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Obryv u granicy Olimpa
27.01.2008 14:46 | morningstar2008 morningstar2008
Spolzanie grunta s Olimpa daet vozmozhnost' predpolagat' chto grunt vulkana sostoit vodopeschanoi zamorozhennoi smesi. Ottayavshie grunty otkalyvayutsya i splyvayut ostavlyaya posle sebya krutye otkosy. Po foto Olimp mozhno opredelit' chto v osnovnom gora v bol'shei svoei chasti povrezhdena tol'ko s Yuzhnoi storony. Severnaya storona zhe ne osypalas' do sih por. Krater na vershine Olimpa tak zhe imeet harakternye vodopeschannye podvizhki. Olimp.doc(181KB)
http://www.astrolab.ru/cgi-bin/galery3.cgi?id=9&no=71
http://www.astrolab.ru/cgi-bin/galery3.cgi?id=9&no=64
http://www.astrolab.ru/cgi-bin/galery3.cgi?id=9&no=69
Vernee budet skazat', s Solnechnoi storony vulkana proishodit intensivnaya potaika. No moi interes k etomu voprosu zaklyuchaetsya v drugom. Izvestno, chto eto vulkan. No vulkanicheskie vybrosy na Zemle eto bazal'tovaya lava. A v sravnenii s Olimpom bol'she pohozhe na to, chto eto byl gryazevoi vulkan.
- >> Obryv u granicy Olimpa (morningstar2008 morningstar2008, 27.01.2008 14:46, 2.6 KBait, otvetov: 1)
- Re: Obryv u granicy Olimpa (A. V. Ivanov, 4.02.2008 4:02, 469 Bait)