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Titlebook: Geomorphology of Europe; Clifford Embleton Textbook 1984Latest edition Palgrave Macmillan, a division of Macmillan Publishers Limited 1984

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Baetic Cordillera and Guadalquivir Basin, Cabo de la Nao (. Fig. 13.1). In its north-eastern part, it merges with the Iberian Cordillera while to the north and north-west it is separated from the Hercynian block by a triangular depression drained by the Guadalquivir. The Balearic Islands mark its prolongation to the east and, past Gibralta
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The Appennines and Sicily,s from which it is difficult to separate exactly and without question. At the other extremity, the chain extends to Sicily—the largest Italian island—separated from the mainland by the Strait of Messina (3–5 km wide).
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Caucasus Mountains and Armenian Highlands, the Scythian platform (Hercynian) and the Arabian platform (Precambrian). The Great Caucasus forms the outer ridges of the Alpine orogenic system, while the Armenian highlands form an inner sector, comprising typical block, folded-block and folded systems of ridges, extensive uplands with bevelled
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Ural Mountains,s, it is a unique mountain system, not just for Europe but in the context of the whole of Eurasia. The main structural forms are elongated and divided by parallel deep-seated faults. Transverse faults, located by geophysical surveys and also expressed in the relief [see Yanshin (1966), Ogarinov (197
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Hercynian Europe,ian massifs are often referred to as the Mittelgebirge, meaning literally ‘middle mountains’, because they attain only moderate heights compared with the higher Alpine and Carpathian chains to the south.
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Structural and Tectonic Framework of the Continent of Europe,ndent guide to the geomorphology of Europe, this book also aims to complement and explain the ., published in 16 sheets on a scale of 1: 2.5 million. Reference to individual sheets of the Map is made in this book; an understanding of the features depicted on the Map will be facilitated by consulting the relevant sections.
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