Töréssáv

Töréssáv is a Hungarian term that translates to "fracture zone" or "fault zone" in English. It refers to a region of the Earth's crust where rocks have been broken and displaced due to tectonic forces. These zones are characterized by the presence of faults, which are planes of fracture where movement has occurred. The rocks within a töréssáv can be significantly deformed, crushed, and altered.

Töréssávok are often associated with seismic activity, as the movement along faults releases energy in the form of earthquakes. The width and complexity of a töréssáv can vary greatly, depending on the geological setting and the magnitude of the tectonic forces involved. Some töréssávok are narrow and linear, while others can be broad and intricate systems of intersecting faults.

The study of töréssávok is crucial in understanding the Earth's geological history, plate tectonics, and the potential hazards associated with earthquakes. Geologists map and analyze these zones to identify areas at risk and to study the processes that shape the Earth's surface. In some instances, töréssávok can also influence the flow of groundwater and the distribution of mineral deposits. The term is primarily used in geological contexts within Hungary and in Hungarian scientific literature.