DescriptionThe Hackensack River and its associated wetlands have been greatly impacted by man. Construction of a dam at Oradell has greatly altered the original river hydrology, and consequently it no longer...
DescriptionCohesive sediment erosion differs significantly from coarse-grained, non-cohesive (sand) erosion phenomena. Non-cohesive sediment erosion can generally be quantified based on applied shear stress...
DescriptionThe study area in this report is the shallow water area of the Delaware River Estuary from Reedy Point, Delaware to the head of tide at Trenton, New Jersey. Shallow water areas are defined as those...
DescriptionThe Delaware River Basin Commission is charged with establishing water-quality objectives for the tidal and non-tidal portions of the Delaware River, which include developing nutrient standards that...
DescriptionMap covers area from Middle Marsh Creek to Fishers Point along Delaware River. Map shows the location for a channel 600 feet wide and 30 feet deep at mean low water.
DescriptionPart of a series of historic maps from the late 1800s and early 1900s. These maps, from the United States Geological Survey, present geographic and topographic information from the time period.
DescriptionPart of a series of historic maps from the late 1800s and early 1900s. These maps, from the United States Geological Survey, present geographic and topographic information from the time period.
DescriptionThis document contains the argument of Thomas N. McCarter, President of Public Service Corporation of New Jersey and Public Service Electric and Gas Company, at the opening of the company's case for...
DescriptionSheet 2: Gloucester County from Deptford Township to Harrison Township. Map shows Deptford, Harrison, and East Greenwich. Also shows a plan of the town of Salem.
Sheet 3: Salem County from...