laposabbak
Laposabbak is a term of Hungarian origin that translates to "flatter ones" or "more flattened ones." It is most commonly used in the context of geology and earth sciences to describe sedimentary rock layers that exhibit a less pronounced dip or inclination compared to surrounding formations. This can occur due to various geological processes such as differential erosion, subsequent deposition, or tectonic uplift that affects different areas unequally.
In practical geological surveying and mapping, identifying laposabbak layers is crucial for understanding the structural history
The term is not a formal scientific classification but rather a descriptive adjective used by geologists, particularly