We present this to you as found by us. It is presented in 4 (four) screen shots.
The Anonymous Poster shared where they had come to know this treatise of sorts on the purported hidden knowledge of “Porous earth / Inner Oceans”
Hello everyone. I’m not usually one to post here, but I’ve found myself captivated by a particular NHI theory/explanation/LARP on Reddit and I want to know if any anons can corroborate it. It was the first time I had seen mention of ‘ringwoodite’ in substantial fashion, but I could swear someone mentioned it here before. The reason I’m convinced of this is that this is a real material with actual scientific papers backing the basis of a “porous earth” which, at the very least, could theoretically support life. Whether this is actually where UAPs come from, I don’t know, but it’s all a bit too grounded in reality for my tastes. Link to the profile making these claims here: https://reddit.com/u/Nskxbehcidnsjx
odvr/s/OeBH4AYPUv And no, this is not me. I present it here because no one on Reddit does anything but doubt, while at least here people entertain such ideas. It lines up with that one green text speaking of “underwater bases” and so forth- I know people who will engage this thread know the one I’m talking about, I just don’t have it on hand.
Regarding exotic matter, the poster has this to say:
> Ringwoodite is key and I can’t really delve into why. Hopefully that starts taking more of a public stage and then I may be able to say more about it. It is not a solid, a liquid, a gas, or a plasma. It is for all intents and purposes capable of doing things to matter that aren’t natural on surface earth.
Wikipedia has this:
> Ringwoodite is a high-pressure phase of Mg2SiO4 (magnesium silicate) formed at high temperatures and pressures of the Earth’s mantle between 525 and 660 km (326 and 410 mi) depth. It may also contain iron and hydrogen. It is polymorphous with the olivine phase forsterite (a magnesium iron silicate).
> For experiments, hydrous ringwoodite has been synthesized by mixing powders of forsterite (Mg2SiO4), brucite (Mg(OH)2), and silica (SiO2) so as to give the desired final elemental composition. Putting this under 20 gigapascals of pressure at 1,523 K (1,250 °C; 2,282 °F) for three or four hours turns this into ringwoodite, which can then be cooled and depressurized.[5]Now the interesting part is that Ringwoodite can be loaded with hydrogen.
If that hydrogen happens to be heavy hydrogen, i.e. deuterium, then the setup becomes similar to cold fusion / LENR experiments (original Fleishmann-Pons experiment was deuterium in palladium).
