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Los Arroturos (Muschelkalk outcrop), Paredes de Sigüenza, Guadalajara, Castile-La Mancha, Spaini
Regional Level Types
Los Arroturos (Muschelkalk outcrop)Mountain Area
Paredes de SigüenzaMunicipality
Castile-La ManchaAutonomous Community

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Latitude & Longitude (WGS84):
41° 13' 0'' North , 2° 44' 26'' West
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:

Right on the border between the municipalities of Tordelrábano and Paredes de Sigüenza is the Place of Geological Interest of Los Arroturos. It is an outcrop of Triassic limestones, of Muschelkalk facies, in which dinosaur footprints and other large organisms of the time (icnites) can be seen. Although the interest is more palaeontological and paleoclimatic, it is also possible to find fragments of fossilized bones in the area.

Justo en el límite entre los municipios de Tordelrábano y Paredes de Sigüenza se encuentra el Lugar de Interés Geológico de Los Arroturos. Se trata de un afloramiento de calizas Triásicas, de facies Muschelkalk, en las que se observan huellas (icnitas) de dinosaurios y otros organismos de gran tamaño de la época. Aunque el interés es más paleontológico y paleoclimático, también es posible encontrar por la zona fragmentos de huesos fosilizados.

List of minerals for each chemical element

External Links

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate

This page contains all mineral locality references listed on This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
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