matthew textor Posted April 20, 2009 Share Posted April 20, 2009 Hi this is Matt can anyone tell me what these crystals are on this rock the crystals are shiny and are copper like color I found it in a creek in Kennedy N.Y. here is 2 photos Link to comment Share on other sites More sharing options...
Northern Sharks Posted April 20, 2009 Share Posted April 20, 2009 I'll hazard a guess and say pyrite There's no limit to what you can accomplish when you're supposed to be doing something else Link to comment Share on other sites More sharing options...
2ynpigo Posted April 21, 2009 Share Posted April 21, 2009 It's often hard to identify minerals from photographs. Any way to get a pic at higher magnification? The crystals look translucent and smoky in color, perhaps quartz. But I can't see them well enough to be sure of an ID. Link to comment Share on other sites More sharing options...
tracer Posted April 21, 2009 Share Posted April 21, 2009 i think i might be seeing some rhombic crystal shapes in the upper right, and the color could easily work with calcite, but what i don't know about this could fill volumes. nice mineral specimen, though. Link to comment Share on other sites More sharing options...
2ynpigo Posted April 22, 2009 Share Posted April 22, 2009 So three common minerals have been suggested. I really doubt its pyrite as the grains are translucent and not opague. To be sure, if you can separate a grain, and crush it to a powder. Pyrite crushed to a powder is black (pyrite has a black streak). Crushed calcite and quartz are white. If you can separate a grain, then put a drop of muratic acid, hydrochloric acid, or vinegar on it to see if it bubbles. Calcite, being a carbonate, will bubble in such acids. Note that the reaction to vinegar will not be as vigorous as to the other acids. Alternatively, if the grain is calcite, it will not scratch glass. Make sure the glass is actually scratched and isn't just a powder of the grain left on the glass. Link to comment Share on other sites More sharing options...
MOROPUS Posted April 22, 2009 Share Posted April 22, 2009 Micaceous mineral? Link to comment Share on other sites More sharing options...
Frank Menser Posted April 22, 2009 Share Posted April 22, 2009 Next to impossible to ID something like this off a picture. There are too many things that can look like that. First we need a locality, State...County. Second, is the white rock quartz or calcite. Take a knife and see if you can scratch it. if you can it is Calcite if not - Quartz. This will narrow down the associated minerals a bit. I see no sign of clevages so i think we can rule out a white feldspar. Once those things are established we can more accurately speculate on what those amber xls are. Be true to the reality you create. Link to comment Share on other sites More sharing options...
Shamalama Posted April 22, 2009 Share Posted April 22, 2009 Looks like a Mica in an eroded white Calcite matrix. Is it from New York or Ontario? if so then it's part of the Grenville group of metamorphic rocks. I've seen Phlogopite Mica in material similar to your picture from those areas. Again these are all big IF's, we really do need more location info. Dave -Dave __________________________________________________ Geologists on the whole are inconsistent drivers. When a roadcut presents itself, they tend to lurch and weave. To them, the roadcut is a portal, a fragment of a regional story, a proscenium arch that leads their imaginations into the earth and through the surrounding terrain. - John McPheeIf I'm going to drive safely, I can't do geology. - John McPheeCheck out my Blog for more fossils I've found: http://viewsofthemahantango.blogspot.com/ Link to comment Share on other sites More sharing options...
Auspex Posted April 22, 2009 Share Posted April 22, 2009 ... we really do need more location info.Dave Mostly Matt hunts 28 Mi. Creek in Kennedy, NY. (Though that doesn't mean this piece came from there). "There has been an alarming increase in the number of things I know nothing about." - Ashleigh Ellwood Brilliant “Try to learn something about everything and everything about something.” - Thomas Henry Huxley >Paleontology is an evolving science. >May your wonders never cease! Link to comment Share on other sites More sharing options...
Shamalama Posted April 22, 2009 Share Posted April 22, 2009 Mostly Matt hunts 28 Mi. Creek in Kennedy, NY. (Though that doesn't mean this piece came from there). When I put Kennedy, NY into google, it takes me to fried chicken restaurants in NYC. Odd. ok... found it... very possible to find that kind of rock near 28mi creek. Could be a glacial erratic transported down from Canada. I had a friend who specifically went looking for that material to find "gem" quality Phlogopite and blue Apatites. Forms very deep within the crust and it's part of a whole complex of metamorphic rocks called the Grenville Provence that was formed waaaaaay back during the Grenville Orogeny when the micro-continent of Avalonia mashed into Laurentia (future North America). Essentially it's a very coarsely crystalline Marble. Dave -Dave __________________________________________________ Geologists on the whole are inconsistent drivers. When a roadcut presents itself, they tend to lurch and weave. To them, the roadcut is a portal, a fragment of a regional story, a proscenium arch that leads their imaginations into the earth and through the surrounding terrain. - John McPheeIf I'm going to drive safely, I can't do geology. - John McPheeCheck out my Blog for more fossils I've found: http://viewsofthemahantango.blogspot.com/ Link to comment Share on other sites More sharing options...
Guest solius symbiosus Posted April 23, 2009 Share Posted April 23, 2009 I don't see anything there that looks metamorphosed. Too me, it looks felsic. Very weathered K-feldspar, plagioclase, a little micaceous stuff, and quartz. Probably a very weathered erratic..., but I'm not a hard rock guy. Link to comment Share on other sites More sharing options...
