Monash University geoscientist Associate Professor Wouter Schellart, and his colleague Professor Wim Spakman from Utrecht University, have discovered how the floor of an entire ocean basin that was destroyed 70 to 50 million years ago off the North coast of New Guinea is currently located at 800 - 1200
km depth below Central and South - eastern Australia.
Not exact matches
The experiments showed the team that, above a
depth of 1,000 kilometers and
below a
depth of 1,700
km, bridgmanite contains nearly equal amounts of oxidized and reduced forms of iron.
Because Atlantis Bank has been drilled before, and its condition is known, fairly swift progress is expected on this first outing, with the hole being opened to a
depth of perhaps 1.3
km below the seabed.
shows that natural VOC induced aerosols above the boundary layer are mostly of natural origin (7:1), and comprise a 2:1 up to > 10:1 amount, compared to SOx (SO2 + sulfate) aerosols in the 0.5 - 10
km free troposphere, or 10 % of the total aerosol optical
depth measured by satellites... Add to that the effect
below the boundary layer and the effect of other natural aerosols (natural fires, sea salt, sand dust, DMS, NOx), good for some 38 % of the < 1 micron fraction of total aerosols (according to IPCC estimates)...
And knowledge never ceases to advance — just in the last month we have that Antartica is forming ice from
below, at a
depth of 2
km.