 SMA 2 >
“Pedreira do Campo” is an old quarry front that exhibits a full submarine sequence composed by marine sedimentary rocks with rich fossiliferous content at the base, overlaid by submarine basaltic hyaloclastites and pillow lavas: the sequence is aged of about 5 millions years.
 36º 56'49''N 25º 08'07''W > SEE MAP
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