It was indicated in a previous paper (Geol. Mag., LXXII, 1935, p. 208) that the Scottish Lower Carboniferous crinoid fauna contains a number of species which have never been adequately described. In the present communication, ten of these are discussed, the remainder, another ten or eleven species, will be dealt with later. All the specimens except four were collected by myself many years ago, but it was only recently that the requisite leisure was found to develop and clean them thoroughly.

I wish to correct by 40 feet the position hitherto assigned to the outcrop of the Ballachulish Slide (or Lag as it is safe to call it) in one of its four easily accessible exposures on the shores of Loch Leven. The change does not appreciably affect the mapping as shown on Sheet 53 of the Geological Survey one-inch-to-the-mile map of Scotland, but it is of some importance on the ground. The locality lies on the north shore of Loch Leven, within a few yards of the main road, opposite a small cottage, midway between Callert House and Callert Cottage. A conspicuous little summerhouse is built on the eastern edge of the quartzite listed below. The dip of all the formations is very steep, so that the breadths of outcrop, measured at right angles to strike, correspond roughly with thicknesses. Details are as follows:—

Prior to a discovery made recently by the writer, of spilitic rocks at Great King Island, the largest member of the Three Kings group of islands, about 26 miles north-west of the north-west extremity of the mainland of New Zealand, such rocks had not previously been found in this latter country. Some account of the types represented at Great King Island may therefore be welcome, particularly since Gilluly's (1935) recent comprehensive paper has focused attention on spilites and their associations.

In 1932 during the early stages of the construction of the undercliff sea wall between Brighton and Rottingdean, whereby the foot of the cliff has now been protected from marine erosion and its top from undue recession in future, opportunity was taken to examine the sections of Coombe Rock and Raised Beach exposed at Black Rock. The face of the cliff has been trimmed and sloped back here and there in the interests of promenaders beneath and, what with this and a certain amount of walling-up, the sections are now less clear and extensive than they were in the first stage of the work. At several points, however, the Raised Beach overlain by the Coombe Rock (“Elephant Bed”) is (April, 1936) well exposed, and its top and/or bottom may still be examined.