05.09.2014 14:15

Ca. 1:20 bis 1:40, Zeitraffer-Aufnahmen von 8 Minuten der fließenden Lava.
Hi Andi,Andi Schönberger hat geschrieben: Hi Uwe
Lieben Dank für Deine Ausführungen
meine Frage war zwar simpel gestellt, hat vielleicht auch etwas naiv geklungen, aber so einfach ist die Antwort darauf doch nicht.
Gerade das WIE![]()
Ist RUV immerhin einen Artikel wert:
http://www.ruv.is/frett/full-frontal-br ... oehoe-lava
Insbesonder zu beachten in dem Artikel:
Dangerous frontal breakouts
..."This is why it can be extremely dangerous to stand close to advancing lava. Even though very little seems to be happening at a given moment, the frontal breakout happens very quickly."
So the lava flow also more than yesterday, "he says, but about a km remaining the Glacial River . Thorvald said that lava is about 11 km long and averages about 2 km wide and still growing.
It is somewhat more active today than yesterday despite being nothing dramatic going on. Gas flow is more and the sun is a red through the clouds. Actually blood red through the plume, "said Thorwald, and adds that it is normal in terms of the sun through the cloud of smoke as this.
It's pretty handsome mocha that flows here east of the eruption site, and probably three or four km altitude and the smoke is mostly gas. We have noticed that nornahár (Hexenhaaare) are falling to the ground, go wicked and being blown onto the sand, "said Thorwald, who had to explain to the journalist what nornahár were.
Nornahár needles are formed in a fissure eruption that gather in bundles and look like hair but are actually ashes.
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