"but they in which are mere recently found, a minutes basis truth. The Oolite is blue does not apparently exist on the spot but must be closely in place. The black band came on into a blue gray band just as it is in the tent at truck. This may be a Big Sandy glacial pebbles deposit. The Bridgman formation is more shown in a small quarry to the east of Big Sandy. It appears to have the same thickness here as at Camden about 20 feet. The Sturges and Catawba are more abundant than at Camden. The Oolite is inconstant seen many times along with Camden gravel for say one mile east of Big Sandy.