Geological Faults:
Movements to the continental tectonic plates, which make up the outer shell or crust of our planet, also affect the Earth's energy field. As the plates move apart, slide past each other or move together, there is a great crushing, buckling or heaping up of material which results in discontinuities such as faults, thrusts, fractures and fissures not obvious at the surface but buried deeply below. These movements create more energy all the time and are especially large when earthquakes occur. These faults also occur on a smaller base due to geological ‘creep’ as all matter including rocks are in a constant state of movement. The British Geological Society's Solid Geology Maps mark out most of these localized faults, which can be from a few yards to several miles long. Mounting pressure within these faults can effect the electrical field of mineral deposits especially quart bearing rocks (piezoelectricity) and ironstone, some will produce their own energy particularities especially at sites where they form an outlet for radon gas and other high particle energy. The pathways of these energies are really deflected and run through nearly all materials and can add to the geopathic stress of a building.