vrstvité
Vrstvité is a term used in geology and soil science to describe a layered or stratified structure. It refers to the presence of distinct layers or strata within a rock formation, soil profile, or sedimentary deposit. These layers are typically formed by the deposition of different materials over time, or by variations in the physical or chemical conditions during their formation.
In sedimentary rocks, vrstvité structures are common and arise from successive deposition of sediments like sand,
In soil science, vrstvité refers to the distinct horizontal layers, or horizons, that develop in a soil
Vrstvité structures can also be observed in other geological contexts, such as in volcanic ash deposits or