“…Approximately 25 mi east of the UFS drill hole, on the eastern side of the North Mountain fault in northern Virginia ( fig. 1), the Gatesburg Formation correlates with a 2,500-to 3,000-ft-thick sequence of sandy limestone and dolomite that was identified as the Conococheague Formation (Limestone) (Butts, 1940;King, 1950;Wilson, 1952;Edmundson and Nunan, 1973;Young and Rader, 1974;Rader and Biggs, 1976;Rader, 1982) (fig. 2).…”