Bedrock stress-release features on Manitoulin Island, Ontario. Manitou
lin Island has large exposed bedrock plains underlain by Ordovician an
d Silurian carbonates. The generally flat-lying strata reveal evidence
of rock stress relased by faults at Little Current and by pop-ups els
ewhere. Four pop-ups occur at widely separated localities on the islan
d and several other small ridges may be pop-ups. Other bedrock stress-
release features may be present but remain undiscovered in the extensi
vely vegetated part of the island.