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Hercynian orogeny
Hercynian orogeny A major and prolonged episode of mountain building that began in the Late Devonian and continued throughout the Carboniferous, affecting a broad belt along an approximately WSW to ENE line from what are now south-western England and north-western Europe to southern Europe and the Iberian Peninsula, and eastern N. America and the Andes. Probably it was caused by northward thrusting and plutonism along a discontinuous front.
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Cite this article
AILSA ALLABY and MICHAEL ALLABY. "Hercynian orogeny." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. 1 Jun. 2012 <http://www.encyclopedia.com>. AILSA ALLABY and MICHAEL ALLABY. "Hercynian orogeny." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. (June 1, 2012). http://www.encyclopedia.com/doc/1O13-Hercynianorogeny.html AILSA ALLABY and MICHAEL ALLABY. "Hercynian orogeny." A Dictionary of Earth Sciences. 1999. Retrieved June 01, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O13-Hercynianorogeny.html |
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Hercynian orogeny
Hercynian orogeny see Variscan orogeny
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Cite this article
PAUL HANCOCK and BRIAN J. SKINNER. "Hercynian orogeny." The Oxford Companion to the Earth. 2000. Encyclopedia.com. 1 Jun. 2012 <http://www.encyclopedia.com>. PAUL HANCOCK and BRIAN J. SKINNER. "Hercynian orogeny." The Oxford Companion to the Earth. 2000. Encyclopedia.com. (June 1, 2012). http://www.encyclopedia.com/doc/1O112-Hercynianorogeny.html PAUL HANCOCK and BRIAN J. SKINNER. "Hercynian orogeny." The Oxford Companion to the Earth. 2000. Retrieved June 01, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O112-Hercynianorogeny.html |
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