A whole century passed from the cessation of all commerce and navigation between Norway and Greenland, till new adventurers began to apply themselves to the discovery of the Eastern district. The first of those who took this affair to heart was Erick Walkendorff, archbishop of Drontheim, who was resolved, at his own charge, to fit out ships for this purpose, but was stopped in this pious design by King Christian the Second, whose disgrace he had incurred. The next was King Frederick the First, whose mind, as it is reported, was bent upon the said expedition, but it was never put in execution. Christian the Third (as Lyscander relates) sent several ships with the same design, but without making any discovery. Frederick the Second succeeded his royal father, as well in the government as in his good design about Greenland; on which errand he sent Mogens Heinson, a renowned seaman in those days. This adventurer, after he had gone through many difficulties and dangers of storms and ice, got sight of the land, but could not approach it; whereupon he returned home again, and pretended, that he might have got on shore, if his ship had not been stopped in the midst of its course, by some loadstone rocks hidden in the sea, so that he could not proceed though he had a very favourable and strong gale of wind, and no ice to hinder him: which frightened him and made him sail back again to Denmark. But the true loadstone rocks, in my opinion, was the terrible fright he was in of not getting safe through the dreadful ice mountains, which threatened him, or else the strong current, which always runs along the states promontory with such violence and rapidity, that it often stops a ship under full sail, so that the ship can make but little or no way at all against it. The cause by others assigned for this strange effect, the fish Remora, which the Northlanders call Kracken, is nothing but a fabulous story of the too credulous ancients, and labours under no less absurdities than the former opinion, that rocks of loadstone, laying on the bottom of the sea, can stay the course of a ship that sails on the surface of it.