args[0]=message
args[1]=DB::DB::Message=HASH(0x61f3250)
Re: Vulkany Marsa
28.01.2008 11:47 | 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. http://www.astronet.ru/db/forums/1225774
I sudya po bol'shoi shozhesti ostal'nyh vulkanov na Marse oni tozhe yavlyayutsya gryazevymi vulkanami.
http://www.membrana.ru/images/forms/4475.jpeg
[Citirovat'][Otvetit'][Novoe soobshenie]
| Forumy >> Obsuzhdenie publikacii Astroneta |
| Spisok / Derevo Zagolovki / Annotacii / Tekst |
- Vulkany Marsa ( xTerra.ru, 13.11.2001 11:53, 1.5 KBait, otvetov: 1)
- >> Re: Vulkany Marsa (morningstar2008 morningstar2008, 28.01.2008 11:47, 3.4 KBait)