Translation of "Cape Ray" into French

The Cape Ray granite forms a dominantly tonalitic terrane derived by partial melting of ophiolitic material.

Le granite de Cape Ray forme une terrane tonalitique dominante engendré par la fusion partielle de roches ophiolitiques.

In 1783 it obtained a second French Shore, more limited in size, to the west, extending from Cape Ray to Cape St. John.

Elle obtient un second French Shore plus restreint, déplacé vers l'ouest, du cap Ray au cap St. John en 1783.