LB TIN'. IN ANTAKi I'lO SHI 3 



close to its junction with M<nnt Erebus and extending seawards for nomc ten 

 inili-s. luit nowhere more than a mile across. Its extremity was about nine miles from 

 Hut Point. North <>f this lay four small islands. These have shire Keen named the 

 l>ellliridi:e Islands. The more westerly one of these was about a mile from the Glacier 

 Snout, and called " Tent Island," as close by it a camp was established when the 

 attempt was made to assist nature by sawing a channel for the ship through the ice. 

 The camp was maintained for some time after the sawing-out operations had been 

 alMindoncd, and for a short time some dredging operations were conducted among the 

 numerous ice cracks round the island. A bare mile to the north was Inaccessible 

 Island, so called on account of the difficulty of exploring it by a single individual, not 

 on account of its real inaccessibility. These two islands were about the same size, and 

 perhaps a quarter of a mile long, between 300 and 400 feet high. A couple of miles 

 further on, on the lowest slopes of Mount Erebus, was Skuary Point, a broad expanse of 

 basal tie rubble and patches of snow where the Skua, Mrgaltstris inaccorniicki, bred in 

 large numbers. It was from this place that most of their eggs were taken for 

 scientific and domestic purposes. 



The shore line is not much indented, except here and there, where precipitous 

 elitl's are exposed It is covered by a vertical wall of ice varying from between 

 two and a hundred feet in height, consequently there is no tidal zone. Access 

 to the shore from the sea or vice tvwi is in many places rendered easy by the 

 " drift " slopes which speedily accumulate in winter. In the neighbourhood of Cpc 

 Royds the shore is not so precipitous, and a small tidal zone exists, consisting 

 of Ixmlders and volcanic sand. This area was not explored till the relief ships 

 arrived in 1904, and then it was not possible to do much. Red Algae were however 

 seen to be abundant 



The state of the ice in the Sound is almost entirely dependent on the weather, 

 and that is an efficient explanation of our failure to escape from Winter Quarters 

 during the summer of 1902-3. A three days' blizzard at the beginning of May, 

 1902, when the ice was about two feet thick, swept every particle of it out of the 

 Sound, again exposing the area that was open when we arrived in February. In the 

 following September a gale again swept out the ice, and we had open water to well 

 within eight miles of Hut Point. Events of this kind are however accidental. 

 Large areas of the Ross Sea are known to be ice-free at irregular intervals, very 

 early in the season, after the return of the sun on August 23rd. Whatever the 

 condition of the fixed ice in the Sound, all through the summer the mouth is choked 

 at irregular intervals with fields of loose ice, brought in by wind and weather from 

 unknown localities, most probably from the eastward, the current setting from that 

 quarter. Part at least of these fields are eddied into the Sound as they are 

 direi-ted northward by the trend of the coast. It is the frequent presence of these 

 masses of loose ice that damps down the swell that may occur in the ROM Sea, and 

 so retards the breaking-up of the fixed ice. During the season of 1902-3 the open 



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