

much smaller than the 

 Hubbard. These two gla- 

 ciers, ending in the bay in 

 lofty ice cliffs, from which 

 icebergs are constantly 

 being discharged, had not 

 suffered any notable 

 change, but between them 

 are two glaciers, to which 

 no name had as yet been 

 given, one of which, now 

 called the Haenke gla- 

 cier, had been subjected 

 to changes similar to that 

 of the Variegated glacier, 

 while the other was un- 

 changed. From a nearly 

 stagnant, moraine-covered 

 condition the Haenke gla- 

 cier had become crevassed 

 to an impassable condition, 

 and its end had moved 

 forward for about a mile. 

 In _ September, 1905, its 

 visible terminus was on an 

 alluvial fan a quarter of a 

 mile or more from the 

 sea, but in June, 1906, the 

 front was in the sea dis- 

 charging icebergs and its 

 sea cliff was united with 

 that of Turner glacier. 



Still proceeding west- 

 ward, beyond Turner gla- 

 cier came the Black gla- 

 cier, which was unaltered ; 

 Galiano glacier, already 

 mentioned, and then Atre- 

 vida glacier. In 1905 we 

 were able to ascend the 

 moraine-covered margin 

 of the Atrevida with ease, 

 and we wandered over its 

 ablation moraine at will, 

 while as late as Septem- 

 ber, 1905, the junior au- 

 thor made a trip com- 

 pletely across the glacier, 

 as Russell had done on his 

 way to Mount Saint Elias 

 in 1890.* 



*National Geographic 

 Magazine, vol. iii, 1891, p. 92. 



