Samuel Hall Young,
Alaska Days with John Muir
(1915)
“ The face of the glacier where it discharged its icebergs was very narrow in comparison with the giants of Glacier Bay, but the ice cliff was higher than even the face of Muir Glacier. The narrow canyon of hard granite had compressed the ice of the great glacier until it had the appearance of a frozen torrent broken into innumerable crevasses, the great masses of ice tumbling over one another and bulging out for a few moments before they came crashing and splashing down into the deep water of the bay. ”
