Titlebook: Landscapes and Landforms of Spain; Francisco Gutiérrez,Mateo Gutiérrez Book 2014 Springer Science+Business Media Dordrecht 2014 Conglomera

antiquated

起波瀾

妨礙議事

The Late Neogene to Quaternary Drainage Evolution of the Uplifted Neogene Sedimentary Basins of Alme last two became terrestrial in the early Pleistocene. The modern landscape reflects the influence of differential regional uplift rates on the long-term dissectional history, operating regionally over the whole period of landform development. The extremes are represented on the one hand by the dee

ORE

Atapuerca Karst and its Palaeoanthropological Sites,Accessible dry caves were used by fauna and hominids, preserving an exceptional archaeo-palaeontological record spanning from ~1.2?Myr until the end of the Middle Pleistocene. The sites of Elefante, Gran Dolina, Galería and Sima de los Huesos have provided exceptional findings for understanding the

脫離

CURB

The Gypsum Karst of Sorbas, Betic Chain,ms, some of them unique worldwide (e.g. gypsum balls, hollow stalagmites, gypsum trees and trays, and deflated stalagmites). The protection of the gypsum karst of Sorbas, due to the wide variety of surface and subsurface geomorphological features, should be considered of top priority for the adminis

Communal

Gallocanta Saline Lake, Iberian Chain,al environments. Lake segmentation due to cuspate foreland growth has divided the original lake into minor ones. Segmentation is still active at present and tends to isolate a minor lacustrine body. Progressively decreasing rainfall, together with sediment supply to the lake, enhanced by extensive a

粗糙濫制

,Playa-Lakes and Yardangs in the Bujaraloz-Sástago Endorheic Area, Central Ebro Basin, largest basins record alternating periods of aggradation and excavation, attributable to more humid and drier periods, respectively. The available radiocarbon dates from the most extensive terrace, allow us to infer deepening of the largest playa (La Playa) by wind erosion of 6?m over the last 2?ka

amenity

Block Streams in the Tremedal Massif, Central Iberian Chain,n by soft shales, display solifluction lobes and benches, suggesting that the formation of the streams is related to the progressive downhill displacement of the boulder deposits in the slopes. The block slopes and streams are relict landforms as the lichens covering the weathered surface of the bou

洞穴

Geology and Geomorphological Evolution of the Ebro River Delta,in response to wave-induced sedimentary dynamics. However, the construction of dams during the twentieth century has drastically changed the equilibrium responsible for the previous morphological evolution of the delta. Nowadays, after the drastic reduction in sediment supply to the delta, the wave-