Thrust faults of this kind are not uncommon in many mountain chains around the world, but the Glarus thrust is a well accessible example and has as such played an important role in the development of geological knowledge on mountain building. For this reason the area in which the thrust is found was declared a geotope, a geologic UNESCOWorld Heritage Site, under the name "Swiss Tectonic Arena Sardona." The area of this "tectonic arena" encompasses 32,850 hectares of mainly mountainous landscape in 19 communities between the Surselva, Linthtal and Walensee. In the arena are a number of peaks higher than 3000 meters, such as Surenstock (its Romansh name is Piz Sardona, from which the name comes), Ringelspitz and Pizol.
In 2006, the Swiss government made a first proposal to declare the region World Heritage to the International Union for Conservation of Nature (IUCN). The IUCN then did not find the area to have an extraordinary or universal value and denied the proposal. The Swiss made a new, this time successful proposal in March 2008. The region was declared a World Heritage Site in July 2008, because "the area displays an exceptional example of mountain building through continental collision and features excellent geological sections through tectonic thrust."[1]
The first naturalist to examine the Glarus thrust was Hans Conrad Escher von der Linth (1767–1823). Escher von der Linth discovered that, contradictory to Steno'slaw of superposition, older rocks are on top of younger ones in certain outcrops in Glarus. His son Arnold Escher von der Linth (1807–1872), the first professor in geology at the ETH at Zürich, mapped the structure in more detail and concluded that it could be a huge thrust. At the time, most geologists still accepted the theory of geosynclines, which states that mountains are formed by vertical movements within the Earth's crust. Escher von der Linth had therefore difficulty with explaining the size of the thrust fault. In 1848, he invited the British geologist Roderick Murchison, an international authority, to come and look at the structure. Murchison was familiar with larger thrust faults in Scotland and agreed with Escher's interpretation. However, Escher himself felt insecure about his idea and when he published his observations in 1866 he instead interpreted the Glarus thrust as two large overturned narrow anticlines. This hypothesis was rather absurd, as he admitted himself in private.
Escher's successor as professor at Zürich, Albert Heim (1849–1937), initially stuck to his predecessor's interpretation of two anticlines. However, some geologists favoured the idea of a thrust. One of them was Marcel Alexandre Bertrand (1847–1907), who interpreted the structure as a thrust in 1884, after reading Heims observations.[3] Bertrand was familiar with the Faille du Midi (Variscan orogeny), a large thrust fault in the BelgianArdennes. Meanwhile, British geologists began to recognize the nature of thrust faults in the Scottish Highlands. In 1883, Archibald Geikie accepted that the Highlands are a thrust system.[4] Swiss geologists Hans Schardt and Maurice Lugeon then discovered in 1893 that in western Switzerland, Jurassic rock layers are on top of younger molasse too, and argued that the structure of the Alps is a large stack of nappes, large sheets of rock that had been thrust on top of each other.[5] At the turn of the century, Heim was also convinced of the new theory. He and other Swiss geologists now started mapping the nappes of Switzerland in more detail. From that moment on, geologists began recognizing large thrusts in many mountain chains around the world.
However, it was still not understood where the huge forces that moved the nappes came from. Only with the arrival of plate tectonic theory in the 1950s an explanation was found. In plate tectonics, the horizontal movement of tectonic plates over the Earth's soft asthenosphere causes horizontal forces within the crust. Presently, geologists explain the formation of most mountain chains by the convergent boundary evolving between tectonic plates accompanied by a subduction process in which the heavier plate dives beneath the less dense plate and sinks into the Earth's mantle.
^Bertrand, M. (1884). "Rapports de structure des Alpes de Glaris et du bassin houiller du Nord". Société Géologique de France Bulletin. 3rd. 12: 318–330.
Badertscher, Nicolas P.; Beaudoin, Georges; Therrien, René; Burkhard, Martin (2002). "Glarus overthrust: A major pathway for the escape of fluids out of the Alpine orogen". Geology. 30 (10): 875–878. doi:10.1130/0091-7613(2002)030<0875:GOAMPF>2.0.CO;2. ISSN0091-7613.
Herwegh, Marco; Hürzeler, Jean-Pierre; Pfiffner, O. Adrian; Schmid, Stefan M.; Abart, Rainer; Ebert, Andreas (2008). "The Glarus thrust: Excursion guide and report of a field trip of the Swiss Tectonic Studies Group (Swiss Geological Society, 14–16. 09. 2006)". Swiss Journal of Geosciences. 101 (2): 323–340. doi:10.1007/s00015-008-1259-z. ISSN1661-8726.
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