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The valley expands and the Ebro's flow then becomes slower as its water volume increases, flowing across Aragon. There, larger tributaries flowing from the central Pyrenees and the Iberian System discharge large amounts of water, especially in spring during the thawing season of the mountain snow.
North of the river there is the Sierra de Alcubierre ranges (811 m) one of the typical limestone plateaus of the valley. The Ebro Valley is a tectonic pit filled with sedimentary materials, accumulated in the Tertiary age in horizontal series. In the center, fine materials such as clays, plasters and limestones were deposited.
Map of the Ebro valley Source of the Ebro in Fontibre The middle Ebro in Zaragoza Final section, in Miravet Floods of 2003, in Novillas (). In 1913, the First National Irrigation Congress was held in Zaragoza, exposing the idea of setting up a community group of an economic and supra-regional nature through the federation of the agricultural, commercial and industrial associations of the whole ...
The Romans carried out various divisions of the peninsula throughout the history of their Empire: Division of 197 B.C. (its limits were not precise, since only the coastline was dominated): Hispania Citerior: Ebro Valley and Mediterranean coast. Hispania Ulterior: Guadalquivir Valley.
In the past many water-mills were powered by the river, but now only ruins of these remain. The valley of the Jiloca is an ancient route between the Meseta Central, the Ebro and the coast of the Levante. Many Roman bridges remain in the pueblos of the valley. [5] [15]
Campo de Belchite is a comarca in Aragon, Spain. It is located in Zaragoza Province, in the transitional area between the Iberian System and the Ebro Valley. The administrative capital is Belchite, the largest town in the comarca. Some municipal terms of Campo de Belchite are part of the historical region of Lower Aragon.
The term "Aiguabarreig" comes from the Catalan word that designates the mixture of waters in the place where two or more streams of water meet and form one. The Aiguabarreig Segre-Cinca-Ebro is formed at the time that the Cinca river brings its water to the Segre river, in the municipal area of La Granja d'Escarp, and then they arrive to the Ebro river, already in Mequinenza.
Bajo Martín is a comarca in Aragon. It is part of the historical region of Lower Aragon. It is located in Teruel Province, in the transitional area between the Iberian System and the Ebro Valley. It borders the Aragonese comarcas of Ribera Baja del Ebro, Campo de Belchite, Cuencas Mineras, Andorra-Sierra de Arcos, Bajo Aragón and Bajo Aragón ...