PROFILPELAJAR.COM

The Buried Valley Aquifer System is a buried valley aquifer in the central basin of the Passaic River watershed in New Jersey, as defined by the U.S. Army Corps of Engineers and U.S. Environmental Protection Agency. This region impacts drinking water sources for twenty-six municipalities in four northern New Jersey counties: Morris, Union, Essex, and Somerset.^[1]

The borders of this area is defined as:

"on the north by Hook Mountain (a basaltic lava flow) and by a line which roughlybisects the Town of Montville. The western boundary is defined by the trace of the Ramapo Fault and the beginning of the Highlands Physiographic Province. The boundary to the south and the east is formed by the Second Watchung Mountain range, including portions of Union, Essex and Somerset Counties, New Jersey."^[1]

This area includes the following municipalities:^[1]

In Essex County: Caldwell, East Orange, Essex Fells, Fairfield, Irvington, Livingston, Maplewood, Millburn, North Caldwell, Roseland, West Caldwell, West Orange
In Morris County: Chatham (borough), Chatham Township, East Hanover, Florham Park, Hanover, Harding Township, Madison, Montville, Morris Plains, Morristown, Morris Township, Parsippany-Troy Hills, Passaic Township
In Somerset County: Bernards Township, Warren Township
In Union County: Berkeley Heights, New Providence, Springfield, Summit

References

^ ^a ^b ^c U.S. Environmental Protection Agency - Region 2 Water. Buried Valley Aquifer System: Support Document, Western Essex and Southeastern Morris Counties, New Jersey, April 1980 Archived December 2, 2013, at the Wayback Machine. Retrieved 24 November 2013.

This water supply–related article is a stub. You can help Wikipedia by expanding it.

[EPA-BVASSupportDoc-1] U.S. Environmental Protection Agency - Region 2 Water. Buried Valley Aquifer System: Support Document, Western Essex and Southeastern Morris Counties, New Jersey, April 1980 Archived December 2, 2013, at the Wayback Machine. Retrieved 24 November 2013.

[1]