferential plane
(cleavage). It is also fairly soft and fairly easy to
carve. It is also highly resistant to chemical
weathering (which is the erosional phenomena Bob was
alluding to). Slate tombstones that are hundreds of
years old can usually be easily read.
In the past 100 years, though, most American
tombstones have been created from two other types of
rock. Those are marble and "granite." In a moment I'll
explain why I put "granite" in quotation marks. First
to marble.
Marble is a crystallized form of what began as
limestone, a chemical precipitate formed as layers in
the bottom of a shallow sea. After deep burial, and
the application of heat and pressure, the limestone
grains (calcium carbonate) flowed together into the
larger and more crystallized forms seen in marble.
Marble is, like slate, relatively soft and quite easy
to carve. It is fairly easy to saw and grind, which is
good since it doesn't cleave like slate. If you've
ever been to a U.S. Military cemetery, virtually all
tombstones you see in the long precise rows are marble.
The effect is quite striking. Marble, unfortunately,
does not resist chemical weathering at all well. Many
tombstones from 100 years ago have become illegible,
hence the "tips" that pass around on "how to raise the
inscription." In the case of shaving cream, in the
absence of affirmative knowledge to the contrary, I
imagine the surfactants (wetting agents) in the shaving
cream penetrate the microscopic discontinuities along
crystal grain boundaries, making those areas easier for
rainwater (which in the NE USA is quite acidic) to
penetrate. Once penetrated, the acids go to work on the
crystal grains, enlarging the discontinuities and
exposing new marble (calcium carbonate) to chemical
attack. As the process continues, tiny flecks of marble
spall off the stone, leaving a white, sugary, irregular
surface behind. In cold climates, ice also penetrates
into the stone and the freeze-thaw cycle adds physical
weathering to the chemical attack (recall that water
expands upon freezing, which pushes the cracks open
even further).
What I called "granite" is, in reality, a trade
term for a wide variety of igneous and crystalline
metamorphic rocks that contain high concentrations of
silica (silicon dioxide, or quartz). The other major
components include various feldspars, dark minerals
(pyroxenes, hornblendes, micas), and other rock-forming
minerals. As a class, "granite" is difficult to work
into tombstones. It is both hard and tough. This
different mineral composition and more challenging
geologic history, however, provides it with an
excellent ability to resist chemical weathering. A
year ago, Benigne & I found the grave of her
grandmother's uncle, who was buried in Northeast
Pennsylvania in 1914. Rain in this area is as acidic
as any location in the country and more acidic than
most. The fine granite tombstone that was described in
his Will looked as though it had been erected the week
prior to our visit; it was untouched by the 85 years of
weather it had experienced.
Having said all that, please understand that the
forgoing are general statements. There will be specific
locations where 200 year old marble tombstones are in
remarkable states of preservation, and there will be
cases where 200 year old slate tombstones have
dissolved to low piles of shaley rubble, but those are
exceptions to the general conditions described above.
Pete Dohms, Geologist
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