빌라마요르 데 칼라트라바‬에서 가장 멋진 ‪9‬개의 천연기념물

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.

The Fuente Agria is one of the most emblematic icons of Puertollano. Located on the Paseo de San Gregorio, this fountain is known for its water with a high iron content, which gives it a characteristic flavor and health benefits.

Puente Morena is a prominent place on the Jabalón River, in the province of Ciudad Real. It is known for its hydrological monitoring station, which is part of the Guadiana River basin. This station collects important data on water flow and other hydrological parameters. Additionally, Puente Morena is significant for its geological characteristics. It offers a classic Upper Ordovician stratigraphic section, showing three different units: Mixed Banks, Urban Limestone and Chavera Slates2. This makes it an interesting site for geological and paleontological studies.🌄🚴😎

The Moreno fountain

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.

The path that passes by the Río Guadiana lets us see this area where a dam has been built and which can be a good time to take a short break!