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Alto Tajo · 19 places

River sources, lagoons and rivers of Alto Tajo

Alto Tajo’s water usually emerges from rock: karst springs, river sources and aquifer-fed lagoons. Local rivers therefore retain cold, clear water in summer. Highlights include tufa-dammed Taravilla Lagoon, salty La Salobreja and the Cuervo’s source.

Beneath Alto Tajo lies an invisible second landscape: passages and cavities carrying water. It emerges in springs and river sources, sometimes spectacularly, feeding lagoons and rivers.

Types of water you will see

Explore Rivers and catchments to understand their relationships. The Tagus, Gallo and Hoz Seca link Albarracín’s headwaters with Molina and the canyon; Arandilla, Bullones and Salado trace smaller branches and their memories.

  • River sources and springs, where rivers emerge from rock.
  • Tufa lagoons, dammed by rock barriers built by water itself.
  • Salt lagoons, rare in the mountains, associated with salt-bearing rocks.
  • Rivers such as the Tagus, Gallo, Cabrillas and Hoz Seca.

Traces to keep reading

These places connect the theme with the territory’s stories. Choose a trace and open its page to follow the story.

This landscape through layers of time

The places in this theme preserve traces of these eras. A single place can appear in several.

All places (19)

Water source

Setiles lagoon or Laguna de los Majanos

Water source

Source of the Escabas River (Serranía de Cuenca)

Water source

Presa de la Rocha or Campillo Dam (Zaorejas)

Zaorejas
Water source

Laguna de Taravilla: an 11,000-year-old natural tufa dam

Taravilla
Water source

Laguna de la Salobreja (Orea): a saltwater lagoon in the mountains

Orea
Water source

Nacimiento del Río Cuervo: tufa waterfalls in Vega del Codorno

Vega del Codorno
Water source

Source of the Tagus River and its monument (Montes Universales)

Frías de Albarracín
Water source

Las Juntas of the Tagus and Hoz Seca: where the Tajillo becomes the Tagus

Checa, Peralejos de las Truchas
Water source

Tordesilos lagoon: birds on the eastern boundary

Tordesilos
Water source

Pozo del Soto (Villanueva de Alcorón): a mine that became a lake

Villanueva de Alcorón
Water source

Source of the Guadiela River (Cueva del Hierro)

Cueva del Hierro
Water source

Hoz Seca or Oceseca River: the cold heart of the Park

Canyon

Tajuña Valley in Torrecuadrada: Protected Karstic Canyons

Torrecuadradilla
Water source

Laguna Grande de El Tobar (Beteta): a lake with saltwater at the bottom

Beteta
Water source

Lagoons of La Yunta: cranes and steppe birds near Gallocanta

La Yunta
Water source

Lagoons of Tortuera: the wetland trail of the high plateau

Tortuera
Canyon

Pozo Galeano (Villel de Mesa): gorge and waterfall of the Mesa River

Villel de Mesa
Canyon

Tajuña gorges: 11 km of river between Anguita and Luzón

Anguita
Water source

Lagunas y parameras del Señorío de Molina: Natura 2000 wetland plains

Tortuera

Frequently asked questions

Why do Alto Tajo’s rivers flow in summer?

Karst acts like an enormous sponge: rain infiltrates limestone and emerges gradually all year through springs.