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Person

Alison D Gordon

Hydrologist, Hydrologic Simulation Program

Email: agordon@usgs.gov
Office Phone: 609-771-3934
Fax: 609-771-3915

Location
3450 Princeton Pike
Suite 110
Lawrenceville , NJ 08648
US
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This dataset contains the well location, construction information, and water-level measurements for 983 wells measured during a groundwater-level synoptic of 10 confined aquifers of the New Jersey coastal plain. Groundwater-level measurements were made from October 2013 to January 2014. Well-location and water-level data are publicly available from the U.S. Geological Survey's National Water Information System (NWIS).
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This dataset contains 10-foot contours of the 2013 Lower Potomac-Raritan-Magothy aquifer potentiometric surface in the Coastal Plain of New Jersey. The potentiometric-surface contours show altitudes at which water levels would have risen in tightly-cased wells and represent conditions in October 2013 through January 2014. Groundwater-level data from 92 wells cased in, and with the screened interval open to the Lower Potomac-Raritan-Magothy aquifer, were used to construct the potentiometric surface and are publicly available from the U.S. Geological Survey's National Water Information System.
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This dataset contains 10-foot contours of the 2013 Middle Potomac-Raritan-Magothy aquifer potentiometric surface in the Coastal Plain of New Jersey. The potentiometric-surface contours show altitudes at which water levels would have risen in tightly-cased wells and represent conditions in October 2013 through January 2014. Groundwater-level data from 171 wells cased in, and with the screened interval open to the Middle Potomac-Raritan-Magothy aquifer, were used to construct the potentiometric surface and are publicly available from the U.S. Geological Survey's National Water Information System.
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A third revision of the New Jersey Coastal Plain (NJCP) groundwater flow model, using MODFLOW-2005 (version 1.12.00), was completed to maintain the model’s usefulness for water-resource managment and development. The regional groundwater-flow model was initially developed for the U.S. Geological Survey (USGS) Regional Aquifer System Analysis (RASA) program. Periodic revision of the model is required as the result of changing hydrologic stresses, different and more complex water management needs, and increased knowledge of hydrologic conditions. The RASA model was initially constructed in the 1980’s as a quasi-3D model with 10 aquifers. The 9 intervening confining units were simulated using vertical leakage parameters...
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This dataset contains 10-foot contours of the 2013 Wenonah-Mount Laurel aquifer potentiometric surface in the Coastal Plain of New Jersey. The potentiometric-surface contours show altitudes at which water levels would have risen in tightly-cased wells and represent conditions in October 2013 through January 2014. Groundwater-level data from 158 wells cased in, and with the screened interval open to the Wenonah-Mount Laurel aquifer, were used to construct the potentiometric surface and are publicly available from the U.S. Geological Survey's National Water Information System.
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