Liquid and gaseous minerals

The very name liquid and gaseous minerals already contains something incongruous. All because we have good reason to imagine mineral something, then hard. It turns out that liquid and gaseous minerals exist in nature. Simply geology under the terms mineral, stone or rock formation understands the whole inorganic nature, regardless of whether it is liquid, solid or gaseous. This position of science is explained by the fact that the division of nature into these three states is conditional and depends on the surrounding a temperature. If the average temperature on Earth dropped or increased, for example, by twenty degrees, many minerals would transfer to other aggregate states, but the terminology would not change from this.

The very name liquid and gaseous minerals already contains something incongruous

Water, mercury - these are the main liquid minerals known now in nature. The most important of these is, of course, water - a very important liquid mineral for mankind, with which many strange things are connected. Oil is widely used in industry, and native liquid mercury is sometimes found in various deposits in the form of small droplets.

In addition to mercury at a non-high temperature, some substances also exist as liquid. For example, metal gallium. It looks like real solid metal, but in the palm of your hand it begins to melt: the heat of the hand is enough to turn it into a sparkling liquid.

Gaseous minerals oxygen, nitrogen, neon, argon and krypton surround us in the atmosphere, and the earth's crust is imbued with huge amounts of gases. For example, one cubic kilometer of granite concludes up to 26 million cubic meters of water, up to 5 million cubic meters of hydrogen and up to 10 million cubic meters of carbonic acid, nitrogen, methane and other gaseous substances. These same gaseous minerals firmly hold magma. Slowly, during long geological epochs, the inner core was freed from these reserves of gaseous minerals, piercing them with a hard shell. At the so-called explosion temperature, they quickly stand out, splitting a piece of rock into minute debris. It is with these explosions that the origin of volcanic activity is related, since volcanoes highlight in the terrestrial atmosphere, colossal amounts of gaseous minerals.

Gaseous minerals, getting into the water, sometimes form tasty and useful mineral waters, and sometimes they contain combustible components that represent fine fuel.

During the decay of radioactive substances, gaseous helium minerals are emitted, as well as other heavy gases, emanations of radium and thorium. They quickly pass their life cycle and again freeze in the form of heavy and slow-moving atoms of solid matter.

All these processes lead to the fact that Earth loses these gaseous minerals. Overcoming the forces of gravity, light atoms are freed from the power of the Earth and fly back into the world of interstellar spaces.