The movement of peat machines is complicated by the presence of unevenness in the form of bumps and stumps, high moisture content of the deposit in some areas and, finally, deformability of the peat deposit. All this significantly worsens the passability of peat machines in comparison with machines moving on flat hard ground. The purpose of the tests is to select the most rational frame variant in terms of its durability, minimum weight and manufacturability of construction.

The author's model of the cognition process called transfinite is proposed. The objectivity of this model is illustrated by paradigm shifts in geology. The formulation of postulates of the last quantum paradigm is given.

The energy content of rock, the calculation of which was proposed by the author in earlier works, is considered as the energy of rock existence. By analogy with the energy of existence of a particle (rest energy), a certain limiting velocity is derived from this value, beyond which the rock as an element of the Earth and the Solar System ceases to exist. The invariance of the interval between geological events is based on it.

In modern geology we can state a paradoxical situation: on geological maps and sections of essentially any purpose time and space are geometrically combined, moreover, they are represented by a mass of rocks that can be characterized by a certain stock of internal energy, and the relationship between these fundamental physical parameters remains virtually unexplored.

Quite a lot has been written about actualism in geology. And this fact alone indicates that the issue is not only complex, but also extremely important.

Zonality is a planetary property of groundwater that determines the shape of its spatial and temporal arrangement in the Earth's interior. This definition requires clarification of the physics of our ideas about zonality.

It is known that the most active interaction between land postdemic waters and sea basins occurs in the areas of alluvial flows, as river valleys are powerful natural drains ...

Hydrochemical studies in the basin of the lower reaches of the Amur River within the Miaochansky Range proved the possibility of using hydrochemical methods to search for tin-polymetallic deposits in the mid-mountainous relief under humid climate. In this article, the features of the formation of the chemical composition of water in this area, touched on the issues of quantitative assessment of the results of hydrochemical searches.

As it is known, mineral waters of Matsesta are diluted with fresh waters of meteoric origin at a considerable depth. The main mass of fresh water enters the depths of the deposit from the north-east, from the zone of the Akhshtyr, Akhun and Bytkha ridges, through a system of open cracks and karst passages. Dilution processes at Matsesta have captured the water-bearing limestone strata to a depth of about 900 meters. The dynamics of this process has been studied in great detail, and the hydrochemistry is still not sufficiently clear and understood ...