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n of Borneo. On that island there are coal-seams under approximately similar circumstances to those on Labuan. So far as I know, however, they have not hitherto been closely examined with respect to vegetable palaeontology. At Labuan fossil plants are found, though very sparingly, imbedded in balls of clay ironstone from strata above the two lowermost coal-seams. The upper coal-seams are besides exceedingly rich in resin, which crosses the coal in large veins. From the thickness and conversion into a hard sandstone of the layers of sand lying between and above the coal-seams we may conclude that a very long time, probably hundreds of thousands or millions of years have passed since these coal-seams were formed. They also belong to a quite recent period, during which the vegetation in these regions varied perhaps only to a slight extent from that of the present time. It is, however, too early to express one's self on this subject, before the fossils which we brought home have been examined by Dr. Nathorst. Coal mining was stopped for the time, but orders were expected by every post to resume work. The road between the mine and the harbour town was at all events pretty well kept, and Mr. COOKE, one of the directors of the company, still lived at the place. He showed me all possible hospitality during the time I remained on the north side of the island for the purpose of collecting fossils. The rest of the time I was the guest of the acting Governor, Mr. TREACHER, a young and amiable man, who showed me several collections in natural history from Labuan and the neighbouring parts of Borneo, and after our return to Europe sent me a collection of leaves and fruit of the kinds of trees which now grow on the island. I expect that this collection will be very instructive in the study of the fossil plants we brought home with us. At the steep shore banks on the north coast very fine sections of the sandstone strata, which lie under and above the coal, are visible. While I went along the shore in order to examine these, I visited some Malay huts built on poles. They were surrounded at flood tide by water, at ebb by the dry beach, bare of all vegetation. In order to get inside these huts one must climb a ladder two to two and a half metres high, standing towards the sea. The houses have the same appearance as a warehouse by the seaside at home, and are built very slightly. The floor consisted of a few rattling bamboo splin
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