Kemerovo - Supply of Coal

Coal is one of the major minerals in the world, the extraction of which is the main direction of the Russian industry. Of course, the field of coal sales occupies a relatively impressive segment in the world market. Nowadays, the coal breed is in high demand, because for many years it is the most popular solid fuel in everyday life.
In particular, the export of coal Kuzbass is known throughout the world. Active supplies of coal by wagons are carried out in the Kemerovo region. The sale of coal in Kemerovo is executed thanks to the work of over fifty mines and 36 coal quarries. And the first coal was mined here as early as 1933. Coal delivery to Kemerovo these days is a distributor of more than 50% of all consumable coal fuel in Russia. The largest exporters of coal are only domestic companies, since our coal provides more than half of the world. Because of this "buy coal in Kemerovo" - the offer is invariably relevant. In addition to buy coal breed Kuzbass usually seek at a moderate cost, many customers. For this reason, nowadays it is not difficult to buy hard coal in bulk. Purchase of coal ore is possible at a bargain price for all parties. And actually "I'll buy coal in bulk" means the selection of the optimal acceptable rates. In addition, all exporters of coal can offer the best prices for all comers. Since all exports of coal ore Kuzbass is focused on meeting the global consumer demand. Therefore, all domestic suppliers of coal are heading for an optimal sales market.
Buying coal ore, it is necessary to understand its types. All sold brands of coal have the following deciphering: G - gas, A - anthracite, K - coke, OC - fumed caking, T - lean, B - brown coal, F - fatty, SS - weakly sintering, D - long coal. The name of each species often contains a symbol meaning an oxidizing number (for example, OK2). In general, the scope of use of this fuel is very wide. After all, this kind of fossil fuel was used by people one of the first. Coal has practically carried out the world production revolution, which contributed to the wide development of the entire coal mining sector. By the way, the age of most known coal deposits is about 350 million years old.
The actual formation of coal is possible due to a rich accumulation of plant mass and the absence of dioxygen. Actually, the coal rock itself is formed in conditions if the accumulation of decaying phytomass occurs more likely than its natural decay. Naturally, the optimal conditions for this is standing water without oxygen circulation, which does not allow bacteria to breed. These conditions, in turn, must protect from the decomposition of a single layer of phytomass. Thus, the natural formation of peat mass occurs, the so-called original material for the formation of coal ore. However, the methods for extracting this coal directly depend on the level of the deposits.