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The Laguna Blanca in Argamasilla de Calatrava is an interesting natural formation. It was created by volcanic explosions that created depressions filled with rainwater1. This lagoon is known for the whitish colour of its waters, a result of the minerals present in the soil, such as bicarbonate and sodium sulphate. It is an excellent place for bird watching, as many species choose it as a stopover, resting or nesting point. In addition, the area around the lagoon has archaeological remains dating back to the Paleolithic, which adds historical value to the place.

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The “El Charcazo” recreational area in Corral de Calatrava is a lovely place to enjoy a day outdoors. It is located about 300 metres from the exit of the town towards Abenójar, on the CM-4112 road. This place is part of the Don Quixote Route and is of great volcanic, scenic, hiking and architectural interest. It has barbecues, picnic tables under the shade of holm oaks, and a small lake with ducks. It is ideal for bird watching thanks to its two large wetlands. Although it is a perfect place for a picnic or barbecue, it is important to remember that swimming in the reservoir is not permitted. In addition, there are toilets available and a fountain with non-potable water.

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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.

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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.

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Detour to El Charcazo Carretera CM-4112.

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Extinct Cañada de Calatrava lagoon next to the tunnel that crosses the A-41. It's better not to go if what you want is to see water.

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Extinct Cañada de Calatrava lagoon next to the CM-4115. Don't cayalis if you plan to see water.

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Great recreational area "EL CHARCAZO" in Corral de Calatrava, picnic, barbecue, swings, Hermitage of San Isidro, the pond, etc.

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