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The Po Valley, Po Plain, Plain of the Po, or Padan Plain (Italian: Pianura Padana [pjaˈnuːra paˈdaːna] or Val Padana) is a major geographical feature of northern Italy. It extends approximately 650 km (400 mi) in an east-west direction, with an area of 46,000 km 2 (18,000 square miles) including its Venetic extension not actually related to ...
The Po has a drainage area of 74,000 km 2 in all, 70,000 of those being in Italy, of which 41,000 is in montane environments and 29,000 on the plain. [2] The slope of the Po's river valley decreases from 0.35% in the west to 0.14% in the east, a low gradient.
The Po Valley is the largest plain in Italy, with 46,000 km 2 (18,000 sq mi), and it represents over 70% of the total plain area in the country. [17] The Po Valley is divided into two bands: [22] the high plain, which borders the Alpine and Apennine hills, and the low plain located in the center and extended up to the Po delta.
The valley gives rise to the longest river in Italy, the Po, before it enters the Pianura Padana (or the Plain of the Po). It has a length of some 32 km, from Saluzzo to Crissolo, and is home to the Monviso mountain. It is bounded by the Val Pellice, Valle Varaita and the Valle del Guil.
The Po River, the longest river in Italy, flows over 650 km from west to east across the country, and ends at a delta projecting into the Adriatic Sea near Venice. The river flows through some of Italy’s important cities of the north. On the very left of the image, next to the river, the city of Turin can be seen.
Padania (/ p ə ˈ d eɪ n i ə / pə-DAY-nee-ə, UK also /-ˈ d ɑː n-/- DAH-, [1] Italian: [paˈdaːnja]) is an alternative name and proposed independent state encompassing Northern Italy, derived from the name of the Po River (Latin Padus), whose basin includes much of the region, centered on the Po Valley (Pianura Padana), the major plain of Northern Italy.
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The key evidence of the difference is the geologic behavior of the Po Valley in northern Italy. Compressional forces have been acting from north to south in the Alps and from south to north in the Apennines, but instead of being squeezed into mountains the valley has been subsiding at 1 to 4 mm (0.16 in) per year since about 25 mya , before the ...