Earth crust displacement

Theory of the Earth crust displacement shows that over long periods of time, approximately forty one thousand years, certain forces act in the direction of the outer limits of endurance.Among the critical factors are: massive accumulation of ice at the poles, which changes the weight of the crust, the Earth's axis tilt, which is every 41 000 was changed for more than three degrees (which should not be confused with the volatility that causes the precession of the equinoxes), and, of course, relative proximity to massive celestial bodies like the Moon and the Sun, which also varies throughout the precessional cycle of several thousand years.The theory of Crustal Displacement states that the entire crust of the Earth can shift in one piece like the lose skin on an orange.The assumption is that the outer crust of the earth in relation to the cellular interior, but the tectonic plate movements, the movement is extremely slow.
Vertical displacements of the earth's crust along the rupture resulting from such earthquakes can generate destructive tsunami waves which can travel across an ocean spreading destruction across their path.
Tectonics actually talking about a series of plates that move very slowly in relation to each other.But when it comes to Earth crust displacement, all the plates as a single whole, part of the outer shell of the Earth, which moves in relation to the interior of the Earth.
Most earthquakes happen where tectonic plates meet and glide against each other. Quakes occur when the frictional stress of the movement exceeds the strength of the rocks, causing a failure at a fault line. Violent displacement of the Earth's crust follows, leading to a release of elastic strain energy.
The Crust is a thin layer of solid rock. The material that makes up the crust tends to be lighter than the materials below. The Earth’s crust “floats” on the inner layers. If the Earth were the size of a peach, the crust would only be as thick as the peach’s skin (and not as fuzzy). If the Earth hadn’t cooled enough for the crust to form on its surface, we wouldn’t be here. Neither would any living thing we know of.
Scientists have never been able to dig or drill down through the crust to the mantle. Driving 100 kilometers is easy. Drilling that far through solid rock is hard. Well, it’s solid rock. But, we can study the inside of the Earth by observing volcanoes and geysers. The heat that melts rock into magma, and turns underground water into steam, comes from under the crust.
Most of the evidence usually cited to support the idea of an ice age, there are better fits the theory of earth crust displacement.