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Reno (river)

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Parent: Adriatic Sea Hop 4
Expansion Funnel Raw 61 → Dedup 0 → NER 0 → Enqueued 0
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Reno (river)
NameReno
CaptionThe Reno near Porretta Terme
Source1 locationTuscan-Emilian Apennines, Tuscany, Italy
Mouth locationAdriatic Sea near Casalborsetti, Ravenna
Length211.8 km
Basin size5040 km2
Discharge1 avg95 m3/s
Tributaries leftSilla, Limentra di Treppio, Limentra di Sambuca, Setta, Idice, Sillaro, Santerno
Tributaries rightVergatello, Leo

Reno (river). The Reno is a major river of northern Italy, flowing from the Tuscan-Emilian Apennines across the Emilia-Romagna region to the Adriatic Sea. With a length of approximately 212 kilometers, it is the longest river originating within the Apennines and the tenth-longest in Italy by total length. Its significant basin and historical role in regional hydropower and agriculture have made it a vital geographical feature of the Po Valley plain.

Geography and Course

The Reno originates on the southern slopes of Monte le Piastre in the Province of Pistoia, within the Tuscany region. It initially flows northward through a deep valley, passing towns like Pracchia and Porretta Terme, known for its thermal springs. Near the historic town of Bologna, the river emerges onto the vast alluvial plain of the Po Valley, where its course becomes wider and more meandering. It finally discharges into the Adriatic Sea between the Lidi di Comacchio and the port of Ravenna, near the locality of Casalborsetti. The river's lower course has been heavily modified by human intervention, including significant diversion works completed in the 18th century under the Papal States to prevent its waters from merging with the Po.

Hydrology and Basin

The Reno drains a basin of over 5,000 square kilometers, encompassing parts of the Metropolitan City of Bologna, the Province of Ravenna, and the Province of Forlì-Cesena. Its flow regime is characterized by strong seasonal variations, with high discharges in autumn and spring due to Apennine rainfall and snowmelt, and notably lower flows in summer. The average discharge at its mouth is about 95 cubic meters per second. Major regulation works, including the Suviana and Brasimone reservoirs on its tributaries, were constructed in the 20th century for hydropower generation and flood control. The river's sediment load has historically contributed to the progradation of the Ravenna coastline.

History and Human Use

Historically, the Reno's lower reaches were part of a complex deltaic system with the Po and Santerno rivers, creating vast marshlands. During the Roman Empire, the area was managed via the Via Aemilia and drainage canals. Major hydraulic engineering began in the Renaissance, with projects by Leonardo da Vinci and others, but the pivotal intervention was the "Cavo Benedettino" diversion channel completed in 1767 under Pope Clement XIII, permanently separating the Reno from the Po. The river's energy powered numerous mills and, later, early industrial activities in Bologna. Its waters have long been used for irrigation across the fertile Emilia-Romagna countryside, supporting crops like wheat, fruit trees, and sugar beet.

Ecology and Environment

The Reno's upper course flows through protected areas within the Apennines, featuring mixed forests of beech and chestnut. The middle and lower riverine environments have been significantly altered by channelization and agriculture, though residual stretches of riparian forest with poplar and willow remain. The river mouth and adjacent wetlands, part of the Po Delta system, are ecologically important for migratory birds and are included within the Po Delta Regional Park. Environmental concerns include water abstraction for irrigation, reducing summer flows, and historical pollution from agricultural and industrial sources, though water quality has improved in recent decades due to European Union directives like the Water Framework Directive.

Tributaries and Settlements

The major left-bank tributaries, which drain the larger, mountainous part of the basin, include the Silla, Limentra di Treppio, Limentra di Sambuca, Setta, Idice, Sillaro, and the significant Santerno. Right-bank tributaries like the Vergatello and Leo are shorter. Important cities and towns along its course include Porretta Terme, Marzabotto (site of the ancient Etruscan city of Kainua), Sasso Marconi, and the outskirts of the major urban center of Bologna. In the lowlands, the river passes near Molinella and Argenta before reaching the coast near Ravenna, a city famed for its Byzantine mosaics and UNESCO World Heritage sites.

Category:Rivers of Italy Category:Rivers of Emilia-Romagna Category:Rivers of Tuscany Category:Geography of the Province of Bologna