The Eruption of Kilauea 1959-1960 Chap 2
Loading...
52,954
Uploader Comments (mmikemoore)
see all
All Comments (27)
-
idiots idiots idiots if science is all smart why can't we stop so called mother nature just think allah gave u brain or if you wanna call him god
-
i would pay good money to watch this live.
-
LAAAva!
-
Did anyone then capture the sound this made?
-
i really want to go inside kilauea
-
yes. kilauea has been erupting from 1959 until today. i doubt that it has stopped erupting... keep up the steady flow of lava, kilauea! =p
Loading...
If I'm not mistaken, molten lava is less dense than solid rock (unlike water, where the solid phase is lighter than the liquid.) So, why does the cooled surface of the lava not sink?
Envergure 1 year ago
@Envergure,
Viscosity varies greatly, but one of the first analogs for the three types of plate boundaries; divergent, convergent, and transform was observed in lava lakes in Hawaii. As the surface of the lake cools, it breaks into "plates" which interact. Most interesting, and related to your question, are the subduction zones; where one plate of cooled lava dives beneath another. Remember the incredible temperatures involved as well.
mmikemoore 1 year ago
holy moley.
too bad no HQ.
wgibbens 2 years ago
The other 3 chapters are in HQ...I think YouTube will eventually get around to converting this one sooner or later..
mmikemoore 2 years ago