itself, and it has some quartzite boulders. See the specimens. Below it recurs as then quartzite amy( matter (or specimen), and a siliceous li. Then we went on to Stog Cove and Deadmans Point, to see the Cornish li., a very peculiar laminated high metamorphosed li. See the samples. These are the oldest rocks in the Redland Flier, and all that are have seen are said to be equivalent to sequence series of the Cambrian and Cambris Ordovician", However no one has found the first trace of a fossil and nor we since put any closer or, therefore there is no evidence here to check the age other than the Armor li., of Silurian age that unimportant rules are these "Cambrian" To one the whole series is of early Portuguese age. In the later Portuguese came the not only granitic igneous intrusions. We then drove back to Camden where we had lunch and the back to Haterville via Stape, North Appletum, (Cambridge is the junction between the Penzance and the metamorphic series). The contact appears to be rather a little north of North Appletum. Then Park Learmont, Haterville (not the name of yesterday), Liberty and Alton. Put up for the night at the Edmund Hotel.