Deep Seated Water Illustration Explained

Global water management strategies are missing a key component in their planning and water conservation models, resulting in overdrawn surface water supply sources such as endangered rivers and depleting shallow ground water resources. A century of innovation and scientific discovery indicates there may well be a set of pathways that can lead to natural, sustainable abundant water.

Shallow water is a part of the hydrologic cycle, which is water evaporation – clouds, rain, water runoff — surface water. Shallow water is an open system, draining into ponds, lakes, rivers and eventually into the oceans. Part is evaporated into the clouds, dropped as precipitation, and the process continues. Part seeps or infiltrates into the ground from the surface, contributing to the recharge of shallow aquifers. Shallow water is also called a water table aquifer, open to the atmosphere, interchanging at one atmosphere of pressure. That is why one needs pumps to access shallow water.

Shallow wells are wells intended to access the water table aquifer. In early days, they were developed by hand pumps, nowadays by more sophisticated water pumps. The depth of a ‘shallow’ well has no fixed definition. Its depth can be from as little as 25 to 50 feet down to several hundred feet, in desert environments, for example. The main characteristic is that no matter the situation, that layer of water is open to the atmosphere.

An aquifer is a sub-surface layer of water-bearing permeable rock, rock fractures, or unconsolidated materials. Any of these three can carry or store water. An aquifer can be confined by impermeable rock or clay, which is called an aquitard. Or it can be unconfined, taking in or passing water along through a permeable stratum, such as sandstone, gravel, or fractured rock. Fractured-rock water-bearing fractures can be horizontal, vertical, diagonal, or combinations of the three. A horizontal aquifer contains water all from one level. A vertical or diagonal aquifer may itself go quite deep, or connect with other fractures that go deep, and, therefore, access waters deeper than shallow water, or underlying a shallow water aquifer. There can be multiple layers of aquifers, separated by aquitards, such as clay and impermeable rock. These step down in benches or successive layers of permeable zones. The waters found in each bench or zone are separated by aquitards and are distinct from each other.

The shallow, unconfined aquifer is easily contaminated from surface sewers, pipeline breaks, spills from various sources, seepage from mine tailings, agricultural runoff, etc. Therefore, it is common in shallow wells to add a borehole casing to try and protect the well water from such contamination.

A deeper aquifer implies water that is not only to be found deeper, but also sometimes is separated from the hydrologic cycle. The sources of deeper aquifers can be rock-fracture systems, ranging from close to distant, or deeper sources of water, such as contained fossil (or old) water systems. Fossil water is a buried water system, which was once part of an active hydrologic cycle but has over geologic periods of time been buried. One example is the deep Pleistocene Era lakes to be found in the Agustin Plains of New Mexico (Gila River). Another source of fossil water may be ancient ice sheets, such as the fresh water discovered buried offshore of New England. Fossil water can be found at varying depths, from hundreds of meters, to a few thousand, to many kilometers deep, such as the ocean-like aquifer under the Xingjiang’s Tarim Basin, China, containing reputedly ten times more water than the total of America’s Great Lakes. Although the Tarim Basin aquifer is saline at thousands of meters, there are other more shallow locations where huge fossil water aquifers have produced fresh water, such as the Nubian Sandstone Aquifer System in Libya (in the latter case the water being meteoric (originated by precipitation.)

All rocks have a varying degree of porosity and permeability. Some rock formations contain a great deal of water. Sandstone, for example, has both high porosity and permeability. Clay can contain water and may have low porosity and virtually no permeability. Connate water is formed when layers of deep water-bearing rock undergo the process of lithification (the transforming of sediment or other material into stone), and under great pressure the water is driven out of the rock. Both fossil and connate water could be contributing sources for deep aquifers.

Sub-surface inflows and outflows are inter-basin or cross-basin flows. Deep aquifers quite distant from one another can communicate through faults and permeable zones, volcanic lava tubes, fissures, etc. Water precipitated into the fractured rock systems of mountains can infiltrate deep and flow through gravitation and other pressure to come out in seeps, springs, and artesian wells far distant from the source. Such spring or well water can only be associated with specific distant sources through sampling and chemical analysis. These sources are usually long-lived, having viability over thousands of years and hundreds of miles. If you have an artesian well or water spring, you may not be easily able to identify its source or sources. Paleo-rivers or buried river valleys may contain water in the alluvial sands and gravels which were buried over geologic time, resulting in ‘river formations’ deep underground.

