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pressure toward Antarctica, the one place on the globe not experiencing plate pressure, allows new land to pop

up between the tips of South America and Africa.

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ZetaTalk: Tidal Waves

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ZetaTalk: Tidal Waves

Note: written prior to July 15, 1995

As great as the danger to humans and the fauna and flora of the Earth that earthquakes bring, greater still is the

devastation that the shifting waters will bring. There are several factors at play. Water is more liquid than the core of

the Earth, and certainly more liquid than terra firma. Where the Earth, dragged by its core, is Shifting into a new, albeit

temporary, alignment with the giant comet, its waters resist greatly. Thus the waters slosh over the nearby land, in the

direction opposite to the shift. This is lessened by a tendency of the waters directly under the giant comet to rise up to

meet the comet. The waters heap up, in what appear to be giant waves. This tends to lessen the sloshing over a

shoreline on the comet side, but has no effect on the water's movement on the dark side of the Earth.

The Earth's record of gigantic tidal waves, which the establishment is desperate to explain in other than pole shift

terms, is caused by the frequent pole shifts. This is the case even in situations where a plate adjustment affects

hundreds of miles of ocean bottom, creating a massive line of compressed water which promptly moves in the only

directions it can - to the right, left, and up. In the depths of the ocean, this causes a tidal wave of perhaps 20 feet in

nearby shores. Where items are dropped into the ocean, such as the honeycombed ice of a former South Pole did

during the Flood, the displaced water cannot go down, so must go all four directions. In instances such as this, the

resulting wave is in proportion to the object dropped. A continent sized object caused the Flood, a meteor a mile in

diameter would hardly cause more than a high tide, despite alarmist speculation.

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ZetaTalk: Climbing Water

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ZetaTalk: Climbing Water

Note: written on Jun 15, 1999.

Those 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 build, is takes the easiest path. When the force of pressure is extreme,

compressing the water a 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:

1. the level to which it has climbed is higher than the level elsewhere, and the wave recedes, or

2. the pressure behind the wave decreases.

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.

Note: below added during the Nov 30, 2002 Live ZetaTalk IRC Session.

There is more to the level that water rises than simply water finding its level. Tidal bore carried water up-river in a

rush, rising above the sea level with force, for many miles. Tidal bore carries water up ravines, in some cases shooting almost straight up, appearing in a gusher at the plateaus overhead. One factor to consider is the force or pressure that

water is under, and this is equivalent to the water higher, elsewhere. This is the factor that allows cities to have tap

water, due to water stored at a high point in the vicinity, which then pushes out into pipes. 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. Thus, rolling across the flat low lands such as the State of Texas, and moving hundreds of miles

inland, on a roll, it does not simply stop when it starts to reach foothills. Why would it stop? Because the overall

elevation is more than the sea level? Weigh this, with the force of water, all on the move, behind the lip of the flood

tide. This water on the move is greater than the resistance in front of it, so it continues.

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ZetaTalk: Flood Tide

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ZetaTalk: Flood Tide

Note: written on Jun 15, 2001, during the 2001 sci.astro debates.

There is a difference in the type of wave that would be caused by an asteroid, and that caused by a sloshing ocean

during a pole shift. During a pole shift, the crust of the Earth rapidly moves a quarter turn or more, in strong shifts

attempting to do a half turn as the core is doing a complete flip, dragging the reluctant crust with it. As anyone

carrying a saucer of soup knows, the soup and the saucer do not always move as one. If the saucer moves suddenly,

the soup may stay behind, slopping. The soup is free to move or not move, where the saucer is attached to the hand of

the server. The oceans of the world are pooled where the crust has offered a dip, but during a pole shift, when the

crust suddenly moves under it, slopping likewise occurs, with the waters not dragged with the core as is the crust,

which is attached to the core. What happens to oceans which are thus lifted out of their beds, and pushed up over land

higher than that from which they came?

Tidal waves are often shown as rising high, a tower of water crashing down upon hapless humans standing in horror on

a beach. Where a wave generated by an underwater displacement, such as occurs when plates adjust due to subduction

during an earthquake, will roll in a deadly line of pressure until the shore is reached and then rise up when the depth of