Geography
Mangualde is dominated by a plateau/table sloping to the south, cut by tributaries of the Dão and Mondego Rivers: the municipality is crossed in the north by the Dão River defining its northern frontier, while its southern border is limited by the Mondego. In addition to these rivers, Mangualde is crossed by a series of gently-flowing ravines and rivers, such as the Ribeira de Frades, Ribeira do Castelo and the Ribeira de Videira, in the western extend of the municipality. The Fagilde reservoir is the largest extension of these limits, and supports the community to the north of Mangualde.
Along the valleys there are many fertile alluvial lands, of which, the more fertile parcels are located in the central part of the municipality, around the civil parishes of Mangualde, Fornos de Maceira Dão, Espinho and Alcafache.
Geomorphologically, Mangualde is part of the Maciço Antigo (Old Massif), dating to the Paleozoic. It was affected by a period of prolonged erosion, that was later rejuvenated by upheaval associated with mountain-building. Most of the area is composed of granite, and mitigated by mountain hydrology. A small group of mountains along the east, the Serra do Bom Successo, witih extend to Guimarães de Tavares. In addition, other mountainous areas include the Serras de Abrunhosa-a-Velha, Cunha Alta and Almeidinha which link to the Serra da Senhora do Castelo. Disperse and running along lower elevations, the topography is highlighted by the higher elevations in Tabosa, Roda an Fagilde.
Read more about this topic: Mangualde Municipality
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