WATER SHORTAGE HOAX EXPLAINED – What is “primary” water? Interview with Dr. Stephan Riess in 1985 |
WATER SHORTAGE HOAX EXPLAINED – What is “primary” water? Interview with Dr. Stephan Riess in 1985 | Menu Skip to content NEW POSTS Primary Water WATER WARS LINKS VIDEOS StopTheCrime.net WEBSITE WITH MORE INFO digigod digigod WATER SHORTAGE HOAX EXPLAINED – What is “primary” water? Interview with Dr. Stephan Riess in 1985 This video is a must watch for anyone concerned with the question is there really a shortage of water in California, and elsewhere? According to Dr. Stephan Riess and many others there is NO Shortage of Water. Primary water is plentiful and renewable. Watch this rare interview to find out more. After watching this go to www.PrimaryWater.org and HELP spread the Water Action Alert – 1/2 page double sided flyers about the REAL science of water – hand them out far and wide . . . Be part of the SOLUTION! What is Primary Water? 1985 Interview with Dr. Stephan Riess. You tube link: http://youtu.be/r3_HUTvPmDk Dr. Stephan Riess in 1985. TRANSCRIPTION OF YOUTUBE: 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. Ross Frazier: The water here is very pure water, isn’t it? Dr. Riess: It’s exceptionally good. It’s usually about one-third of the mineral content of the prevailing Colorado River water. Ross Frazier: This is because you’re extracting primary water from very deep. Dr. Riess: This is because it is primary water obtained below the crust and is in the non-oxidizing zone. Ross Frazier: So this is not being oxidized? Dr. Riess: No. Ross Frazier: And it is not picking up contaminants. Dr. Riess: It does not dissolve or pick up any contaminants and therefore it is superior water. It does not need any more cleaning or pre-treatment for the distribution system. Ross Frazier: And you don’t have any, or very little if any, radiation? Dr. Riess: Well, there may be fast dissolving radon which is about one day lifetime in the water in the reservoir. Ross Frazier: And radon will not be a really factor here. Dr. Riess: No, it is no factor at all. Ross Frazier: Because it’s decay is so rapid. Dr. Riess: Right now. And in itself is not very serious. Ross Frazier: It wouldn’t be anywhere near the contaminants that could be picked up as a result of surface testing of nuclear weapons. Dr. Riess: Naturally, that is the point. When they are talking about claiming waters, bad waters, which are already bad at the origin from the faucet and then going to the industrial and whatever uses there are and then go through the sewage lines, the retreating is absolute insanity. Ross Frazier: It is not necessary because . . . Dr. Riess: It’s ridiculous. An article that I got in the paper here before me today is talking about treating two hundred million gallons of sewage for re-use. Now who in the Devil would want to use sewage water again? Ross Frazier: It’s unnecessary. Dr. Riess: Absolutely unnecessary. Ross Frazier: Your water supplies literally are limitless. Dr. Riess: Naturally, they’re limitless. They claim that the water is from the surface seeped in over long periods of time into the rock structure. Itself an impossibility. Absolutely. Ross Frazier: It didn’t go down through impervious rock. Dr. Riess: Neither below the zone of oxidization. The pressure there is too high for water to continue. Rock is twice the pressure or the weight from water itself. And water is incompressible. Absolutely incompressible. Rock is more compressible than water. This is the standard knowledge that we have had for a long time. Ross Frazier: Incompressibility of water has been known for many years. Dr. Riess: That’s why it is used in the industries for pressure checking. And to talk about reclaiming water from sewage use for public demand, why it’s ridiculous. Absolutely unnecessary. Absolutely. Ross Frazier: So that the water, even the best water, can be obtained out of the water cycle, is by all standards poor grade water related to the water that you are finding below the surface of this granite. Dr. Riess: That’s right. Once the rainwater hits the ground it immediately starts to absorb contaminants. Always Ross Frazier: All the soluble elements that can be absorbed will be absorbed into it. All the contaminants that the precipitation washes out of the atmosphere on the way down through to the earth. Dr. Riess: Absolutely, absolutely . . . and accumulates. It’s the rub of it. Ross Frazier: Now as a health matter, for public and personal health, water is absolutely an essential ingredient for health, isn’t it? Dr. Riess: Not only that but for the existence of life on the planet, whether it’s animal life, human life or vegetation. Ross Frazier: But all the water that is on the planet at the moment that fills the oceans ultimately, or primarily, has been generated from the source that you’re finding now. Is that not so? Dr. Riess: All the water that is now coming to the surface by deep well drilling may be a million years underground old. Ross Frazier: And the salinization, also the complexity of sea water, is the result of soluble elements being taken out of surface water and being washed into the ocean. Dr. Riess: Which had to come into the ocean by run-off by rain. It couldn’t be there any other way. No question about it. Ross Frazier: That is referred to generally as cycle water, or water that has gone through the evaporation, cloud formation, precipitation and the flow back into the ocean via the rivers. Dr. Riess: Why science, and the teaching today of science has ignored the presence of about 1,500 big wells or springs in the world