Guillermo Cobos Campos/Fototeca CENEAM
Until the 1970s, the lower section of the Arga River, near its confluence with the Aragón, meandered through a wide floodplain, with intense fluvial dynamics. At the time, it was deemed necessary to carry out works to contain the river's floods, leading to its rectification and channelling in the section from the town of Falces to the mouth of the Aragón River.
By the mid-1980s, it was observed that the channelling was insufficient, and the river overflowed during some floods. Additionally, the shortening of the new route increased the flow velocity, causing serious imbalances and damage in this area of significant ecological interest.
These phenomena have worsened in recent years, due, among other factors, to the effects of climate change.