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oldmancoyote1

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Posts posted by oldmancoyote1

  1. Without a better focused image, it's hard to tell.  From what I see, it appears black.  The arsenopyrite that I am familiar with is usually a lighter grey color, but wikipedia shows some black specimens.  It could be a tellurium gold mineral called Calaverite.  If so, it's dangerous.  Heating it will emit poisonous fumes.

    482460966_ScreenShot2020-02-08at7_16_59PM.png.e078eb9d7154c4be3ab6680f391afb9d.pngCalaverite

     

    In general when submitting photos for mineral id, sharp focus is very important, and scratching it with a knife can leave useful clues .

  2. On 9/19/2019 at 3:38 AM, delnorter said:

    Walking back and retrieving my back pack with pan, 1/4” screen, pick and such, I decided to sample this cut bank. Filling a pan with screened material from this top grey layer and washing it out at the river...

    Thanks Delinorter.  Good hunting.  I took the week end off and detected the local park.  Found a gold ring.  First gold I found with my detector.

  3. On 9/16/2019 at 5:08 PM, LipCa said:

    I think this is what they call "prospecting".....  How have you tested the top layers?  Have you ran a half cubic yard through your box or just done sample pans? 

    Do you have any indication of how far it is to bedrock? If it is more than a couple feet, you got a lot of work ahead of you!

    What makes you think you "may" have found the right spot in the first place? It doesn't sound like you know what is on bedrock.....

    More info and we might be able to help you better

    Thanks for the reply.  Here is the deal.  The creek is quite small, about 12 feet across at most points.  I have dug down about 2 feet at four locations where the bed rock is exposed close by, and I have sluiced or panned the entire hole.  At 73 this is very hard work.  After two feel I am exhausted.   I don't have many of those holes in me.  My experience here and the experience of a friend is that the gold only starts about 2 feet down.  

    The creek was mined in the 1800's, again extensively mined with a huddle bug about the beginning of the last century, and judging by the ages of the beer cans, several times after to some degree.  I am worried that most of the gold is gone and all that remains is on the bedrock.  

    I guess I am looking for some encouragement.  Sampling and panning the length of the creek to find mineable  surface material is daunting when I worry that the creek is pretty much exhausted.  It takes an 7 foot wide hole through the cobbles etc. to expose the bedrock at 2 feet.  Only a hole that wide will remain free of sliding sand.  If I can find a place where the upper layer pays at least a little, I can see putting in the work to reach bedrock where I would expect most of the gold to lie.  I dread spending a summer exploring the length of the creek and finding nothing.  Am I naive to think I might find a surface exposure with mineable gold?  Geology I understand, but practical mining has very little to do with geology.

  4. Around here in the Klamaths bedrock is at lest 2 feel down and often much deeper.  Digging through several feet of boulders and cobbles is serious hard work.  Then there is sand sliding in from the sides making progress very slow.  To beat that, I need to set the sides of the hole far apart or I get a hole with a hand-sized bottom continually filled with sand from the sides.  That is a lot of work.  Historically the creek was a huge gold producer.  I see little or no gold in the upper material.  Have I just not found the right spot, or is sluicing here hopeless?  Should I spend more time prospecting for productive material near the surface, or give it up?

  5. I'm a bit skeptical of it being a meteorite, but it is hard to tell from photos.  Iron meteorites have a rusty coating and of course respond to a magnet with a loud clank!  Stoney meteorites are usually coated with a black crust.  Inside they are often granular, a bit like granite, or composed of dark green olivine.  It's an odd shape for a meteorite lacking aerodynamic qualities.  Looks a bit like a petrified pregnant rock troll.  :  )

  6. I think an important point is just how flexible a cell phone or tablet based system is.  As a sometimes iOS programmer I am frustrated by the limited information displayed on my detectors.  There are wonderful things I could do if I could import data into one of my iOS devices.  As it is easy to import the audio, I am toying with what I might do with it including 3D maps, vertical profiles and trace stacking to reduce noise.  There are technical issues, but I think I could overcome some of them.  Maybe next winter.

    I'm hoping to someday see a mainline detector with data-out streams.  I'll geek out if I do.

  7. It's often a good idea to check out anything that's different or anywhere there is a change of some kind.  Contacts can be a good choice.  If it works out, keep at it, but don't push things beyond a reasonable effort.

    Regarding the photo, you have indicated a contact between a blue soil and a red soil emphasized by a change in topography.  It might work out.  Try it.  Don't overlook the contact between blue and red soil along the upper right corner either.

     

    Good luck.

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