FRANK SCHWARTZ' CONTRIBUTIONS TO IDENTIFICATION AND FORMATION OF FULGURITES ON THE BARRIER ISLANDS OF NORTH CAROLINA
Beach fulgurites are found as pieces along the upper intertidal zone. More than 150 beach specimens were collected for this study. A few specimens are the size of a football, others are like a small plate, most are the size of an egg. The specimens are gray and brown and are smooth, gritty, or bumpy in texture. Some specimens show remnants of the original beach sand layering, whereas others show later infilling of voids. Beach fulgurites are oddly shaped, wider, and more bulbous than those formed in deserts. This is due to electrically conductive saltwater in the pores surrounding the sand grains transporting heat away from the central tube. The intense, nearly instantaneous heat causes the saltwater to volatilize and escape upward to lower pressures while forming pockets, channels, interconnected tunnels, and domed vents not seen in desert fulgurites. Petrographic thin sections show heat deformation of quartz ranging from the inner glass, to melted and toasted grains, to the outer crust. It is unlikely a complete beach fulgurite specimen will be found due to erosion by crashing waves and the daunting task of collecting it in a thunderstorm. Consequently, it may not be possible to determine the original diameter, depth, and continuity of beach fulgurites.