ā¦and the Guadiana, the Alto Alentejo is a continuation of the Spanish tablelandsāa series of plateaus, either crystalline (Paleozoic Cambrian and Silurian schists), at 600 to 1,300 feet (180 to 400 metres) with poor soils except where outcrops of diorite have weathered into rich black soils, or limestone, with piedmontā¦
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