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- W1997799807 abstract "‶Every fresh district that a geologist examines adds to his store of facts, and strengthens his theoretical ideas as to the origin of the structures he observes.″ Such was a passage in an able article in the ‶Quarterly Magazine″ for July 1859, a copy of which I found in the hotel on the Eggischhorn in September last,—a passage that may serve as my excuse for presenting several geological notes which I made last autumn during a short tour through Switzerland and Savoy. In particular, I was struck with the phenomena of weather action exhibited by the Alps, and took every opportunity during my stay of observing and noting down the more prominent features of Alpine configuration. It is only when we attain the summit of some Alpine eminence that we can adequately realise the importance of the part played by weather action in bestowing upon the Alps their present forms. On ascending the Eggischhorn, for instance, we gradually leave wooded and grass-covered slopes to find ourselves traversing at last nothing but loose earth and loose stones; and finally discover that the peak (9682 feet above the sea) consists simply of a pile of great blocks over which one must clamber for a quarter of an hour to reach the summit. From this point, the Spitze, or peak of the Eggischhorn, a magnificent and world-renowned panorama, opens on every side. From the Eggischhorn I observed, sharply defined against the cloudless sky, peaks similar to, although on a smaller scale than, the" @default.
- W1997799807 created "2016-06-24" @default.
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- W1997799807 date "1877-01-01" @default.
- W1997799807 modified "2023-09-25" @default.
- W1997799807 title "Phenomena of weather action and glaciation exhibited by the Alps of Switzerland and Savoy" @default.
- W1997799807 doi "https://doi.org/10.1144/transed.3.1.11" @default.
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