deindustria, energÍa monfragüe biosphere reserve · z e p l a e d º r a canal ca nal cana l d e...
TRANSCRIPT
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Valrío
Valdencín
San Gil
Pradochano
Sartalejo
Avarientos
Fuentedel Sapo
Pajaresde la Rivera
Valderrosas
Viñuelas
Jarilladel Sur
BaldioVega
de Mesillas
Sta. Mªde las Lomas
Valdeíñigos
Urdimalas
La Bazagona
Pantanode Navabuena
Haza dela Concepción
Grimaldo
La Estación
Casasde Belvís
Valdemoreno
Retamosa
PalazueloEmpalme
Aldehuelade Jerte
Pedrosode Acim
Hinojal
Santiagodel Campo
Gargüera
Arroyomolinosde la Vera
Colladode la Vera
Serrejón
Millanes
Toril
Belvísde Monroy
Mesasde Ibor
Higuera
Romangordo
Casas deMiravete
Campillode Deleitosa
Valdecañasde Tajo
La Aldeadel Obispo
El Batán
Pueblade Argeme
Villarrealde San Carlos
Mirabel
Holguera
GalisteoAlagóndel Río
Talaván
Casasde Millán
Torrejónel Rubio
Torremenga
Tejedade Tiétar
Pasarónde la Vera
Saucedilla
Jaraicejo
Deleitosa
Riolobos
Carcaboso
Serradilla
Cañaveral
Monroy
Casatejada
Majadas
Almaraz
Torrecillasde la Tiesa
Casar deCáceres
Malpartidade Plasencia
Torrejoncillo
Talayuela
Jaraízde la Vera
Navalmoralde la Mata
Plasencia
Map: Geological routesMonfragüe Biosphere Reserve
0 102 4 6 8
Kilometers
DIPUTACIÓN DE CÁCERES
MINISTERIODE INDUSTRIA, ENERGÍAY TURISMO
GOBIERNODE ESPAÑA
National Park Border
Biosphere Reserve Border
Information
Interpretation CentresCI
Municipality Border
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w.la
ruin
agra
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com
Monfragüe route
Campana de Albalat route
Mineral route
Stops with geological interpretation0
Route starting point
Extremadura
Cáceres
Badajoz
2
1
43
5
6
7
8
9
12
1
2
35
4
CI
CI
CI
CI
CI
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at the Monfragüe
Biosphere Reserve
Geological routes
The relief which can be observed in Monfragüe is the result of a long geological history which dates back to the Paleozoic era, around 500 million years ago, when the entire area was covered by the sea.
The large landscape forms are in the shape of peaks and valleys, resulting in an appalachian type relief, with overhangs in the form of ridges. This succession of ridges and U-shaped valleys is intertwined with meadow vegeta-tion, with large expanses of holm oaks and cork oaks and Mediterranean undergrowth with thickets and heaths. Here we propose several different alternatives so that you can learn about this geology.
01 Monfragüe route
39,1 km(including the ascent
to the castle)
3 h and 20 min
4 h and 45 min
Scan the QR code and download the
track (KML) of the route to your
device
9 stops with geological
interpretation
Portilla del TiétarTorrejón el Rubio tourism office
Route profile Start Finish
This route, which starts at the tourism office of Torrejón el Rubio, has been designed to discover the geological a�ractions of the Monfragüe national park in a motor vehicle or by bike. The route's 9 stops with geological interpretation explain the different geological formations that can be found at the park: from the spectacular Armorican quartzite rocks of Peña Falcón, to the folds of Portilla del Tiétar; including the area's oldest shale, mining activity, the fossil record, the geomorphology of the park and much more.
The route covers the park's most
interesting spots in terms of
biodiversity
Disharmonic folds at Portilla del Tiétar
Scan the QR code and download the
track (KML) of the route to your
device
5 stops with geological
interpretation
Karst formations
Miravete Peak
Zincite crystals in La Norteña
3 h and 05 min
4 h and 30 min
Scan the QR code and download the
track (KML) of the route to your
device
2 stops with geological
interpretationArmorican quartzite
03campana
de albalatroute
mineralroute
An ideal route to discover the geological a�ractions of Campana de Albalat in a motor vehicle. This region is formed by the municipalities of Casas de Miravete, Romangordo and Higuera de Albalat. 5 designated stops starting at the Geology Interpretation Centre in Casas de Miravet, explaining the different geological formations that can be found in the area: karst phenomena in limestone, fluvial terraces in El Tajo, mining activity, rañas (glacis with stones), armorican quartzite and the appalachian relief.
Casas de MiraveteGeology Interpretation Centre in Casas de Miravete
Route profileStart Finish
An ideal route to discover the geological a�ractions of the mountain ranges of Santa Catalina, La Cueva and Los Canchos in a motor vehicle or by bike in the municipalities of Serradilla and Mirabel, eastern border of the synform of Monfragüe. This route, which has 2 stops with geological interpretation and starts at the Mark of Man Interpretation Centre, in Serradilla, enables visitors to discover the armorican quartz-ite of the Sierra de la Cueva, the appalachian relief, the chiastolite deposit next to the castle of Mirabel, etc.
34,1 km(including round trip to Sierra de la Cueva)
A visit to the Mark of Man Interpret.
Centre and the castle of Mirabel is
highly recom-mended
SerradillaMark of Man Interpretation Centre (Serradilla)
Route profileStart Finish
Vultures at Peña Falcón
Pedreras at the Sierra de Monfragüe
4 h and 30 min
Castle of Mirabel
Chiastolite
02
45,7 km(including the round trip to La Norteña)
You can complement the
route with a visit to the Geology
Interpret. Centre (Casas de Miravete)
The route passes by the
interesting Muslim site,
Makhada Al-Balat