@Vasilis
2) you say the ''kawa was already there''
But I ask you this...
- How did it get there in the first place.
It we were to analyse the statement of oxides depositing into cracks of the stone on the bottom of the ocean...
Where did the oxides come from if not from the stone itself?
I'm trying to imagine water loaded with mineral oxides flowing into tiny fisures in the layers on the bottom of the ocean ... where oxigen concentration is low...presure is high and in some cases temperature is high.
The oxides did not flow into the cracks...THEY WERE BORN THERE...thats why they are bonded to the stone.
Yess i'll give you this...they may have formed on the bottom of the ocean....
But it's highly more probable they may have been formed by infiltrating water that flowed through the cracks once the deposit surfaced and was exposed to the oxigen in the air and flowing and infiltrating water under the effect of gravity. But seeing that we cant dive to the botom of the ocean in the oxigen poor zone to extract a jnat and check it for kawa...but we have proof kawa exists in an aerobus enveironment...who knows.