Hydrography

Charca de Las Escarbajas

The Charca de Las Escarbajas is situated approximately halfway between Mieza and Vilvestre. This modest water pool is situated within the remarkable territory of Las Arribes del Duero. It is one of numerous water accumulation formations within this territory, which are significant for the local ecosystem.

It is of interest to ascertain the reason behind the formation of these ponds. The formation of the area is largely influenced by the geological characteristics of Charca de Las Escarbajas, which is characterised by a gentle and hilly topography, as well as the presence of granite bedrock. These materials have a low permeability, which results in the accumulation of surface water in specific areas during the rainiest seasons.

As previously stated, ponds are of significant ecological importance, as they serve as vital habitats for numerous species. They are of particular significance for amphibians, which are experiencing a progressive decline in their populations. Charca Las Escarbajas serves as a biological refuge for these creatures due to their significant dependence on the bodies of water that facilitate their life cycles.

These small oases, situated in an area of considerable ecological value, also serve other species, particularly birds, which act as a watering hole and an ideal feeding ground. These areas facilitate the reproduction of a wide variety of insects that constitute a significant proportion of the local fauna. Furthermore, Charca de Las Escarbajas is situated amidst a landscape of holm oaks and cork oaks, within a vast expanse of meadowland that serves as pasture for livestock.