The next day Lempree concluded that the 60' lentil may also be in place on the Highgate that was undramming by the sea and that it finally fell over and slumped some. It's ttherefore both a fieldn and a lentil in place. Elsewhere the Drantm rules unconformably the High- gate, showing the importance and extent of the overlap of the Drantm. Later it comes seen that this dist. is not the Orallett. The out thrust of the Grinrocki or what I thought was the Chazy (south of Drantm) is far away. The latter is once intacty the lower Beelemantun. Lempree says the lower white formation is oiliceros and not a limestone, Later saw it is no rather at all. Both are of the Grinrocki formation.