Guide books of excursions in Canada1-10 . dvance. Described by. In Lituya bay In Lituya bay Brady Portage Baker Betwn 1786 and 1786 and 1794 and 1794 and 1880. Before 1800 . 2% miles (4 km.)3 miles ( km.)5 miles (8 km.)1 to 3 miles( ) Otto Martin. Lawrence Martin. Serpentine Toboggan Western Malaspina . Serpentine Western Malaspina(Guyot) Before 1817 .Before 1840 . Lawrence Martin. Lawrence Martin. Betwn 1837and 1880. Before 1882 . About 20miles (32km.) Lawrence Martin. be-fo
Guide books of excursions in Canada1-10 . dvance. Described by. In Lituya bay In Lituya bay Brady Portage Baker Betwn 1786 and 1786 and 1794 and 1794 and 1880. Before 1800 . 2% miles (4 km.)3 miles ( km.)5 miles (8 km.)1 to 3 miles( ) Otto Martin. Lawrence Martin. Serpentine Toboggan Western Malaspina . Serpentine Western Malaspina(Guyot) Before 1817 .Before 1840 . Lawrence Martin. Lawrence Martin. Betwn 1837and 1880. Before 1882 . About 20miles (32km.) Lawrence Martin. be-fore 1889 . H. W. Seton-Karr. Nellie Juan Toboggan Baker U. S. Grant. Lawrence Martin. Before 1891 . Lawrence Martin. Eastern Malaspina Muir Before 1891 . Before 1890 and Over 1,500ft. (450m.)300 yards(270 m.) I. C. F. Reid. Fredericka C. W. Hayes. Patterson 1891. H. F. Reid. Columbia About 1895 About 18971808 G. K. Gilbert. La Perouse G. K. Gilbert. Columbia G. K. Gilbert. Barrv Lawrence 34883—n 162 With these facts in mind it is reasonable to predictthe advance of other and longer glaciers in the Yakutat Bayregion as a result of avalanching during the 1899 earth-quakes, for, just as the several Alsek glaciers, 55 to 75miles (88 to 120 km.) east of Yakutat bay, and the Loganglacier, 80 miles (128 km.) to the northwest, advanced in1908, 1909, and 1912, respectively, so the other and longerice tongues of the St. Elias range will eventually feel this im-pulse and push forward. In 1913 for instance, Sewardglacier may move forward. This glacier heads on thedivide with Logan glacier which advanced in 1912 afterat least 200 years of stagnation. A strong advance ofSeward glacier would break up the central, stagnantportion of the Malaspina and change the dirty, moraine-mantled slopes at Sitkagi bluffs into a clean, crevassedceberg-discha-ging, tidal ice front. GRANBY BAY, OBSERVATORY INLET. BYR. G. MCCONNELL. INTRODUCTION. The objective
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Keywords: ., bookcentury1900, bookdecade1910, booksubjectgeology, bookyear1913
