A geomagnetic reversal is described below:
Does the chaotic impulse of a metastable metallic hydrogen (MSMH) comet striking the pebbleshell of earlier comet debris cause the mysterious pole reversals of the Earth? The supermagnetism and super-density of this matter would be enough to totally rejuvenate the intensity of the magma plumes which rise towards the surface imo. A cascade of movement from geomagnetic pole to geomagnetic opposite pole by the mega-comets would create an energy whirlstorm within the Earth's interior. Plate movement would eventually accelerate accordingly and mountain building would proceed at an accelerated pace.
A geomagnetic reversal, which is sometimes called a "polar reversal"[1][2] or a "pole shift",[3] is a change in the Earth's magnetic field such that the positions of magnetic north and magnetic south are interchanged. The Earth's field has alternated between periods of normal polarity, in which the direction of the field was the same as the present direction, and reverse polarity, in which the field was in the opposite direction. These periods are called chrons. The time spans of chrons are randomly distributed with most being between 0.1 and 1 million years. Most reversals are estimated to take between 1,000 and 10,000 years. The latest one, the Brunhes–Matuyama reversal, occurred 780,000 years ago. Brief disruptions that do not result in reversal are called geomagnetic excursions.
Does the chaotic impulse of a metastable metallic hydrogen (MSMH) comet striking the pebbleshell of earlier comet debris cause the mysterious pole reversals of the Earth? The supermagnetism and super-density of this matter would be enough to totally rejuvenate the intensity of the magma plumes which rise towards the surface imo. A cascade of movement from geomagnetic pole to geomagnetic opposite pole by the mega-comets would create an energy whirlstorm within the Earth's interior. Plate movement would eventually accelerate accordingly and mountain building would proceed at an accelerated pace.
External triggersSome scientists, such as Richard A. Muller, believe that geomagnetic reversals are not spontaneous processes but rather are triggered by external events that directly disrupt the flow in the Earth's core. Proposals include impact events[28][29] or internal events such as the arrival of continental slabs carried down into the mantle by the action of plate tectonics at subduction zones or the initiation of new mantle plumes from the core-mantle boundary.[30] Supporters of this theory hold that any of these events could lead to a large scale disruption of the dynamo, effectively turning off the geomagnetic field. Because the magnetic field is stable in either the present North-South orientation or a reversed orientation, they propose that when the field recovers from such a disruption it spontaneously chooses one state or the other, such that a recovery is seen as a reversal in about half of all cases.