, when a geologist describes the core directly at burovaya, they immediately take it out, the geologistnd there’s always a bucket with... and a brush, yeah, or a spray bottle to wet it, because you can see it much better when it’s wet, and what do we see? here you can see something white, and something gray, which means something gray is the host rock, these are some sandstones, maybe oleurolites, orgelites, what was once sand, clay, which were deposited at the bottom ancient sea, and then it shrank, then it shrank, heated up, pressed and cemented. and became a strong rock, and so in the strong rock, then it cracked , superheated water vapor began to flow through the cracks, we call it a fluid or hydrothermal solution, very hot, more than 100 ° for it, but still liquid, because pressure, yes, due to pressure it liquid, although sometimes there are supercritical fluids, which are indistinguishable states, liquid and vapor, above 373, it seems, degrees. which means due to the fact that he is so hot, he is good dissolves many minerals, but when it enters the crack, it interacts with these

magic is happening, wow, now it has become clear that it has become less scary, by the way, on the burovaya describes it, and there is always a bucket. with water and a brush, yeah, or a spray bottle to wet it, because you can see it much better when it’s wet, and what we see here is, well, you can see something white, and something gray, which means something gray is the host rock, these are some kind of sandstones, maybe oleurolites, orgelites, something that once it was sand, clay, which were deposited at the bottom of the ancient sea, and then it compressed, then it compressed, warmed up a little, and was pressed into cement. and became a strong rock, so in the strong rock, then it cracked , superheated water vapor began to flow through the cracks, we call it a fluid or hydrothermal solution, very hot, it is more than 100°, but still liquid, because pressure, yes, due to pressure it is liquid, although sometimes there is a supercritical fluid, which is an indistinguishable state, liquid and vapor, above 373, it seems, degrees. which means , due to the fact that it is so hot, it dissolve

wow, now it’s clear that it’s become, it’s become less scary, by the way, here at burovaya, when a geologisty from the drilling rig, they immediately take it out , the geologist documents it, describes it, and there’s always a bucket of water and a brush, or a spray bottle, to wet it, because you can see it much better when wet, and what we see here is something white, and something gray, something gray - this is the host rock, these are some sandstones, maybe oleurolites, orgelites, something that once was sand, clay, which were deposited at the bottom of the ancient sea, then it compressed, heated up, was pressed, cemented and became strong rock, and so in the strong rock, then it cracked , superheated water vapor began to flow through the cracks, we call it fluid or hydrothermal. you have to hit it right away and see what’s there there will be, but if you find quartz, this does not mean that there is necessarily gold there, even when we go to sites, we chop these quartz veins, well, 90% of them are empty, like a drum, as they say, except for quartz. which, in general , is not of great int