have been transported hundreds of miles in certain fine thin nature since the majorette are now subdivided, if transported far they could have been ground either completely away or to small parts. In all of this we seem to see a Articelle dome in Pennsylvania time. I understand that sometime enclimates also occur in the Carey, where due may near a shore line still preserved. Morgan tells me that he has the mapped evidence to show that the Bozzy is a transgressive formation over the Articelle dome. The Bozzy has a thickness of about 2000 feet and relaps unconformably on formation down to the Kibla. The Franks enclimates was originally thought to relate the Brabannela as typical of early Penn. age. Morgan says the Franks is faulted against the Brabannela, as as one traces the Franks around in continued strips it is seen to interfinge with the Bozzy.