venerdì 23 dicembre 2011

mercoledì 21 dicembre 2011

Po River Sunset - Lido Po, Guastalla (RE) - September 29, 2011

From Wikipedia:

The Po (Latin: Padus and Eridanus, Italian: Po [ˈpɔ], ancient Ligurian: Bodincus or Bodencus, Greek: Πάδος and Ἠριδανός) is a river that flows either 652 km (405 mi) or 682 km (424 mi) – considering the length of the Maira, a right bank tributary – eastward across northern Italy, from a spring seeping from a stony hillside at Pian del Re, a flat place at the head of the Val Po under the northwest face of Monviso (in the Cottian Alps) through a delta projecting into the Adriatic Sea near Venice. It has a drainage area of 74,000 km² in all, 70,000 in Italy, of which 41,000 is in montane environments and 29,000 on the plain.[2] The Po is the longest river in Italy; at its widest point its width is 503 m (1,650 ft).[1] The Po extends along the 45th parallel north.
The river flows through many important Italian cities, including Turin (Torino), Piacenza and Ferrara. It is connected to Milan through a net of channels called navigli, which Leonardo da Vinci helped design. Near the end of its course, it creates a wide delta (with hundreds of small channels and five main ones, called Po di Maestra, Po della Pila, Po delle Tolle, Po di Gnocca and Po di Goro) at the southern part of which is Comacchio, an area famous for eels. The Po valley was the territory of the Roman Cisalpine Gaul, divided in Cispadane Gaul (South of the Po) and Transpadane Gaul (North of the Po).
The river is subject to heavy flooding. Consequently over half its length is controlled with argini, or dikes.[1] The slope of the valley decreases from 0.35% in the west to 0.14% in the east, a low gradient. There are 450 standing lakes.[2]

martedì 13 dicembre 2011

Jogger - Fellegara (RE) - December 4, 2011

Where the Canalazzo Torrent meets the Crostolo Torrent - Santa Vittoria, Gualtieri (RE) - September 29,2011

Pietra di Bismantova - Castelnovo ne' Monti (RE) - November 13, 2011

From Wikipedia:

he Pietra di Bismantova is a geological formation in the Reggiano Apennines, in the comune of Castelnovo ne' Monti, province of Reggio Emilia, central Italy, c. 45 km from Reggio Emilia. It has the shape of a narrow, quasi-cylindrical plateau (measuring 1 km x 240 m) whose steep walls emerge c. 300 m as an isolated spur from the nearby hills. The top has an altitude of 1,047 m over the sea level. It is included in the National Park of the Appennino Tosco-Emiliano.
The spur is composed of yellowish calcarenite over a marl basement, all formed in the Miocene as a sea bottom. It includes fossils belonging to a tropical environment. It is surrounded by woods, mostly of oaks.
The Pietra di Bismantova is mentioned by Dante Alighieri in his Divine Comedy (Purgatory, IV, 25-30).

mercoledì 26 ottobre 2011

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