Thurman
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- Joined
- Aug 27, 2014
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- Location
- New Smyrna Beach, FL
- Detector(s) used
- Minelab Xtera 70
- Primary Interest:
- All Treasure Hunting
The Skykomish river roars out of the Cascade range in western Washington through a historic mineralized area and empties softly into Puget Sound at Everett Washington. Rich, well documented, tributaries add to the gold content in the river. I will be speaking about the river roughly 20 miles East and West of Gold Bar, WA. I have no experience elsewhere.
My experience here is very limited (vacations), but a couple of fine prospectors (you may know them as Magic Mike and Sluice Goose!), have taught me what little I know, which is:
B. With this limited knowledge, where should one look for even better recovery? Places where the this small gold would accumulate season after season?
C. What about downstream where the whole river slows.....in all seasons?
What I would appreciate is additional conceptual thinking, as well as local knowledge from any local prospectors who are willing to chime in.
All the best, Thurman
My experience here is very limited (vacations), but a couple of fine prospectors (you may know them as Magic Mike and Sluice Goose!), have taught me what little I know, which is:
- The Bazooka will get it!
- This is a natural river with seasonal floods from snow melt and then dropping water summer through winter.
- The gold available here to the panner/sluicer is consistently small and fine.
- Extensive Sampling shows almost NO gold in the stream waters or gravel/sand bars. It would be possible to pan all day behind boulders, in the cobbles, bridge abutments, - all the places shallow and deep normally explored - inside and outside bends, without a color. I know...... this.
- YET! Should you find access to a suitable inside bend and work the rocks and gravels up-bank in the flood zone, especially in the bushes and briars, you will find gold and sometimes lots of it (relatively speaking).
- From what I read here and elsewhere, small gold can be very typical of a particular river (Snake river).
- The small gold then, carried by he "bed load" should be fairly consistent through the seasons. Perhaps more during flood since the previous season gold is being added from the banks and tributaries. But "water volume" wise, maybe about the same - if it matters here.
- Now, the small gold will drop and deposit, along with any other part of the bed load/sediment of the same weight and/or weight-resistance to water flow (there is a word for that, Doc). Yes, the black sand is with the gold.
- This fine gold, of course, will only drop and when the combination of water velocity and bottom texture allows it to deposit.
- This of course, is why flood gold everywhere is found in the shallow/slow water. Classically a sand bar (which I have read can be skimmed).
- Here, on the Skykomish, this should explain why the flour gold is almost exclusively in the flood zone "bushes." The water velocity at flood stage on an inside bend near the banks is slowest, augmented by the interference and bottom texture of the vegetation to help the small gold to drop and deposit.
- But, as the river slowly falls, why - in the now slowest water in the gravels and cobbles - does the gold not drop and deposit?
B. With this limited knowledge, where should one look for even better recovery? Places where the this small gold would accumulate season after season?
C. What about downstream where the whole river slows.....in all seasons?
What I would appreciate is additional conceptual thinking, as well as local knowledge from any local prospectors who are willing to chime in.
All the best, Thurman
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