Los paisajes de la región de Milmarcos: sistemática y cartografía (Cordillera Ibérica, Provincias de Guadalajara, Soria y Zaragoza)
- A. García-Quintana
- J.A. González Martín
- J.F. Martín-Duque
- J.F. García-Hidalgo
ISSN: 1576-5172
Argitalpen urtea: 2000
Zenbakien izenburua: V Congreso Geológico de España (Alicante, 10-14 julio 2000)
Zenbakia: 1
Orrialdeak: 249-254
Mota: Artikulua
Beste argitalpen batzuk: Geotemas (Madrid)
Laburpena
Landforms constitute the physical framework of the landscape, whether it is considered in a territorial or in a visual approach. The composition, tectonic structure and geologic history of a territory determine the topographic development of the landscape and its textures. Here, we summarize the study o f the landscape's structure of a region o f 600 km2 located in the centre of the Iberian Peninsula, characterised by an alternance o f rock strata with different consistency and erosionability. The Mesozoic materials are folded and faulted because o f the alpine movements, and flattened to Neogene planation surfaces. The Cenozoic materials are in a horizontal disposal. During the Quaternary, the river system of the Mesa River was incised and developed. As a consequence of these circumstances, a wide variety of landforms is displayed. A typological classification o f the structures o f the landscapes of this region and their mapping has been made.