rétégezésnek

Rétégezésnek is a small, relatively unknown geological formation located in the eastern Carpathian Mountains. Its name, derived from an Old Hungarian word meaning "layered stone," accurately describes its most prominent characteristic: distinct, horizontal strata of sedimentary rock. These layers are primarily composed of sandstone and shale, with occasional thin seams of limestone.

The formation is thought to have been created during the Neogene period through a process of sedimentation in a shallow, ancient sea. Over millions of years, tectonic uplift and erosion have exposed these layers, creating a visually striking landscape. The coloration of the rock varies across the formation, ranging from pale yellows and grays in the sandstone to darker browns and greens in the shale, a result of differing mineral content and oxidation.

While Rétégezésnek lacks significant paleontological discoveries, its geological structure offers valuable insights into the region's past environmental conditions. The consistent layering suggests periods of stable deposition, interrupted by occasional shifts in sediment type. Access to Rétégezésnek is limited, with no established tourist trails or infrastructure, making it a site primarily of interest to geologists and local researchers. Its remote location and rugged terrain contribute to its undisturbed state.