water-bearing rock

Gas companies say it is in those first few hundred feet where the borehole penetrates water-bearing rock.

Water-bearing rocks proved difficult to excavate, which meant freezing techniques had to be used.

The borehole extracts rain water which falls through the grounds into water-bearing rocks.

It was deduced that the dowsing method could produce water-bearing rocks more quickly than could conventional methods.

The water-bearing rock.

Here an Afghan Cameleer reportedly lost his life whilst innocently bathing in the only water-bearing rock pools for many miles.

Theories include the melting of near-surface ice, absorption from the thin Martian atmosphere, and seasonal discharges from local aquifers, layers of water-bearing rock.

Layers of porous and permeable limestone create water-bearing rock and soil that affect the climate, weather, and hydrology of South Florida.

The main water-bearing rocks are those of the Tarango formation and associated alluvia and the Cenozoic sequence of fractured pyroclastic and lava flows.

The Worsley Four Foot mine was reached in April 1910 and more water-bearing rock was anticipated before the Arley mine was reached.

Surtseyan eruptions can happen on land as well, and are caused by rising magma that comes into contact with an aquifer (water-bearing rock formation) at shallow levels under the volcano.

The village is in a region which is underlaid by a large porous water-bearing rock structure called the Magnesian Limestone aquifer, which dips downwards to the east.

The gas fields are considered by some a safer choice than current experiments under the the North Sea and the Sahara Desert where a water-bearing rock layer, or aquifer, is being used.

Underground thermal energy storage (UTES) uses permeable, water-bearing rock formations called aquifers—or, where aquifers are unavailable, a network of plastic tubing inserted into boreholes drilled into the earth—as underground storage areas for water.

The main water-bearing rocks of these sequences are the upper units of the Guadalupe group (particularly the Areniscas de Labor and the Areniscas Tiernas), with a total thickness of about 160 m, and the sandy lenses of the La Sabana formation.