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Updated: October 7, 2026
In the peninsula of Lacuy, the strata over a width of four miles have been upheaved by three distinct, and some other indistinct, lines of elevation, ranging within a point of north and south.
In one place they rested on, and in another place were capped by, tuffs and girt-stones, apparently of submarine origin. The neighbouring peninsula of Lacuy is almost wholly formed of tufaceous deposits, connected probably in their origin with the volcanic hills just described.