Naked Science Forum
Non Life Sciences => Geology, Palaeontology & Archaeology => Topic started by: VistaHunter on 14/08/2012 01:15:19
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Hello,
I have an interesting rock that I would like some help in identifying. I found this rock on my friends property up by Mt. St. Helens in Washington State. For a long time I actually thought this rock was a meteorite because it appears oriented, is weakly magnetic, and has very thin black coatings in areas that I thought may have been remnant fusion crust.
I know now that it is not a meteorite because I sent a sample in to New England Meteoritical Services for petrographic analysis. They informed me that it is a volcaniclastic rock composed of chalcedony.
The rock fascinates me very much and I would like to learn more about it.
How did it form?
Clearly it came from the bowels of Mt. St. Helens right?
Was it once a giant molten geode?
Did brecciation occur on impact?
Any insight would be much appreciated!!
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Here is a slab photo.
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What are the black inclusions within the matrix that I can scrap out with my fingernail? Carbonates?
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What is the brown substance throughout the matrix that gives the agate a yellow golden hue? Sulfides?
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One Crystal appears to have formed wavy bands or perhaps was melted and warped. Why?
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Another crystal has formed or was recrystallized right in the middle of dense agate. Why?
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Closeup of breccia.
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More Slabs.
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What you found is not uncommon in near volcanoes. Your rock is probably a lava flow breccia that had its voids filled with chalcedonic silica. The banded "wavey" agate is typical, as the hot fluids circulated through the breccia and precipitated silica and/or replaced precipitated calcite.
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Thanks Bass.
Can anyone tell me what the soft black inclusions within the matrix might be?
What might the brown substance be that leached into the agate and quartz?