LONDON Mineralogical Society, June 7.—C. PALACHE: The form relations of the lead oxychlorides, laurionite, paralaurionite, and fiedlerite. The separate identity of each of the first two minerals is confirmed and their homoeomorphism is exhibited by a re-orientation of laurionite. The form series of fiedlerite has been simplified by the choice of a new unit form. New forms are described on paralaurionite and fiedlerite. The crystallography of all three species is summarised in new angle-tables, and their habits are illustrated by a series of drawings. F. A. BANNISTER: The crystal structure and optical properties of matlockite (PbFCl): W. Nieuwenkamp's recent work proving the identity of matlockite with artificial lead fluochloride, PbFCl, has been confirmed. New chemical analyses, X-ray work and optical measurements have been carried out on single crystals of matlockite from Cromford, Derbyshire. Single crystal photographs of the mineral have also confirmed the crystal structure proposed for artificial PbFCl. Artificial BiOCl, BiOBr and BiOI have crystal structures of the same type, and the relationship between matlockite and these and other compounds is discussed: Artificial Pb2OCl2 has a crystal structure quite different from that of matlockite. Mendipite, Pb3O2C12, contains no fluorine, and it is improbable that fluorine has been overlooked in the oxychloride minerals from Laurium, Greece. V. ZSIVNY and L. ZOMBORY: Berthierite from Kisbanya, Carpathians. This rare mineral, previously known from two localities in old Hungary, is now described from a third, namely Kisbanya in comitat Szatmar (now Chiuzbaia in Satu Mare, Roumania) where it occurs as bundles of needles with stibnite and rhombohedral carbonates. Analysis agrees closely with the formula FeS.Sb2S8, but the specific gravity 4-65 is much higher than values previously recorded. L. J. SPENCER: Beryllium minerals (euclase and phenakite) from Africa. Apart from beryl, there are very few recorded occurrences of beryllium minerals in the whole of Africa. Euclase is described from pegmatite on the Lukangasi mica claim, Morogoro district, Tanganyika Territory. The main crystal on the single specimen collected measures 7-2 cm. by 3-5 cm., being much larger than any euclase crystal hitherto known. Seventeen crystal forms were determined. Small crystals of phenakite from pegmatite at the Klein Spitzkopje, Soutfr-West Africa, are of two distinct habits, prismatic and lenticular. A. C. SKERL and F. A. BANNISTER: Lusakite, a cobalt-bearing silicate from Northern Rhodesia. The mineral occurs embedded in quartz-magnetite-kyanite-rock of gneissoid appearance from 80 miles east of Lusaka. Crystals, generally tabular to (010) varying up to 5 mm. in length, are black in hand-specimens, but show a deep cobalt-blue colour, and strong pleochroism in thin section. The mean refractive index is approximately 1-74 and 2V is near 90°. Oscillation, Laue, and rotation photographs show that lusakite has an orthorhombic unit cell with edges a 7-86, b 16-62, c 5-63 A., and space-group F 17. The unit cell contains 8 [RO.Al2SiO5] where R represents Fe, Co, Ni, Mg, Al, and H. The cobalt content is unique for a silicate and reaches 8£ per cent CoO, or nearly two atoms of cobalt per unit cell. It is almost identical in physical properties with staurolite, and X-ray photographs show that it possesses the same type of crystal structure. A. W. GROVES: The determination of small amounts of copper in rocks. The paper describes the application to silicate analysis of the sodium diethyl-dithio-carbamate colorimetric method for copper. Data on the retention of copper by the ammonia precipitate are given. The method has a range of 0-001-0-25 per cent CuO when a sample of 2 grams is used. L. J. SPENCEB: Thirteenth list of new mineral names. A dictionary list of 112 names collected from the literature of the past three years. Since the first list in 1897, a total of 1,918 names has been collected. L. J. SPENCEB: A new meteoric stone from Silverton, New South Wales. A beautifully oriented stone weighing 351 grams was found by Mr. R. Bedford amongst debris in the old museum at Port Adelaide, which has recently been reorganised as a Nautical Museum. It probably dates from the time (1883) of the discovery of the rich mineral deposits at Broken Hill in the Silverton district. The stone is a white hypersthene-olivine-chondrite of the Baroti type with only little nickel-iron. M. H. HEY: Studies on the zeolites (8). A theory of the vapour-pressure of zeolites. An equation for the water vapour pressure of a zeolite (or other compound showing similar dissociation phenomena) is derived on simple kinetic grounds, and is shown to agree reasonably well with the available experimental data. The equation, which can only be a first approximation to the truth, is compared with other equations previously proposed. Kinetic treatment also leads to a reasonable equation for the rate of diffusion of water within a zeolite crystal. The condition of the water in the zeolites is discussed.
Read full abstract