Clarke and Carron1 reported the first major element analysis of a Georgia tektite (USNM 1396) and discussed its composition in relation to analyses of moldavites and the tektite from Martha's Vineyard, Massachusetts. King2 published an analysis of a second Georgia tektite (DGA-1), and compared it with the previous analysis of USNM 1396. Clarke and Henderson3 and King4,5 have discussed the
... [Show full abstract] chemistry of Georgia tektites in relation to tektites from other occurrences and possible parent materials. Zähringer6 has established identical potassium–argon ages of 34 ± 1 million years for all the North American tektites.