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The Almodóvar del Campo Lagoon is a unique natural and geological feature located in the province of Ciudad Real, within the Campo de Calatrava region, famous for its volcanic landscapes. It is a lagoon formed in the crater of a volcano after a phreatomagmatic eruption (interaction between magma and groundwater). This type of lagoon is called a maar.

It is formed by a Strombolian volcanic cone of pyroclasts, and due to the quarry in it, its internal structure is exposed. Attached to the foot of this volcano is the Almodóvar maar, which is a phreatomagmatic explosion crater that erupted at the edge of the Paleozoic series, cutting a substrate of hard lithology and destroying part of the previous volcano. The maar crater is funnel-type (hard-type substrate) and houses an ephemeral lagoon inside. In its southern and eastern contour the maar has a ring of tuffs, with pyroclastic facies. The phreatomagmatic deposits of the maar ring are located on a Cenozoic red colluvium. The main interest is of a volcanological (petrological) type and as a secondary interest the geomorphological interest stands out.

It is formed by a Strombolian volcanic cone of pyroclasts, and due to the quarry in it, its internal structure is exposed. Attached to the foot of this volcano is the Almodóvar maar, which is a phreatomagmatic explosion crater that erupted at the edge of the Paleozoic series, cutting a substrate of hard lithology and destroying part of the previous volcano. The maar crater is funnel-type (hard-type substrate) and houses an ephemeral lagoon inside. In its southern and eastern contour the maar has a ring of tuffs, with pyroclastic facies. The phreatomagmatic deposits of the maar ring are located on a Cenozoic red colluvium. The main interest is of a volcanological (petrological) type and as a secondary interest the geomorphological interest stands out.

It is a volcanic formation made up of a crater and the Cerro de los Molinos. The crater gives rise to the lagoon and the hill is composed of solid lava. It is located near Almodóvar del Campo, in an easterly direction and, according to historians, it gave origin and name to the settlement of the population.

Lagoon that is located on the east side of the center of Almodóvar del Campo and that, depending on the time of year, is more or less full of water!

Cycling along the CR-501 road bordering the Pantano del Montoro. The concrete dam that contains the waters of the Montoro River is impressive.

Almodóvar del Campo Volcanic Lagoon is a seasonal lagoon of volcanic origin typical of the area. They are lagoons associated with phreatic and phreatomagmatic eruptions. The crater of the maar is of the funnel type.

This dam creates the Montorillo Reservoir which was built in 1950. It controls the Montoro River so local communities and businesses have a safe source of water year-round. It also creates a good habitat for different birds and fish. The area around the reservoir is rural and creates a great area for mountain biking.