TexasThose who have witnessed tidal bore roaring up a ravine are astonished that water does not seem to respect the relative sea level during those times. What makes the water climb? Water pressure drives water to climb above its level because at the point where the pressure builds, it takes the easiest path. When the force of pressure is extreme, compressing the water at lower levels, the path of lease resistance is taken. During a tidal wave, this path is away from the bulk of water. A tidal wave moves inland until one of two situations occurs:
Where tidal waves meet mountains, this can result in tidal bore up ravines. Where tidal waves flow inland, this results in a flood tide going hundreds of miles inland. Where the tidal wave finds foot hills or barriers, the force of the wave is broken such that it is slowed, allowing a reduction in pressure behind the wave to arrive before the wave moves far inland. But where the tidal wave finds virtually no barriers, due to the land being flat, it becomes water on the move, and this very momentum carries it far inland, and above a height that would otherwise be expected. Water on the move does more than just push forward, it also creates a void behind it. At first, this water is on the move because there is pressure behind it, like sloshing water in the Gulf. But then, the force of this moving water takes on a life of its own. It has momentum, and moving forward, creates a void behind it, thus drawing the water in the direction of motion, thus continuing the motion. This water on the move is greater than the resistance in front of it, so it continues. For Texas, this means that the water will lap at the foothills of the Rockies, before dying back.
Texas will be devastated by waters sloshing in from the Gulf during the pole shift as well as the rising waters that occur within in the first two years after the pole shift. Being flat land, and low, the Gulf will roll over Texas without opposition, at a height of several feet. This water must go someplace, and will take the path of least resistance. If the water is flowing most rapidly as it moves over the flat land, then water that would normally move toward mountains or natural barriers will be diverted to a faster moving flow area - the Texas plains. Thus Texas, due to its flat terrain, will get more water overall than neighboring areas. Even the high plains will have several feet of water moving across it, where the coastal areas will have tidal waves hundreds of feet high. With few tall trees and faced with the after effects of hurricane force winds and earthquakes that will flatten all but new steel skyscrapers, desperate survivors will have few places to go to escape the moving sheet of water, which will drag whatever it engulfs back out into the Gulf on its return.
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