Water-level conditions in the Black Creek and
upper Cape Fear aquifers, 1992, in parts of Bladen and Robeson
Counties, North Carolina
Water-Resources
Investigations Report 94-4016
By A.G. Strickland
Abstract
Water-level measurements were made in 68 wells
throughout an area of about 860 square miles in
Bladen and Robeson Counties, North Carolina,
during September and October 1992. Water levels
from 58 wells were used to determine the
configuration of the potentiometric surface of the
Black Creek aquifer. A map of the potentiometric
surface shows the potential for ground water to
flow from recharge areas in the local uplands to
discharge areas, such as local streams and wells.
Pumping from wells at major pumping centers, such
as Elizabethtown in Bladen County and Lumberton in
Robeson County, where water-level declines of more
than 12 feet were recorded from 1988 to 1992, has
resulted in cones of depression in the
potentiometric surface. The cones were about 4
and 6 miles long across the major axes beneath the
Elizabethtown and Lumberton areas, respectively,
in 1992. Water levels measured in eight wells in
1988 and 1992, supplemented with water levels in
two additional wells from driller's well-
construction records, were used to estimate
average yearly rates of ground-water change for
the upper Cape Fear aquifer for part of the study
area. During 1988-92, water-level declines
occurred in the aquifer throughout much of the
area as a result of pumping. The greatest
decline, an average of 4.1 feet per year, was in
Bladen County.
Citation:
Strickland, A.G., 1994, Water-level conditions in the Black Creek and upper Cape Fear aquifers, 1992, in parts of Bladen and Robeson Counties, North Carolina: U.S. Geological Survey Water-Resources Investigations Report 94-4016, 1 sheet
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