The U.S. Marine Corps Air Station, Cherry Point, North Carolina, is located in southeastern Craven County in the Coastal Plain physiographic province. The Air Station is underlain by four freshwater-bearing aquifers the surficial, Yorktown, and upper and lower Castle Hayne. These aquifers are composed primarily of sand and sandy limestone to a depth of about 500 feet below land surface. The sediments are saturated with saline water below this depth. The upper and lower Castle Hayne aquifers serve as the principal supply of freshwater for the Air Station. The upper Castle Hayne aquifer is composed of sands and sandy shell beds of the Pungo River Formation and limestone of the River Bend Formation. The lower Castle Hayne aquifer is composed of limestones, sandy limestones, and sands of the Castle Hayne Limestone. The aquifers are separated by clay confining units except where these units are absent or discontinuous. Groundwater contamination has been found in the southern part of the Air Station where pumping from supply wells has created a potential for downward movement of contaminated ground water from the surficial and Yorktown aquifers into the Castle Hayne aquifer. The potential for movement of water from the surficial aquifer downward to the water-supply aquifer is greatest in areas where clay confining units are missing. Missing confining units could indicate the presence of paleochannels. If paleochannels filled with permeable material exist beneath the Air Station, these features could act as conduits for 'U.S. Geological Survey 2Kansas Geological Survey