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Vila do Conde topographic map

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Vila do Conde

The area of Vila do Conde is part of the granite-metamorphic basement, the Iberian Hercynian massif, that extends from the Spanish border to Espinho (15 km (9 mi) south of Porto). Over the Hercynian bedrock there is a prevalence of sandy beaches, and in other areas, the erosion of these sands has allowed the exposure of the rocky substrata. Most of the rock outcrops (never more than 20 metres) disappear north of the Ave River. Yet, these deposits are irregular, and most comparable sediments are not necessarily found at the same altitude. There are also deformations associated with the last inter-glacial period, that have affected these sedimentary layers, most commonly in the beach of Sampaio, where deposits have been discovered between various altitudes (5 and 9 metres).

Wikipedia (CC-BY-SA 3.0)

About this map

Name: Vila do Conde topographic map, elevation, terrain.

Location: Vila do Conde, Porto, Portugal (41.25549 -8.76796 41.42571 -8.61062)

Average elevation: 29 m

Minimum elevation: -3 m

Maximum elevation: 236 m

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