July 2009 Archives


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This delicately detailed pair of stones seemed a bit out of place among all the other material at the mine dump. I couldn't leave them there. A quick scan in a couple field guides suggests Dendritic Pyrolusite. However, it appears that the true mineral identity of the dendrites requires some meticulous laboratory examination...which means I'll leave this identified generically for now.

Eric Graff has been providing a lot of helpful input on the specimens I've posted so far. He notes the following about this one:

Interesting rock! My first guess would be tenorite, CuO, (the only mineral listed from Iron Springs District that is noted for the formation of dendritic patterns).

From Mindat entry on tenorite: http://www.mindat.org/min-3912.html

Morphology:Paper-thin twinned aggregates and laths parallel {100} and elongated [011] (Vesuvius); striated [010] on {100}. Curved plates. Thin shining flexible scales. Stellate groups. Earthy, pulverulent.

Twinning:1. Common on {011}, producing dovetail reentrants and feather-like forms as senn on {100}; also stellate groups andcomplex dendritic patterns. 2. On {100} ?

My second guess would be iron oxide (hematite) as I've heard that can also form dendritic patterns. While manganese oxide does frequently form these types of structures, I don't see any manganese-bearing minerals from that district.

Eric

Thanks Eric!

I'm wondering about scraping some of it off and attempting a flame test on it...


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Mineral TypeDendritic Condensations
Size21 x 7 x 8 cm, 8 x 7 x 3 cm
Collection ID09062105J, 09062106J
Collection LocationNear Comstock Mine, Iron Springs County, Utah, USA
37:36.874 N 113:23.576 W
Collection DateJune 21, 2009


White Light View
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Long Wave UV View
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Amanda collected this little chunk of crystal-infused magnetite. It featured two different types of crystaline structures. The best part though was seeing it under a black light. The two different crystal types fluoresced with different colors: yellow and orange. Additionally, some less prominent material exhibited a white fluorescence. It should be interesting working on identifications for this one.

The LW Ultraviolet images can be seen below each of the white light views. Visible in the second set of images is a beautiful, thin vein of the white-fluorescing material along a less exposed edge of the stone. This was my second attempt at black light photography. It turns out to be pretty tricky. My first set of image exposed a huge amount of visible purple from the light that didn't seem as prominent visually. A lot of heavy color balance gymnastics in the camera RAW conversion process brought it back to something that was workable. Further work in the LAB color space while looking at the rock under black light was also required to take it the rest of the way.

After doing some more research, I picked up a Long Wave UV Filter from UV Systems. I also picked up an 18" black light bulb manufactured by Phillips since it apparently has a higher density of UV compared to visible emission. Placing the LW UV filter across the bulb produced a noticeable reduction in visible purple and the photographs turned out much better. I didn't need to horse around with color balance in RAW or LAB. The only issue was some of the crystal faces that reflected the light directly into the camera still possessed a purple appearance, and I needed to use the selective color filter to remove that. The images you see here are a result of that 2nd set of photographs.


White Light View
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Long Wave UV View
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Mineral TypeMagnetite - Fe+2Fe+32O4
Unidentified Crystal
Unidentified Crystal
Unidentified Crystal
Size11 x 8 x 3 cm
Collection ID09062104A
Collection LocationNear Comstock Mine, Iron Springs County, Utah, USA
37:36.874 N 113:23.576 W
Collection DateJune 21, 2009

Calcite on Magnetite - 09062103J


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The larger crystals on this rock are about 1 cm in length.


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Mineral Type

Calcite - CaCO3
Magnetite (Matrix) - Fe+2Fe+32O4

Size15 x 16 x 8 cm
Collection ID09062103J
Collection LocationNear Comstock Mine, Iron Springs County, Utah, USA
37:36.874 N 113:23.576 W
Collection DateJune 21, 2009
Testing Results

Crystals:
Acetic Acid: Positive Reaction
Streak: Colorless
Hardness: 3

Magnetite:
Magnetism: Positive, weak
Streak: Dark Gray
Hardness: 3-6

Magnetite - 09062101J


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This piece of magnetite possessed the largest crystals of those we found on July 21st. Although, even at that, the longest edge on any of the crystals is no more than 6 mm.

Mineral TypeMagnetite - Fe+2Fe+32O4
Size6.5 x 5.5 x 2.5 cm
Collection ID09062101J
Collection LocationNear Comstock Mine, Iron Springs County, Utah, USA
37:36.874 N 113:23.576 W
Collection DateJune 21, 2009
Testing Results

Magnetism: Positive, weak
Streak: Dark Gray
Hardness: 3-6


Click image for larger version.

This is one of several magnetite rocks we collected from one of the rock dumps near the Comstock Mine in Iron Springs County, Utah. I'm working on identifying the orange crystals and will update this entry when I figure it out. Below is an enlarged view.

Mineral TypeMagnetite - Fe+2Fe+32O4
Unidentified Crystal
Size11 x 11 x 8 cm
Collection ID09062102J
Collection LocationNear Comstock Mine, Iron Springs County, Utah, USA
37:36.874 N 113:23.576 W
Collection DateJune 21, 2009
TestingMatrix:
Magnetism: Positive, weak
Crystals:
Acetic Acid: Negative Streak: Colorless Hardness: 3-6

Introduction

Since October 2004, I have maintained the Belt of Venus website where I have been able to share my enjoyment of amateur astronomy. The treasures that lie deep in the vast cosmos aren't the only things that capture my fascination. Although we lie enmeshed in an enthralling universe, this thin, beautiful bubble of life is pretty hard to ignore. If you enjoy meteorology, geology, botany, zoology--all of those -ologies, -ographies, and -anies--well, so do I. I am easily distracted. I want this to be a place where I can share some of those interests. The Belt of Venus has taken on a life of its own, and I want to keep it strongly focused, so this is where I will try to explore these other natural wonders as the opportunity arises.