Gold depositsGerman Group
In an area either common or known as gold possession, where should you look first?
Table, surrounding hills, washing, or just where?
The gold properties in that area will help you figure out where to start.
If the gold is flat and cut, it indicates that it was in the water a long time ago.
If the gold is rough and decorated, you know you’re approaching the source.
When the gold is smoother, stop and go back to the hidden gold and start working up until you find the source.
Remember that gold is gold, so there is not necessarily a better kind of gold.
Some are easier to recover.
There are only two kinds of gold deposits:-
-The first type is Lode
which is simply everything that’s still in the matrix and in the ground.
gold deposits refer to gold that is still closed within its original solid rock formation This formation of gold generally begins as a rock collides and is formed over millions of years.
-The second type is placer – or anything else.
Belt deposits are the last place to go, Once the gold is released from the vein, gravity and nature do the rest.
Unless the gold is trapped in a seat, he will find his way to the water one day.
Since gold is trapped in rocks and can be mixed with quartz, calcite, Beirut, and other minerals, gold usually requires specialized mining techniques to extract it.
Plastic mining requires much more equipment, and generally much more expenditure, usually through large commercial operations rather than the average prospector.
Gold is the gold that most prospectors know best.
In fact, decorative gold is no different from old gold. It’s simply the concentration of the same gold that was eroded and traveled away from the vein.
As the gold is very dense, it will move down much slower than the deposits surrounding it.
They tend to become concentrated on or near a friendly surface and form a “back-up” near the original exposure to the base stone.
The gold found from the direct slope over the nearest waterway is called the “Granary Piper” As soon as this gold reaches the nearest waterway and is transported by flowing water, it is now known as “grenous decorum” Dust, floss, and thinners found through waving and waving are usually from the vein even on a nearby mountain.
The organ stabilizers were originally decorated.
The seats are simply where the water was in the past, perhaps even millions of years ago. It consists of erosion or geological events such as heights, earthquakes, or drops of platelets that have altered the flow of current. Some of the most profitable mining activities take place in seats. Many of the seats are largely concentrated in alloy deposits, which continue to feed them.
It could take millions of years, but he’ll get there.
When you decide where to dig, you often want to start collecting water in some way or wash in the desert, where the water flows once. Then let the gold tell you where to go from there. When the gold becomes rough and torn, start moving up, and see the opposite of how it gets to where it’s found.
In addition to liquidation and cooling, you may wish to improve your efforts in mining with a high sink or power pump, dredge, or brake. Clearly, it is much easier to move soft soil or river gravel than to break rocks, but for small-scale miners, smash rocks can fall down 2 or 3 inches of boulders to powder in a short time. Hurry up and move more stuff, get more gold!