cmly made seem up to 200 fut thick and ten miles away, then over the little mountain Spots. One of the interesting features that is the beds feet where the better an opaque many of them one of hematite. This comes from the Basal Olduvicran also with bodies of quartzite of the same formation. One of the bodies are of the earlier Perm. formation. The bodies are usually large, up to 24ft across and while some due section did most are about angular, In place before the bodies they are pockets and lenses of red-muddy so, the whole appears to be a fineglomerate in front of and a fault cliff. It's a desert deposits since the associated sandstone and shales are red beds. Where the coal comes in the Steuartin and Fortom series (each abt 2000 fut) The evidence is rather plain of climate, But humid makes overgrows and lakes in a desert glimata; the Charing pink only where, open north, Goshardo, Tiraloro, Esteria and Leica only grow some plants. Feb. 12 - 1974