Events, exhibitions, shows and entertainment activities may be postponed or even cancelled.
Given the ever-changing situation, we would advise you to always check opening times in advance as well as any restrictions applying to the event directly with the contact people indicated.
We do our best to keep you constantly updated but apologise for any inconvenience caused.
From Brè to Mount Boglia and then to Alpe Bolla, the subsoil is composed of siliceous calcareous rocks and dolomite of the Lower Jurassic. In the area of Denti della Vecchia a more ancient layer comes to the surface: that of the Upper Triassic, which is mainly constituted of dolmitic rock. Between Denti della Vecchia and the Pairolo Mountain Hut there are some “verrucan conglomerates”, which are even more ancient. The Gazzirola Massif is constituted by a crystalline base, made out of gneiss, that represents the most ancient outcrops of the Sottoceneri area.
On the valley floor of Val Colla there are rocks covered in sand, gravel and clays of ice age origin (ancient moraines).
The information on this site, concerning services or products is provided by external partners. This Information is liable to change frequently; for this reason Lugano Region cannot be held liable for any inaccuracies.