Spung is Piney speak for the thousands of intermittent pools of water that dot the Pine Barrens. Rhodehamel (1970) estimated that 2% of the Pine Barrens surface is covered by these closed basins. Everyone who grew up in the Pines knew what a spung is – a pocket of water. The name’s origin is obscure. A “spung” is defined as a purse or fob, a small ‘pocket” formerly made in the waistband of breeches. It was made of wash-leather or stout lining material, and was sewn in just under the waist.
Peter Wolfe, my geology professor back at Cook College (’82), wrote about spungs as ice-thaw features during the 1950s. He grew up on a Pine Barrens farm at Nesco, so we both always had lots to talk about spung dynamics. Their origins have been controversial. In 1999 I paired up with an eminent Polar authority to reinterpret the spungs as Pleistocene blowouts (French & Demitroff 2001). I always get a chuckle out of outside researchers, who still refuse to apply the local appellation, and instead call spungs vernal pools, intermittent pools, bogs, coastal plain ponds, dry ponds, and fens when talking about these cool puddles.