The
geology of the Dachstein massif is dominated by the
Dachstein-Kalk Formation ("
Dachstein limestone"), dating from
Triassic times. In common with other karstic areas, the Dachstein is permeated by a rich
cave system, including some of the largest caves in Austria, such as the
Mammuthhöhle and the
Hirlatzhöhle. Another significant tourist destination is the
Eisriesenhöhle. The Dachstein is famous for its
fossils, including
megalodonts; the
Linzer Weg leads over many such fossils, which are referred to as
Kuhtritte ("cattle footprints"). Glaciers are uncommon in the Northern Limestone Alps, and those on the Dachstein — the
Hallstätter Gletscher ("
Hallstatt glacier"), the
Großer Gosaugletscher ("great
Gosau glacier") and the
Schladminger Gletscher ("
Schladming glacier") — are the largest, as well as being the northernmost and the easternmost in the whole of the
Alps. Several smaller ice-fields also exist, such as the
Kleine Gosaugletscher ("lesser Gosau glacier") and the
Schneelochgletscher ("snow-hole glacier"). The glaciers are retreating rapidly, and may disappear entirely within 80 years. The Hallstatt glacier withdrew by 20 m in the year 2003 alone. By 2018, it is estimated that the glacier has retreated more than 1 km since 1908. ==Climbing==