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Badacsony | Basalt organ
WI_hu510.jpg Badacsony | Basalt columnsThumbnailsBadacsonytördemic and Szent György-hegy

Badacsony (437 m) is the ruin of an ancient volcano. What remains is mainly the basaltic core. Contraction due to cooling and solidification of the lava has resulted in a system of joints separating column-like pieces of rock. Weathering, erosion, and rock falls have formed a landscape of individual columns and groups of columns (organs).

Saturday 8 June 2019 by Martin Mergili in Europe / Hungary (1296 visits)