“The water cycle involves more than just the water that circulates
between the atmosphere, oceans, and surface waters. It extends
deep into the Earth’s interior as the oceanic crust subducts, or slides,
under adjoining plates of crust and sinks into the mantle, carrying
water with it. “
Steven Jacobsen, PhD.
Northwestern University

H20 production is the creation of new water, bringing new, non-atmospheric water to the surface of the earth. It can rise from many sources. Magmatic water deep in the continental crust can rise literally all the way from extremely deep pockets of molten magma four hundred or more miles below the earth to the surface in volcanic explosions, which release huge amounts of ash, gases, and water vapor. Magmatic water may be released more gradiently through thermal springs and seeps, as is found across Iceland. Connate is another productive source of water, as it stems from the original water content of rocks, squeezed out in the process of lithification under pressure and heat. Fossil water is trapped water buried at depth, such as Pleistocene ice sheets.

“The components of water (your classic hydrogen and oxygen) are trapped
inside the molecular structure of minerals in mantle rock, embodying a fourth form of water that is neither liquid, ice, nor vapor…The water in the mantle, which could equal the amount of water in the world’s oceans, may be an integral part of sustaining water on the surface.”
Joseph Smith, PhD.
University of Colorado, Boulder

Deep Seated Water™ (DSW) is a coined term that can be used to identify water originating from deeper sources, such as suggested in the paragraph above. It should be chemically distinct from local shallow ground water and likely be older than surface water. One study suggests that water low in Total Dissolved Solids (TDS) at 3.6 km depth could be attributed to water produced under great pressure during the conversion between clay types. Another paper, analyzing waters deep in the Delaware Basin in the southwest U.S. found similar low TDS and also attributed this to clay conversion under high pressure. In the latter case, chemical and isotopic data precluded that the water source was meteoric.

“Conventional wisdom tells us that the salinity of pore water increases
with depth, becoming fresh to brackish to multiple times the salinity of
seawater…There are major exceptions to this rule.”
Jean-Philippe Nicot
University of Texas, Austin
Bureau of Economic Geology

Deep-seated water (DSW) is just such an exception. In fact, depending on variable sources and different pathways, DSW wells might be expected to produce fresh, high-quality water. Identified and located through the application of high-tech elaboration of remote satellite and other data, DSW can be accessed via water-bearing rock fractures communicating with any of various deep sources of water. Such fracture systems may interconnect, providing pathways for water up to or very close to the surface.

Arlin Howles
Chief Hydrogeologist


“Hydrogeologic Study of the Plains of San Agustin and the Alamosa Creek Valley,” New Mexico Bureau of Geology.

“Water discovered deep below the earth’s surface,” Steven D. Jacobsen, Joseph R. Smyth, USA Today, June 2014.
“Water discovered deep beneath earth’s surface,” Science.

Earth’s Deep Water Cycle, Edition 1, Steven D. Jacobsen, Suzan van der Lee, Geophysical Monograph Series, Vol 168, American Geophysical Union, Wiley, 2006. (An excellent collection of scientific articles on the subject of deep water.)

Arlin Howles: Professional Geologist (Texas), Certified Petroleum Geologist (American Association of Petroleum Geologists).

Salinity Reversal and Water Freshening in the Eagle Ford Shale, Texas, USA, Jean-Philippe Nicot, Amin Gherabati, Roxana Darvari, and Patrick Mickler, ACS Earth Space Chem. 2018,2,11 1087-1094 (Published Sept 13, 2018).

Origin of low salinity, high volume produced waters in the Wolfcamp Shale (Permian), Delaware Basin, USA, Jean-Philippe Nicot, Roxana Darvan, Peter Eichhubl, Bridget R Scanlon, Brent A Elliott, L. Taras Bryndzia, Julia FW Gale, András Fall, Applie Geochemistry, Vol 122, Nov 2020, 104771.

“Freshwater Two Miles Down,” Jean-Philippe Nicot, Researchers’ Corner, Bureau of Economic Geology, Feb 8, 2021,