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GEOLOGY ARTICLE
What is a Herkimer diamond?
by MIKE BALDWIN
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12.18.01--Herkimer Diamonds are beautiful
double-terminated quartz crystals found in Herkimer, New
York. Incredibly, these phenomenal gemstones are close to
five hundred million years old. The crystals are
magnificent works of nature, found in the rock, having a
diamond-like geometrical shape. Thus, the name recognition
of "Herkimer Diamonds". Herkimers rival true
diamonds.
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A true diamond found in the rough is exactly that, a rough
appearing glass - like stone. The true diamond must be
painstakingly cut by man to give it smooth faces and a
geometrical shape. On a hardness scale, a true diamond scores
a ten. Herkimer Diamonds fall at a seven on the scale, giving
the real diamond a close race. They are naturally faceted,
each having eighteen faces and 2 points.
The bedrock in which the crystals are found began forming
approximately half a billion years ago in a shallow Cambrian
Sea that lapped against the southern shores of the ancestral
Adirondack Mountains (near the town of Herkimer, New York).
The limy sediments (calcium magnesium carbonate) which slowly
accumulated beneath the sea's salty waters were gradually
compacted under the weight of thousands of feet of additional
sediments, forming the rock strata Little Falls Dolostone.
While still beneath the sea, water seeped through the pores of
the rock often creating "vugs" by dissolving part of
the rock.
The collecting methods range from casually looking along the
prospecting area, digging through the rubble energetically,
using crowbars, sledgehammers and heavy chisels. The most
popular tools are a 2 or 3 lb. crack hammer and a bull point
chisel. The most popular method of prospecting for loose
Herkimer Diamonds is by breaking them out of a single rock.
Domed pocket mining in the table - layer of the rock is
usually very rich with diamonds. Some pockets are known to
contain thousands of diamonds. Pockets or cups can be up to
six feet in diameter and usually no less than one foot. The
dome-like tops of the pockets are often lined with small,
white cubic-shaped dolomite crystal. Occasionally, the top
will be beautiful black drusy quartz. Pockets containing
diamond crystals are never the same either in size or in
quality. Most pockets, as a rule, will contain diamond
crystals of various sizes. Some pockets may contain large
crystals ranging in size from four to eight inches long and
three to four inches wide. Other pockets with medium sized
crystals range in size from an inch and a half to three to
four inches long and a half inch to two inches wide. Micro
crystals are always found. As the crystals move up in size
they tend to become less clear or more translucent than
transparent.
Some crystals contain anthraxolite or decayed plant life. The
anthraxolite resembles bits of black coal within the crystals.
A special discovery would be an enhydro crystal. These special
specimen are crystals that contain a water bubble within it.
An extremely lucky find is an enhydro which contains species
of anthraxolite floating in the water bubble. Twins, doubles,
clusters, tabulars, smokies, skeletals and phantom crystals
are all valuable specimen found in pockets and are further
described in the Lapidary Section.
The most perfect crystals are usually those less than
1/2" long, but occasionally much larger crystals are
found. Crystals commonly occur intertwined or clustered and
often tiny, perfect crystals are attached to the backs of
larger ones. An avid business of trading has developed among
the multitudes of collectors, many of whom possess literally
thousands of specimens. The most perfect crystals are often
used as display pieces in unusually attractive necklaces,
earrings, and bracelets.
For more information visit
www.herkimerdiamond.com
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