Hi,
When going over well hunted areas looking for nuggets, try to look for spots others pass by. I was working my way up a lead and not having much success, when two large rock masses (schist tors) rose up either side of the lead.
Now every man and his dog had detected up the trail between the rocks but I happened to notice a little ledge about knee height on the side of one of the tors, and it had been capturing a small amount of dark earth that had worked its way down from the top of the tor.
I had to consciously lift up the coil to scan it and 'boing' a signal, now one usually finds a heap of 22 shells around these tors, since its a great place to scan the area from and pick off bunnies. It sounded more solid than a shell casing and it sure was, as the pic shows, it was a nice little pennyweight piece.
So the moral of the story I guess is, imagine you are a nugget, eons ago slowly working your way down the slope, look for spots where you might come to rest, maybe on a rock, which after a lot longer is left high and dry as the earth and softer rock around it is worn away.
Cheers
Kev
PS I had to come back in and edit this post since this is on a PI Technology forum and this post is a bit off topic. So the technology bit is, I was using a compound pulse stream of 20us 60us 20us 60us etc., when I found this piece. In the past I have found 20us 40us 60us 20us 40us 60us etc., very good, much better than a totally synchronous train, but the point is, I believe the former train pattern is less affected by mineralisation than the latter, I don't at this stage know why though?
When going over well hunted areas looking for nuggets, try to look for spots others pass by. I was working my way up a lead and not having much success, when two large rock masses (schist tors) rose up either side of the lead.
Now every man and his dog had detected up the trail between the rocks but I happened to notice a little ledge about knee height on the side of one of the tors, and it had been capturing a small amount of dark earth that had worked its way down from the top of the tor.
I had to consciously lift up the coil to scan it and 'boing' a signal, now one usually finds a heap of 22 shells around these tors, since its a great place to scan the area from and pick off bunnies. It sounded more solid than a shell casing and it sure was, as the pic shows, it was a nice little pennyweight piece.
So the moral of the story I guess is, imagine you are a nugget, eons ago slowly working your way down the slope, look for spots where you might come to rest, maybe on a rock, which after a lot longer is left high and dry as the earth and softer rock around it is worn away.
Cheers
Kev
PS I had to come back in and edit this post since this is on a PI Technology forum and this post is a bit off topic. So the technology bit is, I was using a compound pulse stream of 20us 60us 20us 60us etc., when I found this piece. In the past I have found 20us 40us 60us 20us 40us 60us etc., very good, much better than a totally synchronous train, but the point is, I believe the former train pattern is less affected by mineralisation than the latter, I don't at this stage know why though?