Rock's principal works are: Hierurgia, or the Holy Sacrifice of the Mass expounded (London, 1833; revised edition by W. H. J. Weale, 1893), an exhaustive account of the Eucharistic rites in the Latin, Greek and Oriental Churches, and illustrated from early paintings, sculptures and inscriptions; The Church of Our Fathers, as seen in St Osmund's Rite for the Cathedral of Salisbury, with Dissertations on the Belief and Ritual in England before the Coming of the Normans (3 vols., 1849–54; new edition by G. W. Hart and W. H. Frere, London, 1903).
See the Memoir prefixed to Hart & Frere's edition of The Church of Our Fathers by the Rev. B. W. Kelly; a full list of his writings is given in J. Gillow's Bibl. Dict. of the Engl. Catholics, vol. v. p. 436.
ROCK (O. Fr. roke, Sp. roca, Ital. rocca; possibly from a Lat.
form rupica, from rupes, rock), in geology a mass of the mineral matter of which the crust of the earth is composed (see Petrology
and Geology). In more general usage a “ rock ” is a large
mass of this mineral matter, as distinguished from smaller
pieces which are termed “ stones.”
From this word must be distinguished the verb “ to rock,” to swing an object to and fro, particularly of a cradle in which a child is rocked to sleep, the original meaning. The O.Eng. word is roccian, and is cognate with many words in Teutonic languages, e.g. Du. rukkea, Dan. rykke, Ger. rücken, to pull, tug, push.
ROCK-CRYSTAL, a colourless and transparent variety of quartz (q.v.), used as an ornamental stone. It usually occurs as crystals lining cavities in quartz-veins, which often run through granite, gneiss and crystalline schists. The limpidity of the crystal, its coldness to the touch and its common occurrence in rocks among Alpine glaciers, led to the ancient belief that it
was a kind of congealed water, whence the name crystal, from
Gr. κρύσταλλος (ice). In the Swiss Alps the “ Strahler,” or crystal gatherer,
searches the rocks at much personal risk, and is often
led to a drusy cavity by tracing narrow veins, or strings, of
quartz on the mountain-side. A remarkable druse, or Krystalkeller,
discovered at Zinkenstock in the Bernese Oberland,
in 1719, yielded about 20 tons of crystal, a single specimen
weighing 8 cwt. The famous discovery of the Galenstock, in
1867, furnished magnificent crystals, but they were dark brown
or smoky quartz. La Gardette, near Le Bourg d'Oisans, in the
Alps of Dauphiné, is a notable locality for fine specimens of
rock-crystal. The Alps and India probably furnished the
ancients with their supplies.
Rock-crystal has been used for ornamental purposes since the Mycenean period. By the Romans under the Empire it was highly valued, and carved into vases and goblets, in some cases elaborately engraved. Lenses or globes were used for kindling the sacred vestal fire and for cauterizing the flesh, whilst ladies carried balls of crystal in order to cool their hands during the heat of summer. The artists of the Early Renaissance greatly favoured the use of rock-crystal, and executed beautiful carvings in this material. In modern times the use of rock-crystal has been largely superseded by that of glass, and it is notable that flint-glass is known in France as “cristal,” probably from its resemblance to limpid quartz, or perhaps from the fact that powdered rock-crystal has been used as a source of silica in the manufacture of the finest glass. Rock-crystal is still cut as a faceted stone for personal decoration, but though not without brilliancy it lacks the “ fire ” of many gemstones. It is often known locally by such names as Bristol diamond, Cornish diamond, Isle of Wight diamond, Briançon diamond, Marmaros diamond, Lake George diamond, &c. Rock-crystal is also carved into seals, paper-weights and other trivial objects, and into spheres for divination by crystal-gazing, Japanese balls being specially noteworthy. In Japan the crystal has been obtained for centuries from the granitic districts around Kimpū-san, in the province of Kai. Probably the most valuable application of rock-crystal is for spectacle lenses, which in consequence of their hardness are not readily abraded by use. They should be cut at right angles to the optic axis, or axis of the prism.
