The 22nd Street Show is
one that I attend every year as it offers something for everyone! The event is held inside of a giant tent (or
so they say) anchored on a concrete floor.
Like most of the ancillary shows the parking lot is gravel and a
tremendous amount of dust greets visitors upon arrival, When I first attended the Show several years
ago a hot dog was about the best one could do for lunch. Today the food trucks have found the location
and a variety of decent food is available.
The 22nd Street location is also the building where many of
“The Prospectors” of TV “fame” hang out
and sell their wares. There seems to be
a big market for signed posters and selfies with one of the celebrities!
Prospector Amanda at her booth. |
How this stylized human figure composed of metal
relates to rocks, minerals and fossils is beyond my realm of thinking.
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You name it; you take it home.
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A wash basin for all with lots of partial cephalopods direct from Morocco. I have often wondered how many cephalopods have been collected from Morocco?? |
Last year I purchased several
specimens of red spinel and ruby from a Pakistani dealer, and had some very
nice conversations. This year that
particular dealer was absent, as was another dealer who always had several
tables of minerals and crystals. Instead
the tent is increasingly being populated by some rather ecletic items of little
interest to me.
However, I was able to hunt through
some mineral tables and pick up a specimen of afganite, another one of those $5
minerals that displays a nice bright blue color and is rather uncommon in
collections. I felt fortunate in being
able to ferret out this sample.
A very nice reproduction of the Cretaceous carnivore Albertosaurus offered for sale by
Tribold Paleontology over in Woodland Park, Colorado.
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An impressive reproduction of Torvosaurus, a large carnivore from the Jurassic Morrison Formation
(Skull Creek Quarry, private) near Dinosaur, Colorado.
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Afgahnite is a sodium, potassium, calcarous alumosilicate with a very complicated chemical formula: (Na,K)22Ca10(Si24Al24O96)(SO4)6Cl6 . It usually is a striking blue in color but at times the mineral is white, as is the streak. Afghanite has a medium hardness of ~5.5-6.0 (Mohs) with a vitreous luster and a translucent to transparent diaphaneity. It has a conchoidal fracture as occurs as massive blue material with scattered crystals (hexagonal system). For example, the photos on MinDat are almost always nice doubly terminated dipyramidal crystals while my specimens only has the faintest outline of crystals. It is, or is related to, the feldspathoids, a group of minerals with a low silica content that are not found in rocks containing primary quartz. My specimen has a matrix of metamorphic marble as do most of the specimens from the primary locality where the host rock is a skarn zone (where a limestone has neen intruded and cooked) in an Archean (Precambrian) gneiss and schist: Ladjuar Medam (Lajur Madan; Lapis-lazuli Mine; Lapis-lazuli deposit), Sar-e Sang (Sar Sang; Sary Sang), Koksha Valley (Kokscha Valley; Kokcha Valley), Khash & Kuran Wa Munjan Districts, Badakhshan Province (Badakshan Province; Badahsan Province), Afghanistan Location from MinDat.