Assertion: aquifer's water | /r/HasProperty | fresh
Facets:
value: to saline
type: OTHER
value: relatively
type: DEGREE
value: to fresher
type: PURPOSE
value: along this line
type: OTHER
value: on the downthrown side
type: LOCATION
value: typically
type: DEGREE
Source sentences:
text: Aquifers: fresh water underground
text: Along this line, the water is fresh on the upthrown side of a fault and very saline (usually a sodium- or calcium-sulfate type water) on the downthrown side (fig.
text: Most groundwater is produced from the sand units of the aquifer, where the water is fresh and ranges from less than 50 to 1,000 milligrams per liter of total dissolved solids.
text: Water from these formation is typically fresh, although high salinity affects some water at greater depths.
text: Water in the upper Paleozoic aquifers is fresh only in small areas at or near places where recharge enters the aquifers.
text: Water in the Laney aquifer is fresh to slightly saline.
text: Water withdrawn from the Gulf Coast aquifer in Webb County is fresh to slightly saline and is withdrawn for domestic, stock, irrigation, industrial, and public-supply uses.
text: Water from the Carrizo aquifer is fresh to slightly saline and commonly is used for commercial and industrial purposes and public supply in Webb County.
text: Water from the Carrizo aquifer is fresh to slightly saline and generally fresher near the outcrop.
text: The Lower Floridan aquifer is generally less permeable than the Upper Floridan aquifer and the water produced can be highly mineralized and/or saline; however, the Lower Floridan aquifer is relatively fresh water to the base of the system in central Florida and in updip areas of central and southern Georgia and Alabama.