What is Primary Water? 1985 Interview with Dr. Stephan Riess

What is Primary Water? 1985 Interview with Dr. Stephan Riess
Published on Jun 19, 2015
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This is a very important interview of the late Dr. Stephan Riess from 1985 about primary water. For more information, please visit thewww.primarywaterinstitute.org andwww.primarywaterworks.com.
TRANSCRIPTION OF YOU TUBE VIDEO: WHAT IS PRIMARY WATER?(see attached)
Titles: The Primary Water Institute and PrimaryWater.org
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.
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?
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The Garlock Project – Drilling for Primary Water in the Tehachapi’s

History
Pal Pauer’s mentor Hydrologist and Mining Engineer Dr. Stephan Riess was convinced that the primary water source for California City (California) originated from the Garlock Fault. His dream for testing his hypothesis materialized whenPal Pauer drilled two test boreholes adjacent to the Garlock Fault in the Tehachapi Mountains at a 6,000-foot elevation. The outcome is remarkable!
Timeline
April 15, 2015 Primary Water Institute (PWI) founder Pal Pauer (Pal) was approached by clients for a feasibility study for locating several primary water wells on their property. They provided topographic maps and approximate desired well locations. Pal determined the project was feasible.
July 4, 2015, Pal made a site visit to the Tehachapi Mountains to verify the information provided on the maps. Pal spent one week on site investigating viability and likelihood of primary water at this elevation (6,000 feet). He found a vent or fumarole which was adjacent to the fault and represented a site favored by the property owners. Consequently, the owners and Pal determined and marked locations for 2 wells on the property. Further investigation and drilling test boreholes was the next step.
A search ensued for a suitable drilling rig to make the project possible. Several drilling firms were considered and it was decided by the property owners and Pal that Paul Hern Drilling Inc. had the knowledge and equipment that could drill the wells. Note the state of the drilling rig.
Dec 6 2015, a trip was made by Pal from his home in Oregon to the Tehachapi’s to over-see the project.
Dec 8 Arrived on client’s property to start drilling
Dec 98:30am, drilling begin on site. The first test well was named Maryanne 1. A highly fractured meta-volcanics was encountered at 20 feet which led to the probability of water. Further drilling into the structure where large fractured material was ejected under air pressure along with an ever increasing quantity of water. Work had to be stopped about 100 feet in depth due to the lack of availability of air volume and pressure to remove debris and water. It is estimated that the water that was ejected from a 7-inch diameter borehole was at the rate of 800 plus gallons per minute. Further progress could not be made with available volume of air and pressure. It was determined that water was very good quality between 150 to 250 PPM/L – total dissolved solids (TDS).
The drilling rig was moved to the second well site named Heather 1. This location is part of the same rim of the vent/fumarole that is estimated to be between 2-5 feet in width.
Dec 10, approximately 100 yards across from first site, the same procedures were followed and water was encountered in larger quantity at a 60-foot depth and drilling could not proceed any further due to inability to remove water/cuttings and debris.
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