26; 



PLATE CXLV. THE COAST-LINE NORTH OF BARNE INLET. 



From a sketch made on the Southern Sledge Journey ; Jan. 20, 1903, 6 P.M. 

 (Map A.) 



In this drawing the same coast-line is included which has already been figured 

 in Plate CXLII., but from another bearing. 



The mouth of the glacier emerging by the Goorkha Craters is here visible, 

 while to the left of it is the range of mountains which forms the northern boundary 

 of Barne Inlet. In this range are the following named peaks, Mount M'Lintock 

 the highest, 10,530 feet above sea-level; Mount Henderson, 8120 feet; and Mount 

 Aldrich, 8050 feet. (See also Plate CXLVI.) 



Barne Inlet is some 12 miles across at its mouth between Cape Kerr on the N. 

 and Cape Selborne on the S., and as in the case of the other inlets, namely Skelton, 

 Mulock, and Shackleton Inlets, forms the passage by which an immense flow of 

 glacier ice passes into and merges with the Barrier from the continental Inland 

 Ice-cap. 



PLATE CXLVI. BARNE INLET AND MOUNT M'LINTOCK. 

 From a sketch made on the Southern Sledge Journey ; Jan. 13, 1902. (Map A.) 



Between Cape Selborne and the mountain range beyond is the wide opening 

 known as Barne Inlet. 



The sketch gives detail of the M'Lintock range of mountains, which is absent 

 in Plate CXLV., though the latter represents the same mountains from another 

 bearing. 



Where the inland ice, flowing from this inlet, meets the Barrier ice, there is 

 an immense disturbance which becomes visible in waves and lines of rupture 

 running many miles outward from the coast. The chasms which thus appear have 

 already been described and pictured (see Plates CVL, CVIL, and CVIII., fig. 2). 



PLATE CXLVIL THE "PYRAMID AND TABLE MOUNTAIN" 



RANGE. 



From a sketch made on the Southern Sledge Journey; Jan. 8, 1903, 3 P.M. 

 (Map A.) 



In this sketch part of the land-mass which lies between Barne Inlet to the 

 N. and Shackleton Inlet to the S. is shown. 



