inklináció

Inklináció is a Hungarian term that denotes tilt, angular deviation, or a general tendency. It derives from the Latin inclinatio, meaning leaning, and is used across disciplines to describe how far something deviates from a reference plane or direction, or, more broadly, a predisposition.

In geology, inklináció specifically refers to the tilt of rock layers, i.e., the dip angle relative to the horizontal, with the dip direction indicating the compass bearing toward which the layer tilts. Measurements are taken with clinometers or geological compasses and are essential for mapping fractures, folds, and other structural features.

In astronomy and celestial mechanics, inklináció denotes the angle between an object's orbital plane and a reference plane such as the ecliptic or celestial equator. Small inclinations imply orbits near the reference plane; large inclinations indicate highly inclined orbits. Examples include Earth's orbit around the Sun relative to the celestial equator (about 23.4 degrees) and the Moon's orbit relative to the ecliptic (about 5.1 degrees).

In other contexts, inklináció can describe a general tendency or predisposition, such as an inclination to favor certain activities or opinions. In engineering, devices measure inclination with sensors such as inclinometers or clinometers to monitor tilt in structures, vehicles, or machinery.

Overall, inklináció is a versatile term describing angular deviation from a reference frame and, by extension, a tendency in broader usage. Its precise meaning depends on the field of study.