By means of progressive interactions with reactive forms of potential, this results in the segregation of those elements, which in the form of allotropic intermediate substances were left untouched, whereas the more inferior substances descend even further under even stronger influences of heat and are even further broken down. Once again what is still useful will be precipitated out and deposited, until the most inferior substances of all attain their relatively lowest state of evolvement and thereby their greatest degree of separation from the most noble, which on the other side has risen to the highest state. In terms of its height and depth, this is how the above threshold-element deposit comes into being. Therefore through a graduated process of deposition according to quality, the variously potentiated indifferent elements have different developmental periods. Those with a smaller separation interact earlier than the others, and logically, have to cover shorter developmental paths in order to reach the next higher evolved state. [The Energy Evolution - Harnessing Free Energy from Nature, The Economy Founded on Reactively Produced Energy]

The straightening of a watercourse in order to shorten it and steepen the geological gradient results in an even stronger deposition of sediment and even greater flattening of the geological gradient, a widening of the channel, the warming of the water and its even more rapid disappearance.[7] [The Energy Evolution - Harnessing Free Energy from Nature, The Transport of Ore in Double-Spiral-Flow Pipes]

See Also


Created by Dale Pond. Last Modification: Tuesday October 4, 2022 04:27:10 MDT by Dale Pond.