Cats was contemporary with Hooft and Vondel and other distinguished Dutch writers in the golden age of Dutch literature, but his Orangist and Calvinistic opinions separated him from the liberal school of Amsterdam poets. He was, however, intimate with Constantin Huygens, whose political opinions were more nearly in agreement with his own. For an estimate of his poetry see [Dutch Literature]. Hardly known outside of Holland, among his own people for nearly two centuries he enjoyed an enormous popularity. His diffuseness and the antiquated character of his matter and diction, have, however, come to be regarded as difficulties in the way of study, and he is more renowned than read. A statue to him was erected at Brouwershaven in 1829.
See Jacob Cats, Complete Works (1790-1800, 19 vols.), later editions by van Vloten (Zwolle, 1858-1866; and at Schiedam, 1869-1870); Pigott, Moral Emblems, with Aphorisms, &c., from Jacob Cats (1860); and P.C. Witsen Gejisbek, Het Leven en de Verdiensten van Jacob Cats (1829). Southey has a very complimentary reference to Cats in his “Epistle to Allan Cunningham.”
CAT’S-EYE, a name given to several distinct minerals, their common characteristic being that when cut with a convex surface they display a luminous band, like that seen by reflection in the eye of a cat. (1) Precious cat’s-eye, oriental cat’s-eye or chrysoberyl cat’s-eye. This, the rarest of all, is a chatoyant variety of chrysoberyl (q.v.), showing in the finest stones a very sharply defined line of light. One of the grandest known specimens was in the Hope collection of precious stones, exhibited for many years at the Victoria and Albert Museum. (2) Quartz cat’s-eye. This is the common form of cat’s-eye, in which the effect is due to the inclusion of parallel fibres of asbestos. Like the chrysoberyl, it is obtained chiefly from Ceylon, but though coming from the East it is often called “occidental cat’s-eye”—a term intended simply to distinguish it from the finer or “oriental” stone. It is readily distinguished by its inferior density, its specific gravity being only 2.65, whilst that of oriental cat’s-eye is as high as 3.7. A greenish fibrous quartz, cut as cat’s-eye, occurs at Hof and some other localities irr Bavaria. (3) Crocidolite cat’s-eye, a beautiful golden brown mineral, with silky fibres, found in Griqualand West, and much used in recent years as an ornamental stone, sometimes under the name of “South African cat’s-eye.” It consists of fibrous quartz, coloured with oxide of iron, and results from the alteration of crocidolite (q.v.). It is often distinguished as “tiger’s-eye” (or more commonly “tiger-eye”), whilst a blue variety, less altered, is known as “hawk’s-eye.” By the action of hydrochloric acid the colour of tiger’s-eye may to a large extent be removed, and a greyish cat’s-eye obtained. (4) Corundum cat’s-eye. In some asteriated corundum (see ASTERIA) the star is imperfect and may be reduced to a luminous zone, producing an indistinct cat’s-eye effect. According to the colour of the corundum the stone is known as sapphire cat’s-eye, ruby cat’s-eye, topaz cat’s-eye, &c.
(F. W. R.*)
CATSKILL, a village and the county-seat of Greene county, New York, U.S.A., on the W. bank of the Hudson river, 33 m. S. of Albany. Pop. (1890) 4920; (1900) 5484; of whom 657 were foreign-born; (1910) 5206. It is served by the West Shore railway, by several lines of river steamboats, and by the Catskill Mountain railway, connecting it with the popular summer resorts in the Catskill mountains. A ferry connects with Catskill station (Greendale) on the east side of the Hudson. The village is in a farming country, and manufactures woollen goods and bricks, but it is best known as a summer resort, and as the principal gateway to the beautiful Catskill Mountain region. The Recorder, a weekly newspaper, was established here in 1792 as the Packet. The first settler on the present site of Catskill was Derrick Teunis van Vechten, who built a house here in 1680. The village was not incorporated until 1806.
See J.D. Pinckney, Reminiscences of Catskill (Catskill, 1868).
CATSKILL (formerly Kaatskil) MOUNTAINS, a group of moderate elevation pertaining to the Alleghany Plateau, and not properly included in the Appalachian system of North America because they lack the internal structures and the general parallelism of topographic features which characterize the Appalachian ranges. The group contains many summits above 3000 ft. elevation and half a dozen approaching 4000, Slide Mountain (4205 ft.), and Hunter Mountain (4025 ft.), being the only ones exceeding that figure. The bottom lands along the creeks which drain the mountains, together with rolling uplands rising to elevations of from 1500 to 2000 ft., are under cultivation, the mountain slopes being forested or devoted to grazing. The pure and cool atmosphere attracts summer visitors, for whose accommodation many hotels have been built, some of which have become celebrated. Stoney Clove and Kaaterskill Clove are picturesque gorges, the former being traversed by a rail way, and the latter containing three cascades having a total fall of about 300 ft. The growing need of New York City for an increased water-supply has driven her engineers to the Catskills, where several great reservoirs have been projected to supplement those of the Croton watershed.