The “ pebble " for lenses is found loose in the soil in many parts of the provinces of Goyaz, São Paulo and Minas Geraes in Brazil. Much of the material for spectacles comes also from Madagascar, where large crystals of clear quartz are found in the beds of certain streams, especially in the N.E. part of the island, having probably been derived from quartz-veins in the gneiss and pegmatite. In India rock-crystal has been worked at many localities, and the loot of the palace of Delhi yielded marvellous ornaments carved in this material. At the present day it is cut and polished at Vellum in the Tanjore district in Madras, and is known as Vellum stone. Among the numerous localities in the United States which yield rock-crystal mention may be made of those in Herkimer Co., New York State, whence the Lake George crystals are obtained; and it is notable that some of the Herkimer quartz encloses bituminous matter. Mokelumne Hill, Calaveras Co., California, has furnished some remarkable rock-crystal. In Europe the localities are very numerous, the most important being those in the Alps. Very fine crystals remarkable for pellucidity though not of large size occur in cavities in the statuary marble of Carrara; and remarkably hollowed crystals are known from Porretta near Bologna in Italy. The finest rock-crystal in Great Britain occurs at Tintagel and the Delabole slate quarry in N. Cornwall; and at Snowdon in N. Wales. (F. W. R.*)
ROCKEFELLER, JOHN DAVISON (1839–), American capitalist, was born in Richford, Tioga county, New York, on the 8th of July 1839. In 1853 his family removed to Ohio, living after 1857 in Cleveland, where Rockefeller had begun to work as a bookkeeper in 1855 and where in 1858 he went into the produce commission business. His firm, Clark & Rockefeller, in 1862 invested in an oil refinery, planned by Samuel Andrews,
and in 1865 Rockefeller sold out his share to his partner Clark, bought for $72,500 a larger share in another refinery, and formed the partnership of Rockefeller & Andrews. At about the same time another refinery was started by Rockefeller's brother William (b. 1841), but in 1867 Rockefeller & Andrews absorbed this business, and Henry M. Flagler was added to the partnership. In 1870 the two Rockefellers, Flagler, Andrews and a refiner named Stephen V. Harkness formed the Standard Oil Company, with a capital of $1,000,000 (increased in 1872 to $2,500,000 and in 1874 to $3,500,000), of which John D. Rockefeller was president. This great corporation gradually established itself in practical control of the oil production in America, by means of business methods and financial operations which have been severely criticized, but which brought immense wealth to those concerned. Its capital was further increased in 1882, when separate companies were organized in each state; and in later years, as the first great American “ trust,” the Standard Oil Company was hotly attacked during the anti-trust movement (see Inter-State Commerce). Into the merits of this question it is impossible to enter here. Rockefeller himself retired from active business in 1895; he had for a time large iron interests (mines and ore-carrying vessels) on Lake Superior, which he sold to the United States Steel Corporation, and his personal wealth was probably greater than that of any other man
in the country. In private life he was a devoted member of the Baptist church, and his benefactions were numerous. To “ the University of Chicago founded by John D. Rockefeller ” (in 1892) he had given, up to 1910, $24,809,666, while to the General Education Board he had given $43,000,000§ he founded (1901) and supported the Rockefeller Institute for Medical Research in New York City; he gave large sums to Rush Medical College in Chicago, to Johns Hopkins Hospital in Baltimore, to Barnard College in New York City and to the Baptist Missionary Society; and in 1909 he gave $1,000,000 to
endow a medical commission to investigate the nature of the hook-worm and to suppress the hook-worm disease.
See Ida M. Tarbell's History of the Standard Oil Company (New York, 1903), a severe attack on the Trust; also his own Random Reminiscences (1909).
ROCKET. (1) The name (Fr. roquette, Lat. eruca, a kind of cabbage) of two species of plants. The one, Eruca sativa, is a cruciferous annual with white flowers veined with purple; the leaves have a sharp flavour and are used in southern Europe for salads. The other is a hardy perennial herbaceous plant, of the genus Hesperis, of which Hesperis matronalis is the most familiar species (see Horticulture).
(2) A cylinder of paper, pasteboard or metal, filled with an explosive mixture. This word, which appears in many forms in various languages, is from the It. rocchetta, diminutive of rocca, a distaff, the obsolete English “ rock ”; the application
