Prehnite
or "Pectolprehnite": FL indescribable colors SW!!
Pectolite: FL Orange SW
Manganaxinite: FL Red SW
Calcite {CaCO3}: FL Red-Orange SW
Margarosanite:
FL
Blue-White SW
Willemite: FL Green SW
Prehnite and pectolite were part of
the so-called "Parker suite" of minerals,
along with margarosanite, manganaxinite, xonotlite, roeblingite,
nasonite, charlesite, datolite, and a few others. Prehnite and
pectolite from Franklin sometimes occur as an inseparable
mixture. The crystal grains of each mineral are so closely
intergrown that they look like one mineral. This is why some
collectors use the term "pecto-prehnite" or "pectolprehnite", even
though that's not a real species name.
Minerals like these can have a special quality... a person starts
feeling
the need to be close to them, to have them nearby all the time.
One doesn't feel quite right when the minerals are not around.
This is especially true of Parker suite minerals. Some
collectors become addicted to them. I fear this might be starting
to happen to me. I try to resist. Lately it isn't working.
They must be powerful, these rocks. It's not just the
fluorescence, either. Back in 1899 there were people mysteriously
drawn to roeblingite before they even knew it fluoresced! Think
about this. Was Baron Karl von Reichenbach correct about a
mysterious
energy from minerals? Few may believe his theories nowadays, but
I think he was really on to something.
Few things can do this to a person, where you look at them and
immediately you think to yourself, "I need
that." Imagine. It's a rock, but you need it! Who
could have prepared you for this? The
Parker Shaft minerals in particular can affect a person this way.
If the people who ran things were thinking straight, they'd dig up
those minerals. They'd re-open those flooded mines. Forget
gold. Gold is a waste of time-- it's just one element, it comes
in only one color, and it doesn't even fluoresce! Franklin
minerals on the other hand, now those are worth having!
Unfortunately there's the problem of all those troublesome buildings
now sitting on Franklin. What were people thinking, building on
top of the place? Especially the rock dumps. Destroying
the rock dumps was just wrong.
In the
grand scheme of things, a pile of Parker Shaft mine rock should rank in
importance leagues above parking lots, houses, and stores.
Countless tons of Parker
minerals also lie buried in flooded and collapsed mine stopes, because
at the time it was
too expensive to haul them up to the surface. The mining company
regarded them as worthless, since they weren't actually zinc ores.
Anyway, since you're still reading after my little digression... let's
get back to the rock itself. This was a very difficult specimen
to photograph. Even though the photo is a little overexposed
(making the fluorescence appear brighter), the specimen still looks
better in real life. With some prolonged tweaking of the hue,
saturation, lightness, etc., I was able to make the
photo a fair representation of the real-life fluorescent colors.
However, the true fluorescence of the pectolite-prehnite in the
specimen is still a bit more "peach"
colored than tan, but it's tough to capture with a camera. The
prehnite-pectolite mixture has a very subtle
fluorescence whose exact color is hard to describe. The human eye
can see it just fine in real life, but the camera fails to capture it
adequately. I'd call it a mixture of peach, tan, and pale
bluish. In some specimens the response is more bluish.
Franklin minerals can fluoresce colors that don't even exist... for example,
pink-blue.
The non-fluorescent minerals in the specimen (with daylight colors in
parentheses) include hancockite
(brick-red), andradite
(caramel-colored garnet), franklinite
(black, sub-metallic), hendricksite
(purplish-black mica), and possibly ganophyllite
(tan).
Some collectors call this complex mineral assemblage "Parker Shaft
soup" because there are so many species in it.
I bought this piece from another collector recently. I saw it,
and there it was: I needed
it.
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Site contents copyright 2005, C. Thorsten
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