Inner Western Carpathians

The Inner Western Carpathians are a distinct geological and geographical region within the larger Carpathian mountain system in Europe. This area is characterized by a complex structure, featuring older crystalline and metamorphic cores overlaid with younger sedimentary rocks, primarily limestones and dolomites from the Mesozoic Era. Volcanic activity has also played a significant role, with younger volcanic rocks forming prominent features.1

The Inner Western Carpathians are further divided into separate blocks, including the Central Slovakian Block. These blocks are often dissected by smaller basins filled with Cenozoic rocks. The region's relief has largely developed during the Cenozoic Era, with evidence of older landforms and deeply incised valleys. While the last Ice Age affected the highest parts, glaciers were relatively small.1