Post-glacial dislocations and foldings of cretaceous and drift strata in the island of mÖen, in denmark.

GEOLOGICAL STRUCTURES OF THE ISLAND OF MÖEN—GREAT DISTURBANCES OF THE CHALK POSTERIOR IN DATE TO THE GLACIAL DRIFT, WITH RECENT SHELLS—M.PUGGAARD’S SECTIONS OF THE CLIFFS OF MÖEN—FLEXURES AND FAULTS COMMON TO THE CHALK AND GLACIAL DRIFT—DIFFERENT DIRECTION OF THE LINES OF SUCCESSIVE MOVEMENT, FRACTURE, AND FLEXURE—UNDISTURBED CONDITION OF THE ROCKS IN THE ADJOINING DANISH ISLANDS—UNEQUAL MOVEMENTS OF UPHEAVAL IN FINMARK—EARTHQUAKE OF NEW ZEALAND IN 1855—PREDOMINANCE IN ALL AGES OF UNIFORM CONTINENTAL MOVEMENTS OVER THOSE BY WHICH THE ROCKS ARE LOCALLY CONVULSED.