Queen Anne's County Observation-Well Network
The Queen Anne's County water-level network is one of three county observation-well networks maintained by MGS and funded through county cooperative agreements. Other counties include Anne Arundel and Charles counties.
The primary objective of these networks is to monitor the effects of water-supply withdrawals on groundwater levels at both a local (well field) and regional scale. More specifically the water-level data are used to help assess (1) long-term sustainability of the water supply; (2) well interference (drawdown at each well in a multiple-well system added to drawdowns at the other wells); (3) potential for increased development of the aquifers; (4) potential for salt-water intrusion, where applicable; and (5) the role of ground-water extraction in land subsidence.
The Queen Anne's County observation-well network is currently funded through a cooperative agreement between Maryland Geological Survey and Queen Anne's County Department of Public Works. The network consists of 27 wells located mainly in the western (Kent Island) portion of the County. Aquifers monitored include the Surficial (Columbia) (2 wells), Aquia (17 wells), Magothy (1 well), Upper Patapsco (3 wells), Lower Patapsco (3 wells), and Patuxent (1 well). Frequency of measurement ranges from 12 times a year to semiannual (spring and fall).
Current Water Level Trends
Water levels were measured in two wells in this aquifer (at Barclay and Grasonville). Water levels fluctuate seasonally up to approximately five feet. Current water levels range from 67.41 ft above sea level at Barclay (QA Cg 69) to 17.78 ft above sea level at Grasonville (QA Ec 1). Water-level trends are continuing to increase at Barclay while remaining flat at Grasonville.
Water levels were measured in seventeen wells in this aquifer, thirteen of which are located on Kent Island. Most wells show less than 2 feet of seasonal variation, with the lower water levels recorded in late summer and higher water levels in spring. Current water levels range from 16.91 ft above sea level at Kingstown (QA Be 17) to 9.87 ft below sea level at Centreville (QA De 27). Water levels at Centerville fluctuate by as much as 25 feet seasonally likely as a result of regional irrigation withdrawals. Overall, long-term trends in this aquifer are increasing.
Water levels were measured in one well in the Magothy aquifer (Natural Resources Academy in Matapeake [QA Ea 27]). The most recent water level was 20.58 ft below sea level. Prior to 2014, water levels declined at the rate of about 1 ft per year (ft/yr). Since then, water levels have stabilized
Upper Patapsco aquifer
Water levels were measured in three wells completed in this aquifer. Current water levels range from about 17.16 ft below sea level at Kingstown (QA Be 16) to about 24.53 ft below sea level at QA Ef 29 (Tuckahoe State Park). All three wells show steady water-level declines of about 1 ft/yr over the past 10 years, likely reflecting regional pumping effects in Anne Arundel, Queen Anne’s and Talbot (Easton) counties.
Lower Patapsco aquifer
Water levels were measured in three wells completed in this aquifer. Current water levels range from about 7.88 ft below sea level at Kingstown (QA Be 15) to about 41.55 ft below sea level at Stevensville (QA Eb 182). Two of the wells, located at Kingstown (QA Be 15) and Chester (QA Eb 112) continue to show a decline rate of about 1 ft/yr. The water level trend at Stevensville (QA Eb 182) is relatively flat; however, the well is likely affected by local withdrawals, making an assessment of trends difficult.
Water levels were measured in one well in the Patuxent aquifer at Chester (QA Eb 110). Current water level was about 11.86 ft below sea level. Beginning in 2018, water-level declines have slowed down and began to stabilize. The steep decline starting in 2012 was a result of withdrawals from the Arnold well field in Anne Arundel County.