The ice opened this afternoon in a miraculous manner, in one long lead from land to land, sufficiently wide for us to pass through; and then, as if it had opened expressly for us, closed again, and with such rapidity that our consort, who was following in our wake, having lagged a little behind, was caught and remained beset for some time; eventually, however, boring through and rejoining us. _August 9th._--We succeeded this morning in pushing on for three or four miles, when, being completely stopped by the ice, we were again compelled to make fast. In consequence of the heavy fall of snow yesterday, the surface of the water was coated with a soft sludgy substance, half ice and half snow, which greatly impeded our progress. The statement made by Dr. Hayes in his interesting work, that "along the entire coast of Grinnell Land no glacier appears," is slightly inaccurate; for at the head of Franklin Pierce Bay two tolerably large glaciers are situated, whilst another was seen a few miles to the westward on the same coast. Doubtless Dr. Hayes intended to say _discharging_ glaciers, in which case he would, I think, be nearly correct. For three days were we detained, without the ice allowing us the slightest chance of moving, during which time a complete series of magnetic observations was obtained on the floe, the inclination of the needle being as much as 85° 34´. Both the dredge and trawl were also put into requisition and with good results. Amongst the many zoological curiosities brought to the surface, from a depth of fifteen fathoms, were some crinoids. These echinoderms are very rare, few specimens having been met with, until the deep-sea dredgings of the "Challenger" brought them more into notice. A small island, since called Norman Lockyer Island after the distinguished astronomer of that name, was visited, and its highest eminence ascended for the purpose of watching the movements of the pack. Landing on the ice-foot that fringed the shore, we stepped on to a long shaly beach that rose in well-defined and regular terraces to at least two hundred feet above the level of the sea, showing the different tidal marks, and illustrating clearly the gradual upheaval of the land. Numerous traces of Eskimo were discovered on this small and remote island, consisting of the sites of several encampments, and a bone harpoon point, all apparently of very ancient date. The highest part of the island is from five to six hundred feet above the sea. It is of limestone formation, and on several of the rocks, especially those at its summit, distinct glacial marks were detected. Vegetation was scanty, although here and there the poppy, saxifrage, and willow could be seen cropping up between the stones.