"At the latitude of Borneo Co, the Dan Data section is continued but here in most of the wells some thin sands are present. These may have come from the Dan Data uplift rather than from the eastern land. As the Bend thickens to the north and becomes once and one mud, and as some sand is introduced under Eastern Daly Pinto county it would look as if the Bend Sea terminated into a bay towards the N.E. This would explain the abrupt general asymmetry of the Bend confound with the Monroe-Dropannella. This would mean northwest southeast a Wreckle-Lanoria landbarian.To the north of this land lay the Monroe Sea, and the greater subsiding personline onto its 12,000 feet of Plenty at Jackford, To the south of the Lanier Day the Bend Sea coming in from Donora. See map beyond in Bend Arch.