British Possessions.—Legislation much on the lines of the acts of 1889-1908 has been passed in many British possessions, e.g. Tasmania (1895, 1906), Queensland (1896, 1905), Jamaica (1896), South Australia (1899, 1904), New South Wales (1892 and 1900), New Zealand (1906), Mauritius (1906), Victoria (1905,1906). In South Australia a State Children’s Department has been created to care for and manage the property and persons of destitute and neglected children, and the officials of the council may act in cases of cruelty to children; the legislation of Victoria and Queensland is based on that of South Australia.
See also [Children’s Courts], [Education] and [Labour Legislation].
(W. F. C.; T. A. I.)
[1] There has been some doubt as to whether it is more correct to say a person “overlays” or “overlies” a child, and the question came up in committee on the bill. According to Sir J.A.H. Murray (see Letter in The Times, 12th of May 1908) “to lie,” an intransitive verb, becomes transitive when combined with a preposition, e.g. a nurse lies over a child or overlies a child; “to lay” is the causal derivative of “to lie,” and is followed by two objects, e.g. to lay the table with a cloth, or to lay a cloth on the table; similarly, to overlay a surface with varnish, or to overlay a child with a blanket, or with the nurse’s or mother’s body. The instrument can be left unexpressed, and a person can be said to overlay a child, i.e. with her own body, a pillow, &c. Thus, while “overlie” covers the case where the woman herself lies over the child, “overlay” is the more general word.
CHILDRENITE, a rare mineral species; a hydrous basic aluminium iron phosphate, orthorhombic in crystallization. The ferrous oxide is in part replaced by manganous oxide and lime, and in the closely allied and isomorphous species eosphorite manganese predominates over iron. The general formula for the two species is Al(Fe, Mn)(OH)2PO4 + H2O. Childrenite is found only as small brilliant crystals of a yellowish-brown colour, somewhat resembling chalybite in general appearance. They are usually pyramidal in habit, often having the form of double six-sided pyramids with the triangular faces deeply striated parallel to their shorter edges. Hardness 4.5-5; specific gravity 3.18-3.24. The mineral, named after the zoologist and mineralogist J.G. Children (1777-1852), secretary of the Royal Society, was detected in 1823 on specimens obtained some years previously during the cutting of a canal near Tavistock in Devonshire. It has also been found in a few copper mines in Cornwall and Devonshire.
Eosphorite occurs as crystals of prismatic habit with angles very nearly the same as those of childrenite. Unlike childrenite, it has a distinct cleavage in one direction, and often occurs in compact masses as well as in crystals. The colour is sometimes yellowish-white, but usually rose-pink, and on this account the mineral was named from ἠωσφόρος, dawn-bearer. Hardness 5; specific gravity 3.11-3.145. It was discovered in 1878 in a pegmatite-vein at Branchville, Connecticut, where it is associated with other rare manganese phosphates.
(L. J. S.)