558 . Royal Society. 



and the '23rd and 24th September, 1840; by James Clark Ross, 

 Captain R.N., F.R.S., Commander of the Antarctic Expedition. 



3. Hourly Magnetic Observations for August and September, 

 1840, taken at the Ship's Magnetic Observatory, Van Diemen's 

 Land, under the direction of James Clark Ross, Captain R.N., 

 F.R.S., Commander of the Artarctic Expedition. 



The above papers were communicated by the Lords Commission- 

 ers of the Admiralty. 



4. Variation de la declinaison, intensite horizontal et inclinaison 

 magnetique, observes a Milan, pendant vingt-quatre heures de suite, 

 le 24 et 25 Fevrier et Mars, 1841, par Signior Carlini, Forn. Memb. 

 R.S. 



5. *' Remarks on the Birds of Kerguelen's Land." By R. M'Cor- 

 mick, Esq., Surgeon R.N. of H. M.S. Erebus. Communicated by 

 the Lords Commissioners of the Admiralty. 



The birds usually met with by the author in this island were 

 petrels and penguins ; and besides these, he found two species of 

 gull, a duck, a shag, a tern, a small albatros, and a species of Chionis ; 

 and also a remarkable nocturnal bird allied to the Procellaria. Brief 

 notices are given of the forms and habits of these birds. 



6. " Geological Remarks on Kerguelen's Land." By R. M'^Cor- 

 mick, Esq., Surgeon R.N. of H.M.S. Erebus. Communicated by 

 the Lords Commissioners of the Admiralty. 



The northern extremity of the island is described as being entirely 

 of volcanic origin. The trap rocks, of which the headlands are com- 

 posed, form a succession of terraces nearly horizontal. Basalt is the 

 prevailing rock : it assumes the prismatic form, and passes into 

 greenstone, and the various modifications of amygdaloid and por- 

 phyry. The general direction of the mountain-ranges inclines to 

 the south-west and north-east, and they vary in height from 500 to 

 2500 feet. Many of the hills are intersected by trap dykes, usually 

 of basalt. Several conical hills, with crater-shaped summits, are 

 found, evidently the remains of volcanic vents. Three or four very 

 singular isolated hills, composed of an igneous slaty sandstone, occur 

 in Cumberland Bay, presenting very smooth outlines, and consisting 

 of piles of broken fragments, through which the mass protrudes, in 

 places, in prismatic columns. Vast quantities of debris are accu- 

 mulated at the base of the hills, in many places to the height of 200 

 or 300 feet or more, affording strong evidence of the rapid disinte- 

 gration this land is undergoing, from the sudden atmospheric vicis- 

 situdes to which it is exposed. 



The whole island is deeply indented by bays and inlets, and its 

 surface intersected by numerous small lakes and water courses. 

 These, becoming swollen by the heavy rains, which alternate with 

 frost and snow, rush down the sides of the mountains and along the 

 ravines in countless impetuous torrents, forming, in many places, 

 beautiful foaming cascades, wearing away the rocks, and strewing 

 the platforms and valleys below with vast fragments of rocks and 

 slopes of rich alluvium, the result of their decomposition. 



The most remarkable geological feature in the island is the occur- 



