This, an excellent interview with Dr. Stephen Riess from 1985 on Primary Water, is important enough to warrant reposting here:
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WHY WE DO NOT HAVE A WATER SHORTAGE: WE HAVE PRIMARY WATER
WHAT IS PRIMARY WATER?
1985 Interview with Stephan Riess – YouTube Transcription
The Primary Water Institute and Primary WaterWorks Present Dr. Stephen Riess on Primary Water
The Last Interview September 22, 1985
With Dr. Wayne Weber and Ross Frazier
In Escondido, California
The term Primary Water was coined by the late Dr. Stephen Riess, the geophysicist who independently discovered its existence and pioneered its development, beginning in the 1930s until his death in December 1985.
“My discovery was put to a field test by locating and drilling many wells. The records to date from these tests is 70 producing wells out of 72 attempts, all drilled in hard rock, all located in distressed areas generally considered unproductive.” (Dr. Stephen Riess, 1954)
Primary water is a little known renewable resource that originates deep within the earth. When conditions are right, oxygen combines with hydrogen to make new water.
This water is constantly being pushed up toward the surface under great pressure. The water finds its way towards the surface through fissures or faults. Depending on the geology, primary water can be accessed close to the surface, or even flow out as a spring.
Primary water has never been a part of the hydrologic cycle until it finally arrives at the surface. Traditional hydrologic cycle water is finite and volumes fluctuate relative to available rain and snowmelt.
Primary water is renewable and plentiful regardless of the weather.
This priceless interview from 1985 of Dr. Stephen Riess is presented in its entirety regardless of camera movement and colorful language. Meaning of Dike or Dyke in Geology:
https://en.wikipedia.org/?title=Dike_(geology)
A dike or dyke in geological usage is a sheet of rock that formed in a fracture in a pre-existing rock body. However, when the new rock forms within and parallel to the bedding of a layers rock, it is called a sill. It is a type of tabular or sheet intrusion, that either cuts across layers in a planar wall rock structures, or into a layer or unlayered mass of rock.[1]
Ross Frazier: This is Escondido, Sunday the 22nd of September 1985 and we’re
taking instruction from Dr. Stephen Riess, an eminent earth scientist at his home
in Escondido, high on a rock promontory overlooking the valley and showing
massive protrusions of granite boulders all around. Stephen Riess is a very
controversial scientist and has extensive knowledge worldwide in the finding of
water.
Turning to address Dr. Stephen Riess . .. Do you have any immediate finds in
Escondido in the last three or four months?
Dr. Riess: Yes we’ve been successful in drilling some very good wells and it
happens that both locations are on the highest parts in the county. A thousand
feet higher than the pump stations for the water supply from the water resources
department. And the cost of pumping it from there, these stations, the river
water from Sacramento up into these reservoirs here is $93 an acre foot in power
bills and it is poor quality water. So the point now is that this water wells can
produce the water for $20 pumping cost instead of $93 to lift it from the pipeline
below up to the surface.
Ross Frazier: And with no carrying of silt or anything of that nature.
Dr. Riess: No. It’s clean water.















