REGULAR WATER SURVEY
Dowsed Location of the optimum Drilling-Point / Site for a Tube-Well / Open Well over a suitable Hydrologic-Cycle Subterranean Water Vein (Stream). From the time the earth was formed, water has been endlessly circulating. Groundwater lies almost everywhere below the earth's surface. More than two million cubic miles of fresh water is stored in the earth, and half of that is within a half mile of the surface. Groundwater does not rest; it moves continuously, but at a snail's pace, from its point of entry to areas of natural discharge. Groundwater moves so slowly that its speed is measured in metres per day, and even per year. (Surface water velocities are described in metres per second.) Wells intercept some groundwater but most of it continues until it re-appears naturally in a spring or a seepage area and joins a watercourse.This circulation is known as the hydrologic cycle. Groundwater is part of this continuous cycle as water evaporates, forms clouds, and returns to earth as precipitation. The Process: surface water is evaporated from the earth by the energy of the sun. The water vapour forms clouds in the sky. Depending on the temperature and weather conditions, the water vapour condenses and falls to the earth as different types of precipitation. Some precipitation runs from high areas to low areas on the earth's surface. This is known as surface run-off. Other precipitation seeps into the ground and is stored as groundwater. Think of groundwater as water that fills the spaces between rocks and soil particles underground, in much the same way as water fills a sponge. Groundwater begins as precipitation and soaks into the ground where it is stored in underground geological water systems called aquifers. Rocks that hold water are termed aquifers and the best aquifers are to be found in sedimentary rock formations, as these are the most porous and therefore able to hold a large amount of water. The transmissivity (volume throughput) of water through sedimentary rock is rapid in comparison to less porous rocks. This property is crucial for aquifers that are used to supply drinking water. It allows the extraction of large quantities of water without depleting the long-term supply, because recharge of the aquifer takes place on a short timescale. Variences in porosity and transit times through the aquifer determine the quality or composition of dinking water. Analysis of any source of water will reveal varying amounts of dissolved minerals, and it is these that give the water its quality and taste. Very slow transit times lead to prolonged contact with the minerals inside the rock and therefore more are dissolved by the water. Very permeable aquifers will have very quick transit times and correspondingly the content of dissolved minerals will be low.
Survey Fee: Rs. 5000/- per Point/Site, to be paid in Full in Advance (i.e., Before the Survey), plus Transportation and Miscellaneous Charges.

GEO-THERMAL WATER SURVEY
Dowsed Location of the optimum Drilling-Point / Site for a Tube Well / Open Well over a Vertical Confluence (crossing) of Geothermal Subterranean Water (Primary Water) Veins flowing out of true main Water Domes. Primary Water veins are perennial, subterranean, streams that flow out from 'Water Domes' under pressure. Unlike hydrologic-cycle water, this is water that has never ever seen the light of day, and is formed and rises up from thousands of feet below the surface of the earth. It is not part of the hydrologic-cycle, nor is it part of the water-table. As the veins flowing with Primary water are not dependent on rainfall, and are not part of the groundwater-table, they neither dry-up nor reduce drastically during summer, or even during a prolonged drought.This primary water system exists deep inside the Earth as hydrated minerals. At shallower depths, this diffuse "steam-like" field of water gradually coalesces into pockets of liquid water which eventually connect into underground streams. The water travels upward in a vertical shaft called a "pipe" until its flow is stopped by an obstruction. This point is called a dome of water because the water is, in effect, domed-up. If fissures or cracks in the Earth are connected to the pipe, the pressure of the water pushes the water into the cracks, which then become what we call underground streams, or water lines, which can then travel for great distances under the Earth's surface. Their course through the ground is generally winding and non-linear. There is a difference between regular ground water and the primary water system described here. Ground water is part of the above-ground hydrological cycle involving evaporation, cloud formation, rain, rivers, oceans and the underground water table. Primary water is a totally below-ground hydrological cycle and therefore is not affected by drought. The Primary Water theory was first discovered, advocated and put into practice by world-renowned twentieth century dowsers like the late Henry Gross, Stephen Riess, and Verne Cameron of the United States. Primary Water can be found all over the world, including the desert areas, and even below the sea-bed.
Survey Fee: Rs. 15,000/- per Point/Site, to be paid in Full in Advance (i.e., Before the Survey), plus Transportation and Miscellaneous Charges.

 

N. B. Surveys are done on a 'Best Efforts' basis.  No Refund/s under any circumstances whatsoever,  please note. The Survey Fee DOES NOT INCLUDE any Guarantee from the Water Diviner that the Client will strike water when the Point is drilled. The Water Diviner will not be liable in any way in case of failure to strike water for any reason.