FIG. 1. Hind feet and portion of the vertebræ of a fossil _Dicynodont_ reptile (_Owen_), natural size. Found by Capt. Jas. Scott Helps, in the white shale in a cutting 50 feet deep, at the east of Kimberley mine, facing claim .018, and 40 feet back from the margin of the mine, measuring from the surface. The above was drawn by Mr. Geo. Jas. Lee, in Jan. 1878, soon after it was found. The above specimen, together with three others, were presented by Mr. Geo. Jas. Lee to the trustees of the British Museum, and were, I believe, submitted to Professor Owen, who has now for some years past been engaged preparing a monogram upon the Dicynodonts. From the _Photographic News_ of Oct. 16th, 1885, I take the following: “The British Association meeting at Aberdeen. In the Geological section, Dr. R. H. Fraquair described a new and very remarkable reptile, lately found in the Elgin sandstone, entirely from a photograph of the specimen submitted to him by Professor Judd. He was able to assign the creature to the genus _Dicynodon_, which characterizes similar sandstones in South Africa.” There are no sandstones, however, near the Kimberley mine, but the casts of Dicynodons have been found both within and without the mine, and also in fragments of white shale upon the surface of the ground a few hundred yards away from the mine. In Mr. Ralph Tate’s “Historical Geology,” the following passage occurs:— “Reptiliferous Sandstones of Morayshire: Geologists have maintained, on stratigraphical grounds, that the Reptiliferous Sandstones are of the age of the Old Red Sandstone; but the intervention of a conglomerate implies a stratigraphical break, and a lapse of time of indefinite extent; and the paleontological evidence favors the supposition that these sandstones are of Triassic age.” In the light colored shales to which I allude, and nearly in the same place, a fragment of a fossil fish (_Palæoniscus_) of Triassic age was found, and was presented to the British Museum. I may here repeat a passage from Mr. W. S. Dowel’s paper, already quoted in this chapter: “Professor Liversidge describes the geological formation of the district (Bingera, 350 miles north of Sydney, Australia) as being of the Devonian or Carboniferous age, but when making a visit in 1873 he was unable, in consequence of want of time, and wet weather, to secure fossils in order to verify his opinion. Since then Mr. Donald Porter and others have discovered fossils and indications that clearly go to show that the professor was correct in the opinions he had formed respecting the nature of the geological stratification and the age to which it belonged.” FIG. 2. Portion of a fossil leaf, natural size, found by Mr. Geo. Jas. Lee on Oct. 13th, 1880, in the white shale from the Kimberley mine, at a depth of about 50 feet, facing road 9, south. Length (as restored), 2¹⁄₂₀ inches; apex (restored), ¹⁷⁄₄₀ inch; width (entire), 1¼ inches.