cannot more than 75 feet, without there more pure limestone continue downward into the Cronidul limestone holding the Creigmens fauna Collected from this deep-fenced limestone. Between the latter and the more pure limestone then may be interpose 20 feet of gritty limestone and then 20 feet of the cronidul limestone. The latter rests with a marked lithologic break upon heavy bedded coarse sand- stone shown where the two roads come together Little Smith All of this should provide the at cross creek Creigmens (See if this is true). a unconformity here shown on the sandstone layers. There in here no shale and thus far near Redwood. The Marlius rests directly upon the Massanutten. There is no reason to infer that this quartzite represents the Redwood since it looks just like the Massanutten, at Augusta Spring these upper layers are more weathered but otherwise are alike and here also the Lepuditra layers rest upon the Massanutten.