What Is the White Powder?

What is the White Powder?

The "white powder" is comprised of a group of elements in a

monatomic state. David Hudson calls them "ORMEs" for

"orbitally-rearranged monatomic elements." This is a new

phase of matter with entirely different physical properties

from normal elements. Conventional chemistry texts have

been of little value in explaining ORMEs. Hudson explains

the concept in his video tapes. However, there are ambiguities,

unclear statements, and contradictions among his various videos.

The intent here is to establishment a common baseline

document on which further discussions can be focused. You

are encouraged to contribute to it.

ORMEs are naturally occurring in certain volcanic soils

dating back to early geological events. Such soils are

prevalent throughout the western United States. Soils

which are considered rich in these elements might contain

up to six percent of this material. The remaining 94 percent

or more of the material is ordinary dirt comprised mainly

of silicon compounds. Initial processing consists of removing

the dirt to get the residue. The residue comprises ORMEs or

the "white powder."

Because of the unique and valuable physical properties of ORMEs,

there has developed a desire to produce them from the metallic

form of the elements. In other words, there are reasons to

convert metallic precious elements to ORMEs. Hudson has found

ways to do this although he reports that the cost of doing so is

prohibitively expensive. The reason for the high cost is due

principally to the high, per-ounce cost of most precious metals.

The process itself is tedious but is not particularly expensive.

But it is much less expensive to start with natural material and

to then "simply" remove the ordinary elements from the natural

material to get pure ORMEs matter.

Because the percentage of ORMEs in certain volcanic soils is so

high (up to 6 percent) in comparison with normal high-grade ore

(up to 0.0015 percent), there is considerable interest by mining

companies in the technology required to convert ORMEs to their

metallic form. The yield increases by a factor of 4000. So far,

no mining company has figured out how to do this. The processing

technique is highly proprietary and will not be disclosed,

according to Hudson. Hudson has stated that his sole interest

is in the monatomic form of these elements; he has no interest

in producing the metallic form of the precious elements. Further,

Hudson states that there is never a need to convert monatomic

materials to their metallic state during the manufacturing process.

The only time a conversion is required is to allow standard analytical chemical procedures to be used to identify a small sample of the material.

Hudson further states that he has the technology to separate the

monatomic material into the various elements for specific

commercial applications without conversion to the metallic state.

That is, he can produce the white powder of gold, the white powder of palladium, the white powder of osmium, etc without conversions. He also stated that the white powder which will be delivered to the

members of his spiritual