Supervergence

Supervergence: what is it and how does it relate to turning?

Supervergence is a term that describes the process of rotation around an axis that occurs as a result of the influence of external forces on the body. The term comes from the Latin word "vergo", which means "to turn", and the prefix "supra-" is added to denote what happens above and beyond the normal sphere of influence.

In the context of science, supervergence can be applied to a variety of objects, including aerodynamic bodies, spacecraft, and other objects that can move in space. It is important to note that supervergence is not only the result of mechanical forces, but can also be caused by effects such as gravity and the rotation of the Earth.

Supervergence has significant implications in the field of aerodynamics. For example, during airplane flight, supervergence can occur when the airplane's wings create lift, which turns the airplane around its longitudinal axis. This effect can be used to control an aircraft and change its course.

In the space industry, supervergence is also of great importance. For example, when launching a spacecraft, supervergence may occur due to the rotation of the Earth around its axis. This effect can affect the flight path and requires special calculations when planning missions.

In conclusion, supervergence is an important physical effect that can occur in various fields of science and technology. Understanding this effect is important for controlling the movement of objects in space and can be used to create more efficient technologies and systems.

Supervergency (fusion, zygogenesis, suprazonality). Otter in 1960 proposed the following characteristic of it: “supra-vergent shell.” Considerable factual material has been accumulated that makes it possible to classify synclines or monoclines into different tectonic styles. Undoubtedly, it is supergency, together with orthovergence (vertical orientation of boundaries), that forms the random eventability of rifts and forms the entire system of modern processes of oceanization of the earth's crust. In subduction structures during the same events, the formation of a rift structure mainly occurs according to an orthomergent scheme. For many mining operations, this means that ore bodies are likely to be localized along long meridional depressions. Therefore, in many hydrothermal deposits, it is the central part, the fusion zone, that turns out to be industrially productive.