A year, for example? Out of habit, we measure a year abstractly, as the sum of a certain number of seconds, minutes, or days. The revolutions of the Earth around the Sun are like the movement of a hand on a clock face. Even geologists do not often compare a year (one revolution of the Earth around the Sun) and a day (one revolution of the Earth around its axis) with the real geological processes that occur during this process. What do we mean by a million years of geological history? A million revolutions of the Earth around the Sun? Are these revolutions really so fundamental for the Earth? The events that take place on the planet over a million years are associated with the action of many astronomical and geological forces (with the mutual rotation of the Moon and the Earth, changes in the position of the Solar system in the Galaxy, variations in solar activity, with the "internal rhythms" of the planet, etc.). The life of the Earth is influenced not only by uniform processes, but — to a greater extent — by deviations from the "norm". A tiny change in the speed of rotation releases tremendous energy in the rocky flesh of the planet. The rotation of the Earth is not only an astronomical phenomenon, but also a geological one. Every turn does not go unnoticed.
One way or another, it remains in the planet's memory. Seasonal rhythms of alternating sandy and clay precipitation, evaporation or freezing of salts in lakes, etc. are traced. The earth is not only one of the precisely calibrated wheels of celestial mechanics. She lives, reacts to external influences, and changes. And in this interrelation of terrestrial and cosmic processes, does the ghost of absolute time arise before us again? This ghost is not difficult to exorcise. After all, even within our planet, each geosphere reacts to cosmic influences in its own way, and has its own geological time scale. The change of seasons, day and night plays a significant role in the life of the atmosphere and hydrosphere. It is reflected in the seasonal stratification of precipitation, in the periodic change of temperatures, air pressure, etc. It is quite appropriate to use the standards we are familiar with — clocks. The "micro clocks" of atomic physics, counting down millionths and billionths of seconds, are pointless to use — otherwise the atmosphere will appear unchanged, "crystal" (imagine what it would look like for space aliens living — on our scale — fractions of a second). The atmosphere also reveals peculiar qualities on the scale of centuries and millennia. Here we are already forced to neglect daily and even seasonal changes, and we notice, as a rule, only age-old deviations from the "norm". Diurnal fluctuations in physical properties (temperature, humidity, density) are observed only to a depth of several meters from the Earth's surface.
Seasonal fluctuations penetrate deeper, while secular fluctuations can reach a depth of six hundred meters (this can be observed by the thickness of the permafrost). The life of the planet's interior deeper than one kilometer is practically not affected by the uniform revolutions of the Earth around the axis and the Sun (excluding phenomena related to Coriolis forces). It is possible to measure the life of the earth's interior with the help of astronomical clocks only conditionally, because here geological processes are very slow, and what corresponds to a year in the atmosphere is more fleeting than a minute. We arbitrarily, for no objective reason, raise a certain measure (a year, for example) to the rank of an "absolute time interval." We might as well proclaim a friend to be the lord of the planets and the lord of the galaxies. The special duration and length of geological time intervals cannot be reduced to a simple sum of smaller intervals. Actually, purely arithmetically, we can take the Decamiriad as a set of one hundred centuries, and, say, the geochron as a million years, the megachron as a hundred million years, etc. But in their geological essence, as applied to real geological processes, these intervals are extraordinary. During these periods, events occur in the life of the Earth that in no way occur in our usual, mundane time intervals (minutes, hours, years). In other words, the properties of geological objects vary depending on the accepted time scale. The Aviator online game brings the fun of the casino to your fingertips. Try the aviator online game and enjoy the thrill of winning big.
One way or another, it remains in the planet's memory. Seasonal rhythms of alternating sandy and clay precipitation, evaporation or freezing of salts in lakes, etc. are traced. The earth is not only one of the precisely calibrated wheels of celestial mechanics. She lives, reacts to external influences, and changes. And in this interrelation of terrestrial and cosmic processes, does the ghost of absolute time arise before us again? This ghost is not difficult to exorcise. After all, even within our planet, each geosphere reacts to cosmic influences in its own way, and has its own geological time scale. The change of seasons, day and night plays a significant role in the life of the atmosphere and hydrosphere. It is reflected in the seasonal stratification of precipitation, in the periodic change of temperatures, air pressure, etc. It is quite appropriate to use the standards we are familiar with — clocks. The "micro clocks" of atomic physics, counting down millionths and billionths of seconds, are pointless to use — otherwise the atmosphere will appear unchanged, "crystal" (imagine what it would look like for space aliens living — on our scale — fractions of a second). The atmosphere also reveals peculiar qualities on the scale of centuries and millennia. Here we are already forced to neglect daily and even seasonal changes, and we notice, as a rule, only age-old deviations from the "norm". Diurnal fluctuations in physical properties (temperature, humidity, density) are observed only to a depth of several meters from the Earth's surface.
Seasonal fluctuations penetrate deeper, while secular fluctuations can reach a depth of six hundred meters (this can be observed by the thickness of the permafrost). The life of the planet's interior deeper than one kilometer is practically not affected by the uniform revolutions of the Earth around the axis and the Sun (excluding phenomena related to Coriolis forces). It is possible to measure the life of the earth's interior with the help of astronomical clocks only conditionally, because here geological processes are very slow, and what corresponds to a year in the atmosphere is more fleeting than a minute. We arbitrarily, for no objective reason, raise a certain measure (a year, for example) to the rank of an "absolute time interval." We might as well proclaim a friend to be the lord of the planets and the lord of the galaxies. The special duration and length of geological time intervals cannot be reduced to a simple sum of smaller intervals. Actually, purely arithmetically, we can take the Decamiriad as a set of one hundred centuries, and, say, the geochron as a million years, the megachron as a hundred million years, etc. But in their geological essence, as applied to real geological processes, these intervals are extraordinary. During these periods, events occur in the life of the Earth that in no way occur in our usual, mundane time intervals (minutes, hours, years). In other words, the properties of geological objects vary depending on the accepted time scale. The Aviator online game brings the fun of the casino to your fingertips. Try the aviator online game and enjoy the thrill of winning big.