Pietra Alta
The Pietra Alta (in piedmontese: "Pera Aota" or "Peraota", meaning "High Stone") is a glacial erratic in the comune of Caselette (TO, Italy), relevant for its size and its isolated location. Features. The erratic is a massive boulder with a pyramidal shape, emerging some 10 metres from the ground level and with a circumference of about 50 metres. Its elevation is 368 MSL. It stands in a woody and almost plain spot close to the border between Caselette and Alpignano, not faraway from the small Lake of Caselette. The place is still of a good environmental quality, although  almost encircled by industrial and residential areas. Geology. The Pietra Alta belongs to the "Morainic amphitheater of Rivoli-Avigliana", and in particular to the moraine left by the Riss glaciation. It was transported to its present location by the hudge glacier which occupied the Susa Valley. Its height on the ground level, remarkable if compared to other glacial erratics of Piedmont, can be explained because the Pietra Alta, unlikely other boulders mostly covered by the gound, is almost fully exposed. It consists in an huge block of serpentinite with a volume of 2.600 cubic metres. On its surface can be  detected rinds similar to the so-called "desert varnishes", considered by geologist an indicator of a . Uses. On the boulder there are a lot of climbing routes, and its sides are equipped with bolts and pitons in order to protect the climbers. Many of these routes, some of them very engaging, were described at the beginning of the 1980s by the alpinist Gian Carlo Grassi in his book "Sassismo spazio per la fantasia: arrampicate sui massi erratici della Valle di Susa". The environment surrounding the Pietra Alta is considered very suggestive; the boulder can be easily reached on foot from  Caselette following "Via Pietra Alta", a small asphalted lane which continues with a pedestrian dirt road.