Cima Tosa

Mountain

Cima Tosa 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 reported height of 3,136 metres (10,289 ft). it is the second highest peak of the Brenta group in the southern limestone Alps after the Cima Brenta. The height of the summit marked on the IGM maps is 3,173 m, which would make it the highest peak in the Brenta Dolomites.

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Cima Tosa

Mountain

Texto em inglês

Cima Tosa 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 reported height of 3,136 metres (10,289 ft). it is the second highest peak of the Brenta group in the southern limestone Alps after the Cima Brenta. The height of the summit marked on the IGM maps is 3,173 m, which would make it the highest peak in the Brenta Dolomites.

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Texto em inglês Ainda não há artigo no seu idioma: trecho em inglês.

Cima Tosa 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 reported height of 3,136 metres (10,289 ft). it is the second highest peak of the Brenta group in the southern limestone Alps after the Cima Brenta. The height of the summit marked on the IGM maps is 3,173 m, which would make it the highest peak in the Brenta Dolomites. An electronic measurement campaign in 2015 determined the new height. The change could be linked to the partial melting of the ice cap that covers it. Being the second highest peak of the Brenta group also changed Cima Tosa's prominence making its prominence 589 m above the Bocca di Brenta. The mountain rises above Val Rendena with its 800-metre (2,600 ft) vertical north face with a steep couloir called Canalone della Tosa dividing it from its ante-peak, Crozzon di Brenta. The summit is topped by a snow cupola above the rock face, almost like a shaven head, hence the name Cima Tosa (Iocal dialect: Shaven Summit). The south-eastern side descends in a series of snowy terraces and vertical rock pillars.

Texto: Wikipédia em inglês, CC BY-SA 4.0. · Imagem: Glysiak (CC BY-SA 4.0) ·

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