The height of the Cansiglio plateau above sea level is more than . that rises to a maximum height of above sea level and includes rocky peaks such as Monte Costa, the Cima Valsotta,
Monte Millifret,
Pizzoc and the Monte Cavallo. These mountains separate the Cansiglio from the short
Val Lapisina valley. The outcropping rocks date from the
Late Jurassic to the
Paleocene. The plateau has a limestone soil and features several examples of karst topography which produces depressions and gorges as well as
limestone pavements,
sinkholes and residual
conical hills. There are over 250 caves in the area, the most famous being the
Bus de la Lum,
Bus della Genziana and
Abisso del Col della Rizza. Their depths are , and respectively. The area also contains several
ponors. Being in what is in effect a depression, the plateau traps cold air, resulting in increased humidity and a climate that is 2° colder than comparable areas at the same altitude. Most of the territory of Cansiglio is covered by woods, mostly local
beech, although there are also non-native
coniferous trees such as the
European spruce. Due to the climatic characteristics of the plateau, the vegetation follows a more inverted distribution than usual: species typical of colder environments occupy the lower altitudes, and those typical of milder ones are at higher altitudes.
Anemones grow in large number under the beeches in summer. Large open spaces are used as pastures for
sheep and
cattle. The area is at medium-high
seismic risk, with earthquakes having occurred in 1936 and 1976. ==History==