The Rotating Earth and Plate Tectonics by Robert Maurer
This work explores the nature and origin of the forces responsible for the unrelenting unidirectional movements of continental sized masses away from what was Pangea c. 275 Ma years ago to their present positions.
The analysis given demonstrates that the forces responsible for tectonic movements are related to the rotational velocity of the Earth which is dependent on the Sun’s gravitational pull on the asymmetrical positioning of the Earth’s centre of mass.
The resultant unbalanced rotation gives rise to the Earth’s wobble and the significant circumferential forces that move the continental masses. It is these tectonic movements in which continental and oceanic crusts are continuously forced into the mantle, that forever ensures that the lithosphere is recycled and regenerated.
Furthermore, the offset ‘centre of mass’ gives rise to the generated and tilted N-S principal axis of rotation that applies to all the planets. This action also yields a viable explanation regarding why all the planets (Venus apart) rotate in the same direction as the Sun.
Synopsis
This treatise relates tectonic processes to the circumferential forces associated with the rotational velocity of the planet Earth. This approach allows for alternative explanations to the convection current system, to be offered to describe tectonic plate movements. In developing this argument, the following points will be examined and discussed.
- The positioning of the centre of mass (COM) of the Earth that gives rise to both the tilt and in the case of the Earth, its ‘wobbly’ motion. This is noted by the cyclical movement of the principal of axis of rotation as noted by the Milankovitch cycles.
- The development of the mathematical relationship between the differential circumferential forces in the crust, the offset COM, and the Earth’s rotational velocity.
- The creation of the principal N-S axis of rotation by the mutual gravitational pull of the Sun.
- The extrapolation of the above action to the planets, their common hand of rotation and similar tilt angles.
- The introduction of the concept of the momentum of the moving plates and its initiation of the subduction cycle.
- Subduction is thus shown to be a consequence of the developed momentum of the moving tectonic plates as distinct from being the driving force.
- The development of an alternative cycle of continuous lithosphere regeneration that challenges the presently accepted Wilson cycle.