RE:NeophyteThe Kawa-1 well is situated at the beginning of an upward slope Its a gentle gradient at this point with water depth initially almost as deep as Apache's Block58 in Suriname but sediments laid down from the Berbice Canyon in the Eocene-Paleocene period created additional overburden that basically offset the effect of the upward sloping in terms of sea floor to Turonian ..that basically resulted in the pressure levels at the 4000 meter depth and below equalizing even though the Campanian through Santonian was running upwards to the south which of course resulted in water depth becoming lower ..don't raise the bridge ..lower the water