Leaving Madigan's party on November 19, when forty-six miles from the Hut, Stillwell, Hodgeman and Close of the Near-Eastern Party diverged towards a dome-shaped mountain--Mount Hunt. A broad valley lay between their position on the falling plateau and this eminence to the north-east. Looking across, one would think that the depression was slight, but the party found by aneroid that their descent was one thousand five hundred feet into a gully filled with soft, deep snow. After skimming the polished sastrugi of the uplands, the sledge ran heavily in the yielding drifts. Then a gale of wind rose behind them just as the ascent on the other side commenced, and was a valuable aid in the pull to the summit. From the highest point or cap of what proved to be a promontory, a wide seascape dotted with bergs was unfolded to the north. To the west the eastern cape of Commonwealth Bay was visible, and sweeping away to the north-east was the Mertz Glacier with sheer, jutting headlands succeeding one another into the distance. True bearings to these points were obtained from the camp, and, subsequently, with the help of an observation secured on the 'Aurora' during the previous year, the trend of the glacier-tongue was determined. Hodgeman made a series of illustrative sketches. On November 21 the party commenced the return journey, moving directly towards Madigan Nunatak to the south-west. This nunatak had been sighted for the first time on the outward march, and there was much speculation as to what the rock would prove to be. A gradual descent for seven miles brought them on to a plain, almost at sea-level, continuous with the valley they had crossed on the 19th further to the east. On the far side of the plain a climb was commenced over some ice-spurs, and then a broad field of crevasses was encountered, some of which attained a width of fifty yards. Delayed by these and by unfavourable weather, they did not reach Madigan Nunatak until the evening of November 20. The outcrop--a jagged crest of rock--was found to be one hundred and sixty yards long and thirty yards wide, placed at an altitude of two thousand four hundred feet above sea-level. It is composed of grey quartzose gneiss. There were no signs of recent glaciation or of ice-striae, though the rock was much weathered, and all the cracks and joint-planes were filled with disintegrating material. The weathering was excessive and peculiar in contrast with that observed on fresh exposures near the Hut and at other localities near sea-level. After collecting specimens and placing a small depot of food on the highest point, the party continued their way to the Hut, reaching it on November 27.