Alamanni and Visigoths, and partly ruined by the erections of the middle ages. Orange was included in the kingdom of Austrasia, fell into the hands of the Saracens and was recovered by Charlemagne. It became the seat of an independent countship in the 11th century. From the 14th century till the Revolution the town had a university. At the latter period the town suffered severely from the excesses of a popular commission.
See R. Peyre, Nimes, Arles et Orange (Paris, 1903); A. de Pontbriant, Histoire de la principauté d’Orange (Avignon and Paris, 1891).
Councils of Orange.—In 441 a synod of sixteen bishops was held at Orange under the presidency of St Hilary of Aries, which adopted thirty canons touching the reconciliation of penitents and heretics; the ecclesiastical right of asylum, diocesan prerogatives of bishops, spiritual privileges of the defective or demoniac, the deportment of catechumens at worship, and clerical celibacy (forbidding married men to be ordained as deacons, and bigamists to be advanced beyond the sub-diaconate). In 529 a synod of fifteen bishops, under the presidency of Caesarius of Aries, assembled primarily to dedicate a church, the gift of Liberius, the lieutenant of Theodoric, in Gaul, but proved to be one of the most important councils of the 6th century. Caesarius had sought the aid of Rome against semi-Pelagianism, and in response Pope Felix IV. had sent certain capitula concerning grace and free-will, drawn chiefly from the writings of Augustine and Prosper. These to the number of twenty-five the synod subscribed, and adopted a supplementary statement, reaffirming the Augustinian doctrines of corruption, human inability, prevenient grace and baptismal regeneration. Its acts were confirmed by Boniface II. on the “25th of January 530,” a date which is open to question.
See F. H. Woods, Canons of the Second Council of Orange (Oxford, 1882). (T. F. C.)
ORANGE, a city of Essex county. New Jersey, U.S.A., in the N.E. part of the state, about 14 m. W. of New York City. Pop. (1890) 18,844, (1900) 24,141, of whom 6598 were foreign born and 1903 were negroes, (1910 census) 29,630. It is served by the Morris & Essex Division of the Delaware, Lackawanna & Western railroad and by the Orange branch (of which it is a terminus) of the Erie railroad, and is connected with Newark, South Orange and Bloomfield by electric lines. The city lies at the base of the eastern slope of the first Watchung, or Orange, Mountain, and is primarily a residential suburb of New York and Newark; with East Orange, West Orange and South Orange it constitutes virtually a single community, popularly known as “the Oranges.” The city has a good public school system and various private schools, including the Dearborn-Morgan School (for girls) and the Carteret Academy (for boys). Of historical interest is the First Presbyterian Church, erected in 1813, the third structure used by this church organization, whose history dates back to 1718. The value of the factory products of Orange increased from $2,995,688 in 1900 to $6,150,635 in 1905, or 105·3%, and the capital invested in manufacturing from $1,359,523 in 1900 to $3,441,183 in 1905, or 153·1%. Of the total product-value in 1905, $2,311,614 was the value of felt hats manufactured. Among other manufactures are beer, pharmaceutical supplies and lawn mowers. The city owns and operates its water-works and electric lighting plant. Settlements were made in or near the limits of the present city soon after the founding of Newark, in 1666, and, on account of the mountainous ridge in this region, they were generally referred to collectively as “Newark Mountain.” As a disagreement soon arose between the people of Newark and those of “the mountain” on questions of church administration, the latter in 1718 severed their connexion with the church at Newark and formed an independent congregation, the “Mountain Society.” The church, which was known also as “The Church of the New Ark Mountains,” was at first Congregational, but in 1748 became Presbyterian. In 1782 occurs the earliest reference to the neighbourhood as “Orange Dale,” and two years later it is sometimes referred to as “Orange.” In 1806 the legislature incorporated the township of Orange. Parts of its territory were included in South Orange and Fairmount (now West Orange) in 1861 and 1862 respectively, and in 1863 East Orange was created out of part of Orange. Orange was incorporated as a town in 1860 and was chartered as a city in 1872.
See H. Whittemore, The Founders and builders of the Oranges (Newark, 1896); J. H. Condit, Early Records of the Township of Orange (1807–1845) (Orange, 1897); and S. Wickes, History of the Oranges (1666–1806), (Newark, 1892).
