Bohemia sits on and in a lump. If the story of Hungary was written by the Danube Basin, the huge sub-surface sink that gradually filled with sediment until it became a broad, flat, water-logged grassland, then the story of Bohemia started with the rise of a lumpy plateau, the Bohemian Massif.
It’s not exactly a plateau, but four chunks of folded, faulted, uplifted, and generally mangled rock that started shifting and rising during the Variscan Orogony – the same episode that led to the creation of the Vosges in France. Two other continents collided, and what became Bohemia was one of the lumps caught in the middle as Pangea formed. All that pushing at the edges led to the compressional faulting and folding that shoved the Bohemian Massif upward, in some places over 10,000 feet. Continue reading