Simulations Articles

Simulations

Model G Transmuting Ether Simulator: Create a Subatomic Particle

Below is a simulator of the Model G ether reaction-diffusion system. It is currently set up to generate a one-dimensional representation of a dissipative soliton; i.e., the emergence of a primordial neutron from a spontaneously emerging zero-point energy fluctuation. Just press the “run” button at the bottom. The reaction-diffusion system parameters must be chosen to be close to the values given in the left column, otherwise the system will not generate a soliton structure. You can experiment by altering the provided values and pressing “run” to see the outcome. When finished you may reset the simulator by pressing the webpage reload button on your browser.
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Simulations

Computer Simulation Gallery A series of simulations of the Model G reaction system Simulations carried out by Matt Pulver.     Particle Creation 3D simulation showing a subatomic particle forming from an X potential ZPE fluctuation This is a one-dimensional cross section of a spherically symmetric particle extending radially in three dimensions.   Simulation parameters: Reaction volume radius = 50 …
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    The Starburst Foundation is a nonprofit research institute based in Schenectady, New York and Athens, Greece.
    It was incorporated in the state of Oregon in January of 1984 for the purpose of carrying out scientific research and public education directed to the betterment of humanity and the planet. The Foundation’s research activities are carried out with the intention of:

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  • Latest News

    The Generation of Mega Glacial Meltwater Floods and their Geologic Impact

    A new theory explains how mountain-sized waves of glacial meltwater could have been produced during the last ice age. In a paper published last month in the journal Hydrology: Current Research, Paul LaViolette describes how immense waves of glacial meltwatercould have been produced on the surface of the North American and European ice sheets during periods of excessive climatic warmth when the ice sheet surface was melting at an accelerated rate.
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