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GOLD
"Gold,
Gold, Fool am I." Those words
from "Paint Your Wagon" sum up how
many feel about the yellow metal,
and identifying it can be trickier
than you think, especially if you
are out in the field panning or
prospecting. Not knowing how to
identify gold is where
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the "fool" part can
come in. All that glitters
is not gold, in fact most
gold does not
"glitter" at all.
Gold is a bright metal that
is bright but not shiny, nor does it
reflect light like a mirror,
as fool's gold can. It has
a warm glow that is
unmistakable, and will stay
glowing even when direct light is
removed from it. (No, silly,
it can't glow in a pitch
black darkened room. Just
shadow it with your hand.
Now do that with iron
pyrite) |
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If you wear a ring that is
made of gold, you have a very good
example of how gold glows. Even
when buffed to its highest shine,
gold does not shine like a flat
surface does, as its' surface has a "bubbly" appearance
under magnification that can reflect
light in many directions. If you find
"glittery" gold, KEEP IT! It is gold's
crystalline form, rare, and
very valuable as a collectors item,
and can sometimes be best identified
under magnification.
After this simple explanation, you
will find a more detailed
explanation with references from
Lapis International 5th book on
gold.
Color is
also a good indicator of gold.
However, there are many variations
on the color gold can be identified
with. Most of it is not in its'
pure form and is combined with
copper more than all other metals.
Iron, silver, sulphur, tellurium,
lead, and several lesser minerals in
varying amounts can be found with
gold. In its' purest form, it is a
warm buttery yellow color. Copper
turns it orangish to burgundy
brownish, silver turns it pale
yellowish-green, iron-purple to
blue, tellurium-silverish grey,
lead-blackish. Many of these
minerals can be combined with the
gold together, producing any
variation of the above colors. And
this is only the simplest forms it
can be found in! Can you say "calaverite"?
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Then, there is malleability.
This one is easier. Gold
is a soft metal, easily
flattened and formed into
shapes and figures. It has
rounded, soft edges. If
your sample has square edges
and is brittle, it is
probably not gold. I say
"probably" because gold can be
put into the pores of iron
pyrite under hot water
solution conditions. The
super heated water, with
gold particles dissolved in
it, can place the gold into
the pyrite pores where it
solidifies. And you
thought we were only talking
about magma! Now, you ask
why we CARE |
about iron
pyrite. Well, iron pyrite is known
as "fools gold". It is heavy
with iron, (not
as heavy as the real thing, though)
shiny and metallic in appearance, as
well as silverish to yellowish in
color. And, it is abundant. You
want it to be gold SO much, you can
convince yourself that it is. And
while it may carry gold with it, it
isn't what the placer miner is
looking for. We leave that for the
hard rockers who are into milling
the very nasty sulphides out of it.
So, are
we confused enough yet? Alrighty
then! Let's press on!
Last,
but certainly NOT least, is weight.
Gold is HEAVY. It is VERY HEAVY.
Pick any rock of equal size to the
piece you are curious about and the
gold will be much heavier. Gold has
a specific gravity of 19.1 to 19.3.
( I can find it published in either
number in half of the gold books I
own). Specific gravity is the water
weight relationship of everything to
water. Specific gravity is why
placer mining and water separation
works so well. The gold is 19 times
heavier than water. The only thing
that would be heavier is platinum.
Oh, keep that, too, if you find it.
By comparison, iron's specific
gravity is around 11, and lead 13.
What is
gold? In its purest form, it is a
soft, noble, malleable metal, yellow
in color with resistance to
corrosion or oxidation and does not
rust or tarnish under normal
conditions. Its' English name
probably comes from the Old English
word meaning yellow, and its
chemical symbol AU from the Latin
term for gold, Aurum. In its
uncombined form it has one stable
isotope with an atomic mass of 197
in its nucleus and 118 neutrons and
79 protons.
Gold
forms alloys with numerous other
metals, most commonly the ones
nearest to it on the periodic
table. It combines most readily
with copper. Viktor Goldschmidt
classified gold as a "chalcophile"
meaning that gold has an affinity
for sulfur. However, there are no
known combinations of gold and
sulfur. However, there are
several combinations of gold with elements that are
related to sulfur, namely tellurium
and selenium. Another alloy of gold
is electrum, a combination of gold
and silver usually 25%, but the
silver content can be as much as
50%, and used extensively in the
ancient world for coinage, although
not necessarily from a natural
state ref. extra Lapis English No 5
"GOLD The Noble Mineral" by Lapis
International, LLC;
This
book from Lapis International is a
terrific scientific look at gold,
put into layman's terms Hooked On Gold
highly recommends it.
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These sample rocks are
pretty good examples of what
you might find in the field.
Based on the information on
the page, which rock would
be the "Real Deal", and
which one is for the "Fool"?
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Identifying gold in the field, or
anywhere else, should include
several indicators for the serious
or weekend prospector. Color,
brightness or shine, shape of
pieces, and weight. Remember that
gold is YELLOW and variants of
yellow, soft and rounded, (NOT
cubical and brittle) bright without
being shiny, and HEAVY. So, now,
what do you have in your hand?
For more
examples of gold visit
For the Love of Gold Photo album
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Copyright 2005-2010 Shirley
Weilnau All rights reserved
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