varundusprotsesse
Varundusprotsesse refers to the processes involved in the formation and activity of sandstone varuni-tectonic structures. Also known as raggi-sintiektenic lines, these features are found in eolian sandstones. They resemble fossilized riverbeds and involve reworking of pre-existing layers by water.
The development of varundusprotsesse involves the repetitive action of water as the main driving force. Pockets
Additionally, the interconnected network of fluid flow systems around the sandstone bed breathes life to these
The formation of varundusprotsesse could be interpreted as indicative of hydrodynamic scenario, explaining roughly topological/eearly modification