letitridek
having dreams about rocks
Member since April 2017
Posts: 55
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Post by letitridek on Mar 12, 2018 14:32:31 GMT -5
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Deleted
Deleted Member
Member since January 1970
Posts: 0
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Post by Deleted on Mar 13, 2018 11:39:21 GMT -5
First one looks a bit like some of the material from the Owyhee Sunset area. Does 2 have any metallic inclusions? Number 3 is brecciated jasper, and from the pieces it looks like it is also from the Owyhee basin. I've seen Owyhee jasp with areas of breccia, but nothing quite that wild.
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Fossilman
Cave Dweller
Member since January 2009
Posts: 20,718
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Post by Fossilman on Mar 13, 2018 13:22:02 GMT -5
Number two looks like a type of granite stone...
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minerken
Cave Dweller
Member since August 2013
Posts: 466
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Post by minerken on Mar 13, 2018 13:29:24 GMT -5
Please don't be offended but the third pic probably should be considered a conglomerate rather than a breccia. Because the fragments are rounded instead of being angular indicates that it is of sedimentary origin and has been cemented in a similar way as concrete. As far as a jasper from the Owyhee basin sure no problem.
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Post by rockjunquie on Mar 13, 2018 13:36:28 GMT -5
I thought 1 might be wood, 2 granite and 3 some kind of pudding stone- conglomerate.
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Post by fernwood on Mar 13, 2018 15:24:48 GMT -5
1 does look kind of woody, doesn't it? Would need a photo of a barky looking edge and then a smooth one.
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Deleted
Deleted Member
Member since January 1970
Posts: 0
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Post by Deleted on Mar 13, 2018 16:50:30 GMT -5
Please don't be offended but the third pic probably should be considered a conglomerate rather than a breccia. Because the fragments are rounded instead of being angular indicates that it is of sedimentary origin and has been cemented in a similar way as concrete. As far as a jasper from the Owyhee basin sure no problem. No offense taken, but piece 3 is not a sedimentary conglomerate. This is typical monomict breccia formed by chips popping off the host rock. You often find this re-silicified material directly attached to the host rock from the broken pieces spalled off (due to weathering, tectonic activity, etc.). As to angularity, there are some angular pieces in there, and it isn't always possible to see all the angles and straight lines in a slabbed piece. BTW, I asked whether there were any metallic areas in the second because there are some ore-bearing stones (such as pulsite and Josephine's Crown) that look similar and are cut into gemstones. Difficult to detect metallic flashes in a photo.
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letitridek
having dreams about rocks
Member since April 2017
Posts: 55
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Post by letitridek on Mar 13, 2018 17:32:07 GMT -5
there is no metallic areas in the second one as far as i can tell here is a picture of the edge of the first one if that helps P1000250 by LETITRIDEK, on Flickr
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Post by mohs on Mar 13, 2018 17:42:51 GMT -5
diorite came to mind for the black & white
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NRG
fully equipped rock polisher
Member since February 2018
Posts: 1,688
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Post by NRG on Mar 13, 2018 18:19:29 GMT -5
diorite came to mind for the black & white If not metallic as pointed out above, I'll vote for grano-diorite
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minerken
Cave Dweller
Member since August 2013
Posts: 466
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Post by minerken on Mar 13, 2018 21:07:42 GMT -5
"monomict breccia" Okay consider me corrected
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Post by rockjunquie on Mar 13, 2018 21:18:12 GMT -5
OK, now you guys are just making stuff up. LOL!!!!!
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minerken
Cave Dweller
Member since August 2013
Posts: 466
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Post by minerken on Mar 13, 2018 22:41:21 GMT -5
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Post by rockjunquie on Mar 14, 2018 7:46:11 GMT -5
I was only kidding. I believed you.
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Post by rmf on Mar 15, 2018 20:45:53 GMT -5
#3 is TN puddingstone if it is from TN. They also find identical material in AL, MS, AR and OK They may use different names there. this is a chert conglomerate cemented by limonite. It is messy to cab and hard to tumble but does take a great shine.
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QuailRiver
fully equipped rock polisher
Member since May 2008
Posts: 1,640
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Post by QuailRiver on Mar 20, 2018 3:16:28 GMT -5
rmf is correct about number 3. There was a lot of that material from Tennessee floating around at the rock & gem shows in the Southeastern U.S. back in the 1970s being called "Flint Conglomerate". Later some folks were (and still are) calling it "Tennessee Puddingstone". I think I still have some of it around here somewhere. Best I remember it was sort of soft, at least in areas, but did take a good polish.
Larry C.
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