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  1. en.wikipedia.org › wiki › GuyotGuyot - Wikipedia

    In marine geology, a guyot (/ ˈ ɡ iː. oʊ, ɡ iː ˈ oʊ /), [1] [2] also called a tablemount, is an isolated underwater volcanic mountain with a flat top more than 200 m (660 ft) below the surface of the sea. [3]

  2. 24 wrz 2024 · Arnold Henry Guyot was a Swiss-born American geologist, geographer, and educator whose extensive meteorological observations led to the founding of the U.S. Weather Bureau. The guyot, a flat-topped volcanic peak rising from the ocean floor, is named after him. He studied at the College of Neuchâtel.

  3. Guyot was born on September 28, 1807, at Boudevilliers, near Neuchâtel, Switzerland. He was educated at Chaux-de-Fonds, then at the college of Neuchâtel. In 1825, he went to Germany and resided in Karlsruhe where he met Louis Agassiz, the beginning of a lifelong friendship. From Karlsruhe he moved to Stuttgart, where he studied at the gymnasium.

  4. Guyot, isolated submarine volcanic mountain with a flat summit more than 200 metres (660 feet) below sea level. Such flat tops may have diameters greater than 10 km (6 miles). (The term derives from the Swiss American geologist Arnold Henry Guyot.) In the Pacific Ocean, where guyots are most.

  5. www.encyclopedia.com › historians-miscellaneous-biographies › arnold-henri-guyotArnold Henri Guyot | Encyclopedia.com

    27 cze 2018 · Swiss geologist and geographer. Arnold Henri Guyot 's geological field studies advanced the knowledge of lakes , glaciers , ice ages , mountains, erratic boulders, evolution , and weather . Guyot was born in Boudevilliers, Switzerland, on September 28, 1807. After graduating from the University of Neuch â tel, Switzerland, in 1825, he went to ...

  6. The first is the “death-by-emergence-and-submergence” hypothesis that postulates that guyots are drowned reefs. Regional tectonic and eustatic (sea level) changes cause a temporary emergence of the reef above sea level followed by a rapid relative rise in sea level to drown the reef.

  7. Guyot, Arnold [Henri] (1807-1884), who in 1855 began the first systematic instruction in geology at Princeton, was born at Boudevilliers near Neuchatel, Switzerland. He obtained his doctoral degree at Berlin with a dissertation on ``Natural Classification of Lakes.''

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