Sedimenttivyöhykkeet
Sedimenttivyöhykkeet refers to the distinct zones or layers formed by sedimentary processes in geological formations. These zones are characterized by variations in grain size, composition, color, and depositional structures, reflecting changes in the environment and conditions during sediment accumulation. Understanding sedimenttivyöhykkeet is crucial for interpreting past geological events, such as sea-level changes, climate shifts, and tectonic activity.
In marine environments, sedimenttivyöhykkeet can be observed from the shoreline to the deep ocean. Near the
Terrestrial environments also exhibit distinct sedimenttivyöhykkeet. For instance, river systems can show changes in sediment size
The study of these sedimentary zones involves analyzing rock cores, outcrops, and geophysical data. By examining