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Near Windermere, England, a speck circled, hovered about and landed upon the 300-ft.-by-20-foot plateau which is the summit of Mount Helvellyn, third highest eminence (3,118 feet) in England. Later the speck ascended again, soared away. It was Pilot John Leeming Of the Lancashire Aero Club who, with a bonfire on the snow to indicate the wind and crosses marking possible landing sites, sought to demonstrate upon what a small place an airplane can land...

Author: /time Magazine | Title: Specks | 1/3/1927 | See Source »

...under the auspices of the Canadian Alpine Club, a party of eight mountaineers, numbering in their party Mr. Hall, started up the treacherous slopes of Mount Logan. In the latter part of June they succeeded in reaching the summit and thus achieved the distinction of being the first to conquer the gales and icy blasts of Mount Logan, 19,800 feet in altitude and the second highest peak in North America...

Author: NO WRITER ATTRIBUTED | Title: YUKON EXPLORER TO TELL MOUNTAINEERING FEAT | 12/8/1926 | See Source »

...feet, entered the "chimney"a narrow cleft in the granite, some 150 feet wide, which extends straight up the slope for 1,000 or so feet and enables one to get through the cliffs to the upper final slope of the crest, some distance south of the summit...

Author: NO WRITER ATTRIBUTED | Title: J. E. Wolf Describes Trip to Vicinity of Mt. Whitney in the Sierra Nevadas | 12/6/1926 | See Source »

...summit is a broad, gently-curving dome of white granite, with many large blocks loosened by the weather, and, until one approached the edge and looked down to the base of the tremendous vertical cliffs, all seemed gentle and smiling, for we had a warm, still day. The next day it snowed and visitors were peevish. The view, of course, is immense--peaks on peaks for hundreds of miles, forests and valleys, lakes and streams...

Author: NO WRITER ATTRIBUTED | Title: J. E. Wolf Describes Trip to Vicinity of Mt. Whitney in the Sierra Nevadas | 12/6/1926 | See Source »

...Langley illustrates the dissected dome feature already mentioned. This old summit level is, I suppose, and old plane of erosion, later uplifted, and the dissection guided by the dominant structures of the granite, which includes two vertical planes of easy splitting and, much less marked, a curving horizontal plane of weakness. The weather works into the vertical plane and splits off great blocks, which, falling, form the immense masses at the foot of the cliffs and thus originate the tremendous precipices and great jags of the crest, like splinters set on edge...

Author: NO WRITER ATTRIBUTED | Title: J. E. Wolf Describes Trip to Vicinity of Mt. Whitney in the Sierra Nevadas | 12/6/1926 | See Source »

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