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Panning for Gold (45 minutes)
Did you know that there is gold in the
Connecticut hills? In this experience in your classroom students will actually
pan for fool's gold. Discover how gold is found and
examine various rock samples containing gold and other precious metals.
This hands-on classroom
presentation begins with the students seated at their desks with a brief
discussion of natural resource usage in Colonial Connecticut. The mining of ores
and minerals in the State has had a bright and colorful history; however, gold
mining was not an integral part of that history. Gold is found in the state, but
has never been that abundant, mostly in the form of placer (secondary) deposits,
rather than the more richly concentrated lode (primary) deposits. The Lead Mine
Brook in Thomaston is a source of placer deposits. Instructor will show a sample
of gold found at the brook, (four small flakes that required 11/2 hours of gold
panning!) Next a variety of Connecticut ores and minerals will be shown, where
they are found, their uses today and where they might be found in your house.
Example will include iron, copper, nickel and lead ores, and minerals like
quartz, feldspar, chlorite, fluorite, steatite, barite, kyanite, muscovite,
dolomite, and garnet. Historically, gold rushes
happened in other parts of the U.S., North Carolina, California, and Alaska. The
people who profited the most from these rushes weren’t the miners, but the
suppliers of mining equipment, picks, shovels and clothing, the instructor will
tell the Levi-Strauss story. To pan for gold the property of specific gravity
must be understood. This property is demonstrated by a student who is asked to
hold a piece of pumice, an extremely lightweight volcanic rock in one hand and
similarly sized piece of magnetite, an extremely heavy iron ore, in the other
hand. The students in the class can easily see the difference in the density of
these two samples, by the student’s reaction. Gold panning works because gold is
extremely dense and tends to settle down in placer sands.
Students are then gathered
around a water tub to see a panning demonstration. Placer sand containing iron
pyrite (fool’s gold) is put into the pan, water added, and the water swirled in
a circular motion, throwing a bit of water and waste sand into the tub with each
motion. This process is continued until ‘gold nuggets’ appear, these are removed
and placed into a plastic bag i.e. a ‘poke’ (in mining days was a leather pouch
used to hold gold.) This gold will be collected by the students and assayed
(weighed out for its value) at the end of the program. Students are then divided
into groups of four, which “stake a claim” at a water tub complete with a gold
pan and a ‘poke’. The instructor will bring placer sand around to claims,
students will pan as time permits, students will then return to their seats, and
the assay will take place. The value of gold has
historically been influenced by economic, political and social condition. Gold
has always been viewed as a safe investment. Gold is also measured in troy
ounces. Twelve troy ounces equal one pound as opposed to sixteen avoirdupois
ounces per pound. By this measure there are 31 grams per troy ounce. The student
will measure the weight of their gold in grams, multiply this by the current
value per gram to obtain the total value of their sample. After the assay of all
the teams gold samples additional ‘pokes’ will be handed out to all students and
the gold divided among the ‘claimholders’. Access to water, a sink and six, four
foot by four foot floor space areas for students to work at is necessary for
this program.
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