Last Saturday I took the opportunity to attend a
local estate auction where the handbill advertised thousands of rock, mineral
and fossil specimens. I thought---sure, “thousands”, no way and they are
probably junk. What a pleasant surprise was in store as there were
“thousands” of specimens and while some were junque, many more were very nice
and collectable. Most of the fossils were local Cretaceous baculites and
really not collectable. There were also flats of pretty unspectacular
microcrystalline quartz available and some went for quite a few bucks!
Why? But then there were nice collectable individual specimens thrown
into flats (beer cases) with about two thirds carrying correct labels.
Some of the flats contained specimens from a single locality such as unlabeled
topaz-bearing rhyolite from western Utah. Most other flats were mixed
with perhaps the most interesting being opal (looked Australian) with barite
(almost certainly Hartsel, CO). I guess the packer saw that both were
“shiny”.
I had a great time visiting with, and bidding
against (although very hard), about 9-10 other members of CSMS. I would
guess that the ten of us purchased the great majority of the collectable
specimens. The auctioneer would start out with a flat and request bids
for any single specimen or two and then sell the remainder of the flat at a
single price. I thought that some of my buys were “quite good”!
One partial flat that I purchased had a small
crystal of anatase, something that was not in my collection and a mineral not
all that familiar to me ---but I wanted it. So for $5 I was able to “get
it” along with a beautiful, water-clear, double terminated, scepter quartz
crystal, a piece of rhodochrosite (with crystals), a nice terminated apatite
crystal, some gemmy-green, titanite (sphene) crystals, and several other
specimens. A great buy.
Driving home I kept
probing the back recesses of my mind—what do I know about anatase? Where
had I seen specimen(s)? Then something popped out, or turned on, and I
remembered by blog about the mineral brookite (March 7, 2012). There must
be some relationship! So, in examining the posting I noted my words, and
there it was—anatase: Brookite is a titanium dioxide, TiO2,
crystallizing in the orthorhombic system. MinDat notes that
brookite is one of five titanium dioxide minerals (rutile, anatase, akaogiite, unnamed) that
occur in nature---all belong to different crystal systems! So,
anatase is a polymorph of brookite!
Anatase is in the Tetragonal System while brookite
is orthorhombic; both are usually found in primary sources as single
crystals. I say primary since all of the polymorphs are not rare in
concentrations of heavy minerals from sedimentary rocks. Anatase has a
hardness of about 5.5-6, an adamantine to metallic luster, and a dark steel
blue to black color. The source for the larger crystals seems to be secondary
and derived, via hydrothermal solutions, from titanium-bearing minerals in
igneous and metamorphic rocks (www.MinDat.org)
The specimen now in my collection has a label
indicating that Minas Gerais, Brazil was the place of origin. All-in-all,
it was an exciting day. Now, off to finding shelf space!
Anatase crystal from Brazil partially covered
with a “clay mineral”. Width at junction
of crystal and clay is ~5 mm.
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Brookite crystal from Arkansas. Length is ~1.75 cm.
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ADDENDUM, 5 June, 2103. Partial large crystal of anatase from Cuiaba
District, Minas Gerais, Brazil. Length
~2.0 cm.
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