Just a cluster of Aragonite crystals. Specimen is about 1.5" wide. More info: http://geology.about.com/library/bl/ima ... gonite.htm
Ex. 1/2.5
F/8
ISO 100
Aragonite Crystal cluster
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Aragonite Crystal cluster
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Doug Breda
Doug Breda
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A very professional looking study Doug. I'm guessing that with the the excellent front-to-back sharpness, at 1.5 inches there was some stacking involved? Your specimen makes a nice balanced composition too.
With these crystals (or crystals in general) is there an easily identified top and bottom. Could you tell for example how this cluster was oriented with respect to gravitational pull?
Textbook quality!
Bruce
With these crystals (or crystals in general) is there an easily identified top and bottom. Could you tell for example how this cluster was oriented with respect to gravitational pull?
Textbook quality!
Bruce
Well, what I did was I took some pictures with different F stops and then I took two stacks and I just liked the way the non stacked picture came out. Here is one of the stacked shots (5 photo stack). I thought they were a little hot so I did not use it. The stack shot is a little closer.
Bruce, there is a section on the bottom of this crystal group that suggest it was attached to something else...as for oriented with respect to gravitational pull?
Stacked photo: 5 photo stack Some sharpening applied
Bruce, there is a section on the bottom of this crystal group that suggest it was attached to something else...as for oriented with respect to gravitational pull?
Stacked photo: 5 photo stack Some sharpening applied
Take Nothing but Pictures--Leave Nothing but Footprints.
Doug Breda
Doug Breda
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Bruce
aragonite crystallizes in the orthorhombic system. While these crystals appear hexagonal when looking down the c axis, this is caused by twinning. The flat ends of the crystals would be considered the top or bottom. This is the c face. The three crystal axes in the orthorhombic system are at right angles to each other and are differnet lenghts. Crystallography can be very interesting and frustrating as nature seldom produces textbook examples.
Doug Merson
aragonite crystallizes in the orthorhombic system. While these crystals appear hexagonal when looking down the c axis, this is caused by twinning. The flat ends of the crystals would be considered the top or bottom. This is the c face. The three crystal axes in the orthorhombic system are at right angles to each other and are differnet lenghts. Crystallography can be very interesting and frustrating as nature seldom produces textbook examples.
Doug Merson
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Canon T5i with Canon 70 - 200 mm f4L zoom as tube lens set at 200mm, StacK Shot rail, and Mitutoyo 5X or 10X M plan apo objectives.
My Mindat Mineral Photos
http://www.mindat.org/user-362.html#2