M-state / Ormus or mono-atomic Minerals were actually being studied in the Soviet Union as early as 1973. In fact, the then Soviet Union was far ahead of the rest of the world in researching water and salt and had already revealed that monatomic minerals were found in sea water and other sources of mined salt.
It was only a couple of decades ago that an American farmer, David Hudson, accidentally stumbled upon monatomic gold and other monatomic elements after dousing his fields with sulphuric acid to loosen the mineral salts in his soil.
David Hudson coined the term ORMEs (Orbitally Rearranged Monatomic Elements) to describe the strange white powder, incapable of being perceived by the mind or senses, which comes from gold, platinum group metals, and other "transitional" metals.These "transitional" minerals have not yet "transitioned" into the usual atomic structure characteristic of metallic minerals.The electrons in mono atomic minerals exist in what is called a "high spin state".
Science refers to these minerals as "exotic" matter, not yet known and not shown on the Periodic Table of Elements.
However, new physics indicate that the white powder may not be mono-atomic, but diatomic, or small cluster "condensates".
With this, we generally refer to these elements as ORMUS or "M-State" elements. Analysis of m-state elements has disclosed that their physical weight can be decreased to a negative value at specific high temperatures.
While there appears to be many "free" sources of monatomic elements in this world in many of our natural "soil grown" fruits and vegetables, the most potent sources are available in glacial rock dust, volcanic rock dust, and Original Himalayan Crystal Salt, which is essentially rock dust in an altered crystalline structure.