The Ladeira d`Joana geosite is located on the eastern flank of the Amendoa-Carvoeiro syntrophic, near the village of Pé da Serra.
It is characterized, in general, by metagrauvaques benches, normally amalgamated and with a thickness of some tens of meters, relatively to the metassiltite and metapelite strata.
Serra da Amêndoa
N 39º 39' 17.704'' W 8º 2' 45.765''
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