that go from 10,000 to 200,000 gallons a minute constantly . . . Ross Frazier: Back into antiquity. Dr. Riess: Way back, and are actually 8,000, 7,000, 500, 9,000 feet elevation usually in the granitic system. It is not explained. We have two wells in America, or springs in America, that produce 800 million daily. One is in Missouri and the other is in the desert in western Oregon. The one in Oregon, the western desert of Oregon, is producing the Day River. So, where did it come from? If that was rainwater, all the rain in the state of Oregon on an annual precipitation wouldn’t flow that spring one month a year. Ross Frazier: That river (the Day River) flows twelve months a year. Dr. Riess: Yeah. But it’s flowing twelve months, yeah. Dr. Wayne Weber: We talked a little earlier about some of the chemical differentiations and compositions of the rock involved with the specific location of the wells that you’ve been drilling. Can you elaborate on that a little more? Dr. Riess: Right. The main thing is if you study your structure. If you have volcanic debris from the earlier tertiary period maybe, or even earlier, like here in this country, this here is 50 million years old before it came out of the ocean. There we have contamination produced by the decomposition. The minerals fall apart. They dissolve. Whether it is copper, lead, zinc, or whatever the minerals are, aluminum, they get into the ocean and then you find them all in the water where there is high chlorine you get a high chlorinated water, and often so bad, it is absolutely unusable. But in every event it is very, very damaging to human life, to plant life, and harmful. Dr. Wayne Weber: You’re speaking in terms of ground water at this point? Dr. Riess: Yes, ground water. But when you go and consider those very big, deep sources of water, usually coming in as springs on high mountain systems worldwide, and usually are a lake, and a big lake at times, then we end up dealing with something that could never come from the precipitation cycle because it just isn’t available. Never was. You can’t get precipitation water on a steep mountain range more than about one inch of water per foot of land. And if you have a ten inch rain you have about ten inch of every saturated ground. Then it is all over because there’s nothing going down below twenty or thirty feet. Ross Frazier: Certainly not your impervious granite. Dr. Riess: Not even through the soil. Ross Frazier: Not even through the clay. Dr. Riess: No. Couldn’t. It’s impossible. Ross Frazier: So it runs off on the surface and picks up more contamination as it goes. Dr. Riess: And out she goes into the ocean and that’s the damn trouble that they are getting it here when it’s damaged and ruined if they drill it with very shallow holes. If that rain water gets off and gets into the valley, through highly porous sand and gravel, of course it sinks, and they call that the water table, which it is. Ross Frazier: It sinks through bedrock but only to the top of bed. Dr. Riess: Just the basin. It’s basin water. That’s all there is to it. And it is accumulated for centuries. Now we are pumping it away at about nine times the rate of precipitation. And it is ridiculous. I’ve seen a report here today in the paper where they’re talking about treating 200 million gallons of sewage daily in this county. Ross Frazier: Yes, you mentioned that before. Dr. Riess: Yes, well there it is in the newspaper. Dr. Wayne Weber: As opposed to the system of the ground water in the ground water table, we were speaking earlier also about the water coming from the earth in the form of steam as you mentioned earlier, and you had indicated that as this comes in the form of steam, basically condensing. And so it condenses and comes up through the fractures at that point. Could you elaborate a little bit more on some of the other chemical changes that occur as the steam is coming up and the water is clearing itself. Dr. Riess: The steam generally reduces one percent of its volume to a heavy moist condition of heavy saturated air and then it usually is locked in with the metals and the minerals and remains there for an unexplainable length of time. But eventually it is liberated . . . the whole system. Eventually the water will dissolve any substance on this planet, no matter what it is. Everything is soluble whether it is land, rock, gold, silver, metals, whatever, it will dissolve it. That’s all there is to it. And then you have it in solution. You can analyze the sea water right now and you will find practically everything in it that we have in form of solids. Ross Frazier: Every soluble element is in sea water, virtually. Dr. Riess: There’s no question about that. But, on the other hand, if you then recognize that photosynthesis, which is just plant life, the grasses, the trees, everything that is green and living consumes 600 billion gallons daily worldwide, that’s enough water to empty the last gallon of water in the ocean in less than 3 million years. So what about the rest of it? Ever since the tertiary period, 15-16 million years ago, the ocean has raised by one-third of its total capacity. Ross Frazier: As a result of production of this primary water which you are now extracting. Dr. Riess: Damn right. It is breaking out and it is showing up. I have a record of 915 springs and they go over 10,000 to 200,000, and a larger proportion of them, some of them go into the millions of gallons daily. And usually springs are at the high point of the mountain range. Not in the canyons. Dr. Wayne Weber: Have you ever done any analysis of the type of