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Would the fact that there is a small sort of eruption thing going on and under the sea just off Santorini have an effect?
Originally posted by BobAthome
reply to post by PuterMan
"cone building"
why,,cone building
much more,,,u know there is some small evidence of this,,cone building ?
why does this particular phenomina , ---->increase %, of ,,a V event?
Me.edit on 19-5-2012 by BobAthome because: (no reason given)
Kolumbo is an active submarine volcano in the Aegean Sea, about 8 km northeast of Cape Kolumbo, Santorini island. The largest of a line of about twenty submarine volcanic cones extending to the northeast from Santorini,[1] it is about 3 km in diameter with a crater 1.5 km across.[2] It was "discovered" when it breached the sea surface in 1649-50
The Global Volcanism Program Holocene volcano database contains no names that match your search criteria. You may want to do a more detailed Name Search, or list all volcanoes that start with K.
The crater floor, averaging about 505 m below the sea surface, is marked in its northeast area by a field of hydrothermal vents and covered by a thick bacterial community, the 2006 NOAA expedition discovered. Superheated (measured as hot as 224°C) metal-enriched water issuing from the vents has built chimneys of polymetallic sulfide/sulfates to a maximum height of 4 m, apparently accumulated since the 1650 event.
Originally posted by PuterMan
reply to post by angelchemuel
Kolumbo is an active submarine volcano in the Aegean Sea, about 8 km northeast of Cape Kolumbo, Santorini island. The largest of a line of about twenty submarine volcanic cones extending to the northeast from Santorini,[1] it is about 3 km in diameter with a crater 1.5 km across.[2] It was "discovered" when it breached the sea surface in 1649-50
[url=https://en.wikipedia.org/wiki/Kolumbo_%28volcano%29]Source: The ubiquitous
The Global Volcanism Program Holocene volcano database contains no names that match your search criteria. You may want to do a more detailed Name Search, or list all volcanoes that start with K.
The crater floor, averaging about 505 m below the sea surface, is marked in its northeast area by a field of hydrothermal vents and covered by a thick bacterial community, the 2006 NOAA expedition discovered. Superheated (measured as hot as 224°C) metal-enriched water issuing from the vents has built chimneys of polymetallic sulfide/sulfates to a maximum height of 4 m, apparently accumulated since the 1650 event.
"old caldera" is not where it would head,,obviously,, it would be, well sealed, and hardened.
magma, and ejecta,,
as in water,, even with the littlest pressure,, cannot be soldered,,,,,
old caldera,,nope,,somewhere else.