Comparisson reports are under license of:
“The edges of the Gulf of Buccari (Bakar) are all tall and mountainous, made from limestone. On the top parts is limestone from the Cretaceous period, and below are nummulites. Only at the far side of the two Buccari and Buccarizza (Bakarac) gulfs are there valleys closed in by hills. Buccarizza’s has seas without fossils in its thalweg with layers of marlstone.”
A.L.S.: Buccari, Prague 1871
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