structures where these springs are located. Dr. Riess: Oh naturally. I’m locating them on this basis. If I know that crystallography and mineralogy, then I know that I can depend on that good water on drilling. Dr. Wayne Weber: And the crystallography and the mineralogy would indicate to you which areas are contiguous with what would go into the magma. How does that relate, for example, if you have a dyke, are springs usually connected to a dyke? Dr. Riess: Always on a contact zone whether the dyke has surfaced or not. But it has to be a surface zone. Now the point is, what people ignore, I can go over a thousand acres of land, say a whole section on these ranges (mountain ranges) and I find variations from 5 to 10 different variations within one mile, mineralogically and petrographically. The ordinary person doesn’t even recognize it. Dr. Wayne Weber: Are you talking about surface structure or actual dyke structure. Dr. Riess: Dykes. There I can determine directly whether I have contact to the magma. The water has to come from the magma. Dr. Wayne Weber: But because of the mineralogy and petrology of the dyke then you can say this indeed is something that is in contact with the magma. Dr. Riess: Yes and the metals contained therein. In an analysis of what minerals are involved. Dr. Wayne Weber: Primarily the sulfite group. Dr. Riess: Then I know I’m right and I can dare to drill a well and expect some really good water. Dr. Wayne Weber: So you might have a situation where you have one dyke here and another dyke over there and the mineralogy would be different enough that one would have water connected but not the other. Dr. Riess: Yes. Not a hundred feet away on the other side of the dyke. Dr. Wayne Weber: In general would you see one dyke connected to water here and other dykes in close proximity that are not connected to water. Dr. Riess: Yes. I would say there are water flowing or water containing dykes and non-water containing dykes. The dyke itself doesn’t have the water but did at one time and are carriers. Mineralization produced the water as the mineralization intruded. Say a pound of copper or a pound of zinc might have had millions of gallons of water depositing it. Millions. Read that book from Saltzman. We had figured out how many gallons of water it takes for one pound of borax. Borax is an unknown element prior to 50 million years ago. And the biggest deposit apparently has been Kramer, Colorado. But that is tertiary. That’s the latest mineralization on this planet. Dr. Wayne Weber: So if you have a dyke that you feel is a water former because of the rock analysis the reason that water is still coming today is that it is still in direct contact with the magma but that would generally be somewhere 1,000 or 2,000 feet down. Dr. Riess: Oh sure. Twenty, fifty. Dr. Wayne Weber: How do you know that you have a dyke here with the proper mineralization . . .? Dr. Riess: By the debris. By what the debris is showing on the dyke. That’s the mineralogy of it. Dr. Wayne Weber: I understand that. But once you have that, how do you decide then and what is the basic principle that you are going on as to how to get water from that dyke or near it? Dr. Riess: What is the other side of the dyke analyzing? Maybe ten feet away and I’m out of it. I’ve got to follow the contact zone whatever the incline or dip is. Dr. Wayne Weber: And then you would drill the well, for example, you have a dyke coming in from ninety degrees right here. Dr. Riess: If the dyke shows here (at the surface) it doesn’t mean a thing, I have to drill (pointing at Wayne’s elbow) here (high above the lower angle of the dyke deeper under the surface). Ross Frazier: Because here (showing deep below the surface) is where your fracture zone is. That dyke is here because there was a fracture of the granite plate. The displaced fractures are in the elbow and not in the Dr. Riess: It’s a displacement fracture. Ross Frazier: Those fractures are allowing that steam which is creating the water coming up from the magma to be there at all. Dr. Riess: That’s the passage way. The steam is way below. The steam is five to ten miles down. Ross Frazier: But the steam is the pressure that keeps the water up in those fractures. Dr. Riess: Right, right. Ross Frazier: The bottom pressure is continuous. This is a continuous process. It doesn’t have any end to it, does it? Dr. Riess: No, no. Science is slowing admitting it. There are 28 universities now petitioning the government to put up eight million immediately to start drilling 15,000 foot holes to capture the steam. The steam means not a damn thing. Ross Frazier: But their saying and admitting that there is steam there as primary steam, but they are denying that it is primary water. If I’m not incorrect, steam is water in another form. Dr. Riess: Naturally. Ross Frazier: We’ve been saying this for forty years. Dr. Riess: Since I came out of school. Ross Frazier: Now in connection with your work in the mining field, you found virtually invariably that when you got to a certain depth in these deep mines that you would hit this water that you’re describing and it would flood the mine out. That’s one case when you didn’t want that beautiful primary water. Dr. Riess: That is correct. Ross Frazier: Because it was destroying the whole operation. Dr. Riess: I learned what to look for not to tap caught in it. Ross Frazier: Yes. And you learned that that water was perfectly usable because I understand that at one time you carried some of it for the camp cook and he was astonished at how … truncated (36,539 more characters in archive)