The Aquia formation was named for Aquia Creek where it is exposed in cliff faces along the banks.[2]
Geology
Lithology
When uncovered, it appears dark green to gray-green, argillaceous, with well sorted fine- to medium-grained sand and locally indurated shell beds.[3] It is between 0 and 100 feet thick in Maryland.[3]Quartz and phosphatic pebbles and/or very coarse glauconitic quartz sand mark the base of the unit.[4] A few hard streaks of shells or thin "rock" layers are often reported but appear to be more abundant in the sections south of the James River.[4]
The Aquia formation is broken down into two members: the lower Piscataway member and upper Paspotansa member.[2]
Age
The Aquia Formation is thought to be 59.0-55.5 million years old.[2] The Piscataway member is 59–56.25 million years old, and the Paspotansa member is 56–55.5 million years old.[2] This is the Paleocene period.
Older publications describe the Aquia as being of Eocene age.[6]