ORANGE, the longest river of South Africa, almost traversing the continent from ocean to ocean. It rises in Basutoland, less than 200 m. from the Indian Ocean, and flows west, with wide sweeps south and north, to the Atlantic. It drains, with its tributaries, an area estimated at over 400,000 sq. m., passing through more than twelve degrees of longitude or 750 m. in a straight line from source to mouth. The valley of the river exceeds 1000 m., and the stream has a length of not less than 1300 m. Its head streams are in the highest part of the Drakensberg range, the principal source, the Senku, rising, at an elevation of more than 10,000 ft., on the south face of the Mont aux Sources in 28° 48′ E., 28° 50′ S. The other head streams are S.E. of the Senku source, in Champagne Castle, Giant’s Castle and other heights of the Drakensberg. The Giant’s Castle source is not more than 130 m. west of the Indian ocean in a direct line.
Rising on the inner slopes of the hills these rivulets all join the Senku, which receives from the north several streams which rise in the Maluti Mountains. Of these the largest are the Semene and Senkunyane (little Senku) and the best known the Maletsunyane, by reason of its magnificent waterfall—an unbroken leap of 630 ft. Increased by the perennial waters of these numerous torrents the Senku makes its way S.W. across the upland valleys between the Maluti and Drakensberg ranges. After a course of some 200 m., passing the S.W. corner of the Maluti Mountains, the Senku, already known as the Orange, receives the Makhaleng or Kornet Spruit (90 m.), which rises in Machacha Mountain. The Orange here enters the great inner plateau of South Africa, which at Aliwal North, the first town of any size on the banks of the river, 80 m. below the Kornet Spruit confluence, has an elevation of 4300 ft. Forty miles lower down the Orange is joined by the first of its large tributaries, the Caledon (230 m.), which, rising on the western side of the Mont aux Sources, flows, first west and then south, through a broad and fertile valley north of the Maluti Mountains. At the confluence the united stream has a width of 350 yards. Thirty miles lower down the Orange reaches, in 25° 40′ E., its southernmost point—30° 40′ S., approaching within 20 m. of the Zuurberg range. In this part of its course the river receives from the south the streams, often intermittent, which rise on the northern slopes of the Stormberg, Zuurberg and Sneeuwberg ranges—the mountain chain which forms the water-parting between the coast and inland drainage systems of South Africa. Of these southern rivers the chief are the Kraai, which joins the Orange near Aliwal North, the Stormberg and the Zeekoe (Sea Cow), the last named having a length of 120 m.
From its most southern point the Orange turns sharply N.W. for 200 m., when having reached 29° 3′ S., 23° 36′ E. it is joined by its second great affluent, the Vaal (q.v.). Here it bends south again, and with many a zigzag continues its general westerly direction, crossing the arid plains of Bechuana, Bushman and Namaqualands. Flowing between steep banks, considerably below the general level of the country, here about 3000 ft., it receives, between the Vaal confluence and the Atlantic, a distance of more than 400 m. in a direct line, no perennial tributary but on the contrary loses a great deal of its water by evaporation. In this region, nevertheless, skeleton river systems cover the country north and south. These usually dry sandy beds, which on many maps appear rivers of imposing length, for a few hours or days following rare but violent thunderstorms, are deep and turbulent streams. The northern system consists of the Nosob and its tributaries, the Molopo and the Kuruman. These unite their waters in about 20° 40′ E. and 27° S., whence a channel known as the Molopo or Hygap runs south to the Orange. The southern system, which at one time rendered fertile the great plains of western Cape Colony, is represented by the Brak and Ongers rivers, and, farther west, by the Zak and Olifants rivers, which, united as the Hartebeest, reach the Orange about 25 m. above the mouth of the Molopo. These rivers, in the wet season and in places, have plenty of water, generally dissipated in vleis, pans and vloers (marshy and lake land).
Between the mouths of the Hartebeest and Molopo, in 28° 35′ S., 20° 20′ E., are the great waterfalls of the Orange, where in a series of cataracts and cascades the river drops 400 ft. in 16 m. The Aughrabies or Hundred Falls, as they are called, are divided by ledges, reefs and islets, the last named often assuming fantastic shapes. Below the falls the river rushes through a rocky gorge, and openings in the cliffs to the water are rare. These openings are usually the sandy beds of dried-up or intermittent affluents, such as the Bak, Ham, Houm, Aub (or Great Fish) rivers of Great Namaqualand. As it approaches the Atlantic, the Orange, in its efforts to pierce the mountain barrier which guards the coast, is deflected
