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Spirit “I have been at work for some time building an apparatus to see if it is possible for personalities which have left this earth to communicate with us, It would account, ... for differences in moral character, ... [and] behind changes in a person’s personality in the course of his or her lifetime. Introduction Last Updated: July 31, 2021 Psionic Circles is all about the development of the self through all vehicles of psyche and technology where no subject is barred. Therefore it is only fitting that we look at some of the technological advances surrounding communications of all types including the dead. We first ask ourselves what does it mean to be dead? Does it mean that we find ourselves in Heaven, Mecca, or perhaps Valhalla, if we are good, loyal, or valiant? Or does it mean that our physical bodies are buried, or cremated and then laid to rest, never to be seen again? Here you have your personal belief, or perhaps more appropriately identified as your soul's religion. And does any of these belief systems leave room for the living's ability to communicate with the dead? Lets take a small step back for a minute and identify why we have assumptions (beliefs) about death and the Afterlife Kingdom. Throughout history, our greatest fear has always been death. People live, they grow old and then they pass or and die. It has been assumed that after death we can't see them, associate with them, or speak with them. Unless you believe in Spiritualism along with its movement and visit a Séance to find out how your late husband (Ivan) is doing, is he happy? Or your might communicate with your Great Grand-mother, Gilda, about the location of some lost bars of gold that she meticulously hid from a would-be thief, only to have forgotten where she hid it at dementia's age. Perhaps, there is another way to communicate with your beloved... Thomas Edison one of the greatest minds of the 20th century, Master of "Electronic Communication", and one of our favorite Geniuses, sought to bring light into… -
Administration According to scientist Planet Earth is over 4.5 billion years old. In its beginning it consisted of a multitude oi gases and dust particles and particles. Initially these particles bonded through electrostatic forces. The next phase Last Updated: July 30 2021 Introduction to Rocks and Crystals In the Beginning... Our sun and earth had very similar beginnings. The sun started out as a vast array of gaseous and particles. These particles formed elemental hydrogen. Then within the sun countless collisions occurred between hydrogen atoms creating all of the elements of the periodic table of elements, along with the sun's gigantic mass. The Earth, origin, similar to the sun started as a swirl of gases and particles colliding with one another and growing in mass to form much larger particles. Then due to the disparity of these masses, eventuated as gravitational forces, forming elements, minerals, rocks and crystals each rising and sinking according to the differences in densities and heat. They organized themselves in four distinct levels of strata throughout the Earth from the center out to the crust. The four main layers are the inner core of Earth, followed by the outer core, then the mantle, and finally the crust at the Earth’s surface. Layers of Earth As was mentioned there are four distinct layers of the Earth. The inner core which is made of the metals iron and nickel which is an exceedingly hot ball of molten rock. And so, as the heat pushed the molten rock outwards it quickly created and then moved the silicates, water, air and a host of other minerals to the exterior of the earth forming the next planet level, the mantle. The mantle is made up of solid rock that is also extremely hot that is not completely molten. The heat generated from the mantle is the root cause of the movement, convection, occurring and is responsible for volcanic and seismic activity throughout the earth, at its surface and the exposed mantle on the ocean floor. The final level of the earth is the crust, which is a cold, thin, brittle…Psionic Crystals
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