|
The Catalan Mediterranean System, also known as Mediterranean System, Transversal Ibero-Pyrenaean System and Catalanid System〔Josep Guitart i Duran, Maria del Tura Bolòs et al. ''Història agrària dels Països Catalans (Volum 1) Antiguitat'', 2005, ISBN 978-84-475-2895-0〕is a wide coastal geographical region in Catalonia. It is made up of a double system of coastal mountain chains: The Catalan Coastal Range and the Catalan Pre-Coastal Range, as well as the Catalan Coastal Depression and other coastal and pre-coastal plains located among those mountain ranges. ==Geology== Geologically the Catalan Mediterranean System is the result of a tectonic uplift, about 300 km long and roughly 50 km wide. Transversally the system can be divided in three zones: *Northern Zone, between the Empordà comarca and the Llobregat. This zone is of paleozoic and crystalline composition *Central Zone, between rivers Llobregat and Ebre *Southern Zone, between the Baix Ebre comarca and the Millars River in the Valencian Community. Both the central and the southern zone are of mesozoic and tertiary composition. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Catalan Mediterranean System」の詳細全文を読む スポンサード リンク
|