Pennsylvania Water Science Center

Installing groundwater monitoring equipment


Dennis Risser


In collaboration with the Pennsylvania Geological Survey.

Hydrologic Effects of the Pymatuning Earthquake of September 25, 1998 in Northwestern Pennsylvania

Fleeger, G.M. (PaGS), D.J. Goode, T.F. Buckwalter, and D.W. Risser, WRIR 99-4170, 8 p. [ report pdf ]

Report Abstract

      Within hours after the Pymatuning earthquake of September 25, 1998, in northwestern Pennsylvania, local residents reported wells becoming dry, wells beginning to flow, and the formation of new springs. About 120 household-supply wells reportedly went dry within 3 months after the earthquake. About 80 of these wells were on a ridge between Jamestown and Greenville, where water-level declines of as much as 100 feet were documented. Accompanying the decline in water levels beneath the ridge was an increase in water levels in valley wells of as much as 62 feet. One possible explanation of the observed hydrologic effects is that the earthquake increased the vertical hydraulic conductivity of shales beneath the ridge, which allowed ground water to drain from the hilltops. Computer simulations of ground-water flow beneath the ridge between Jamestown and Greenville indicate that increasing the vertical hydraulic conductivity of shale confining beds about 10 to 60 times from their pre-quake values could cause the general pattern of decreased water levels on hilltops and increased levels in valleys.

Additional Information

      A 3-foot rise in the ground-water level was recorded in USGS observation well MR-1364 in Greenville on September 25. Details on this well are given below. A graph showing the water-level rise in this valley well is also shown below. Water levels generally decreased in ridge-top wells.

ground water level during earth quake

SITE IDENTIFIER 412350080223701
LOCATION Latitude 41`23'50", Longitude 80`22'37"
Hydrologic Unit 05030102, at Greenville, Pa.
OWNER Borough of Greenville
AQUIFER Sandstone of Cussewago Formation of Early Mississippian age
WELL CHARACTERISTICS Drilled artesian well, diameter 6 in,
depth 235 ft, cased to 41 ft, open hole
INSTRUMENTATION Continuous strip-chart recorder
DATUM Elevation of land-surface datum is 965 ft above sea level,
from topographic map. Measuring point: Top of
plywood cover, 2.26 ft above land-surface datum
REMARKS Water levels affected by intermittent pumping
PERIOD OF RECORD March 1964 to current year
(through September, 1997)
Highest water level, 1.43 ft below land-surface datum, Dec. 25, 1968;
lowest, 8.31 ft below land-surface datum, Feb. 12, 1967
FUNDING FOR WELL The observation well is operated by USGS in cooperation with the Pennsylvania Department of Environmental Protection

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