MOROPUS Posted April 24, 2009 Share Posted April 24, 2009 I don't see anything there that looks metamorphosed. Too me, it looks felsic. Very weathered K-feldspar, plagioclase, a little micaceous stuff, and quartz. Probably a very weathered erratic..., but I'm not a hard rock guy. You look as if you were, though! Link to comment Share on other sites More sharing options...
Shamalama Posted April 24, 2009 Share Posted April 24, 2009 I don't see anything there that looks metamorphosed. Too me, it looks felsic. Very weathered K-feldspar, plagioclase, a little micaceous stuff, and quartz. Probably a very weathered erratic..., but I'm not a hard rock guy. A acid test in Vinegar would answer the basic question of silicate or carbonate. If it fizzes or bubbles when submerged then it's a carbonate. If it were a plagioclase I would expect a different fracture pattern and maybe some cleavage but the relative smoothness of the white areas and slight translucency just reminds me of a calcite. -Dave __________________________________________________ Geologists on the whole are inconsistent drivers. When a roadcut presents itself, they tend to lurch and weave. To them, the roadcut is a portal, a fragment of a regional story, a proscenium arch that leads their imaginations into the earth and through the surrounding terrain. - John McPheeIf I'm going to drive safely, I can't do geology. - John McPheeCheck out my Blog for more fossils I've found: http://viewsofthemahantango.blogspot.com/ Link to comment Share on other sites More sharing options...
Guest solius symbiosus Posted April 24, 2009 Share Posted April 24, 2009 Both calcite, and felspars, cleave easily; though one is orthogonal, and the other is rhombic. Too, for it to have that much calcite would indicate a carbonatite, and I don't think there are any of those in this part of the world??? But, like I mentioned, I am not a hard rock guy(are carbonatites even considered "hard rock"???). Link to comment Share on other sites More sharing options...
Shamalama Posted April 24, 2009 Share Posted April 24, 2009 I agree with you that both cleave easily but if the rock had been feldspar, I think the Mica would have less relief over the rock. To me it looks like the Mica has some books that are weathered and worn but others look somewhat intact. Mica is a much softer mineral than Feldspar and would scrape off sooner than the Feldspar in a Glacial or stream environment. But if the rock were carbonate then the Mica would remain longer than the more easily dissolved Calcite. There are large marble formations in upstate New York/Canada that this rock could have come from. Another part of the Grenville Province rocks yield a china blue massive Calcite with flaky crystals of Graphite scattered within. Sure Carbonates are "Hard Rock". Have you ever tried to crack the Laurel Dolomite to get a nice Gravicalymene? -Dave __________________________________________________ Geologists on the whole are inconsistent drivers. When a roadcut presents itself, they tend to lurch and weave. To them, the roadcut is a portal, a fragment of a regional story, a proscenium arch that leads their imaginations into the earth and through the surrounding terrain. - John McPheeIf I'm going to drive safely, I can't do geology. - John McPheeCheck out my Blog for more fossils I've found: http://viewsofthemahantango.blogspot.com/ Link to comment Share on other sites More sharing options...
tracer Posted April 24, 2009 Share Posted April 24, 2009 i'm not seeing what ya'll are seeing. i've hung around a bit in the central mineral area of texas where there's eighty'leven varieties of granite and schist and micas and feldspars out the nostrils, and what i'm seeing looks like yellowish translucent crystals a la calcite or something with limey whitish junk all over it. (p.s. - i hate that i can't talk technical enough). maybe i shouldn't be looking at this on a laptop screen. matt - smash that sucker with a big hammer, and go out and buy a canon SLR and take a macro picture of the internal structure and post it. wait, that might be too intense a methodology for the situation... Link to comment Share on other sites More sharing options...
jpbowden Posted April 26, 2009 Share Posted April 26, 2009 The brown crystals seem to be Bytownite, on maybe milk quartz can't tell the hardness from a picture. You can pick up a lot of these in Western New Mexico. Bytownite Link to comment Share on other sites More sharing options...
mstreman Posted May 14, 2009 Share Posted May 14, 2009 I believe there is a 99% probability this is phlogopite in marble (aka Calcite) and possibly fluorescent. So, yes it is metamorphic. This is consistent with both local marble exposures both North East and East of where collected and/or material brought in by glaciers from Ontario. However, the fact that it has a pristine surface and is not coated in aragonite suggests it was recent and not where it was found owing to glacial transport. Given this was found in a creek and outside the marble belts , there is a chance this washed off a railroad right of way. The material looks like material from Balmat NY talc works--most always flourescent from this location Limecrest Quarry near Franklin , NJ which is from the Franklin Marble Belt. Included the Farber Quarry, in Franklin and the Hamburg exposures. Philogopite usually occurs in igneous rocks but it is also the most common mica in marbles. Philogopite from the Balmat region is yellowish to gold to golden brown and frequently glows yellow under SW UV. Testing the rock with 10% dillute HCl ( 1 part muriatic acid with 2 parts water is close enough)will prove if it is calcite and positive flourescence with a UV SW lamp can strongly indicate it is is in fact philogopite. Eman Link to comment Share on other sites More sharing options...
Recommended Posts
Create an account or sign in to comment
You need to be a member in order to leave a comment
Create an account
Sign up for a new account in our community. It's easy!
Register a new accountSign in
Already have an account? Sign in here.
Sign In Now