Campanile Basso

Campanile Basso is a mountain in the Brenta group (It.: Dolomiti di Brenta), a subgroup of the Rhaetian Alps in the Italian Region of Trentino-Alto Adige, with a height of (2,883 metres (9,459 ft)). It is of a slender, almost fully vertical shape on all sides, rising 300 metres straight up. The mountain is named for its similarity in shape to a belltower (It.: campanile) and it being low (It.: basso) compared to the neighboring and . The German alpinist Karl Schulz introduced in 1884 the name Guglia di Brenta ("Guglia = "spire"), a name widely used until World War I and especially enduring in German literature, but considered inappropriate by locals and Italian climbers. Geologically, Campanile Basso is entirely formed of Triassic sedimentary rock, dense and compact dolomite. Due to its i

Campanile Basso

Campanile Basso is a mountain in the Brenta group (It.: Dolomiti di Brenta), a subgroup of the Rhaetian Alps in the Italian Region of Trentino-Alto Adige, with a height of (2,883 metres (9,459 ft)). It is of a slender, almost fully vertical shape on all sides, rising 300 metres straight up. The mountain is named for its similarity in shape to a belltower (It.: campanile) and it being low (It.: basso) compared to the neighboring and . The German alpinist Karl Schulz introduced in 1884 the name Guglia di Brenta ("Guglia = "spire"), a name widely used until World War I and especially enduring in German literature, but considered inappropriate by locals and Italian climbers. Geologically, Campanile Basso is entirely formed of Triassic sedimentary rock, dense and compact dolomite. Due to its i