Pictures of Herkimer Diamonds and their Association with Other Minerals
The General Mineralization Sequence for
the Herkimer Diamond Mining District*
Youngest
Oldest
Click on any mineral name
to see photos and more
information
Rust - and related iron oxides
The
Main
Event
The depositional placement of the second dolomite
and third dolomites appear to be happening
throughout most of the Herkimer diamond making
history, illustrated using the blue arrows. More data
is needed because it is difficult to find overlapping
relationships with dolomite that let us determine its
time of growth relative to other minerals.
*The
mineral
depositional
sequence
is
determined
by
carefully
examining
many
specimens,
across
the
entire
district,
to
discover
what
minerals
deposit
on
top
of
one
another.
For
example,
calcite
is
found
to
grow
over
the
top
of
almost
everything
on
this
list.
Each
mineral
event
in
the
above
sequence
varies
in
intensity
across
a
deposit,
and
across
the
mining
district
and
thus
lends
a
unique
quality
to
each
individual
location
within
the
district.
This
is
the
main
reason why mines are different.
Rare occurrences of
strontianite, celestite
and chrysocola.
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The information, and photography, on this website is copyright protected
by W. David Hoisington, Ph. D. unless another author/photographer is cited.
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New discovery (2016) of microscopic,
unusually shaped, crystals at the
quartz-hydrocarbon boundary (see
Changes at the Boundary)
Last updated January 2018
Thank you Shannon Haley
Wilbur for the donation of 30
samples from the Fonda
region.1/05/2019 and 3/2/2019
Check out her Facebook.