Ponta da Ferraria e Pico das Camarinhas
SMG 8
37º 51'36''N 25º 51'00''W
“Ponta da Ferraria” is a lava delta formed by basaltic lava flows emitted from “Pico das Camarinhas” scoria cone, 870 years ago. Among the many volcanic features in the geosite, the littoral cone (or pseudocrater), the 62ºC submarine thermal water and the ultramafic xenoliths are worth mentioning.
