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ARABIAN - 15 reference results
Philip the Arabian: see Philip, Roman emperor.
Arabian music, classical musical tradition of the Islamic peoples of Arabia, the Fertile Crescent, and North Africa.

Characteristics, Forms, and Instruments

The chief characteristics of Arabian music are modal homophony, florid ornamentation, and modal rhythm. The melodic modal system of Ibn Misjah (d. c.715) contained, in its final form, eight modes. This system lasted until the 11th cent., when the modes were increased to 12; by the 13th cent. these had come to be called maqamat. Until this time the Arabian gamut had consisted of 12 tones roughly equal to the chromatic scale of Western music.

In the 13th cent. five more tones were added, each a quarter tone below the diatonic whole tone, i.e., below d, e, g, a, b. A new tuning of the gamut was adopted in the 16th cent., and not only the tones but also the nature of the maqamat were changed. Instead of scales within which melodies were composed, they became melodic formulas to be used in composition, a system much like the ragas of Hindu music.

Ornamentation in Arabian music consisted of shakes and trills, grace notes, appoggiaturas, and the tarkib, which was the simultaneous striking of certain notes with their fourth, fifth, or octave. Until the development of instrumental music in the 10th cent., the rhythmic modes were primarily the vocal meters of poetry. In vocal music often a short melody is repeated for each stanza or verse, each repetition being elaborately ornamented.

The principal form of Arabian music is the nauba, a "suite" of vocal pieces with instrumental preludes, that probably originated at the Abbasid court. The principal Arabian instruments, other than those borrowed from older Semitic cultures, were the short-necked lute called the ud, from which the European lute derived its form and name, and the long-necked lute called tanbur. The introduction of the lute into Europe by the Moors in Spain is a certainty; the extent to which Arabian music has exerted greater influence on the West is still a matter of controversy.

History

Little is known of Arabian music before the Hegira (A.D. 622), but afterward under the Umayyad caliphs (661-750) a consolidation of Persian and Syrian elements with the native musical style took place in Arabia. Ibn Misjah devised a system of modal theory that lasted throughout the golden age under the first Abbasid caliphs (750-847). In the 9th cent. at Baghdad many treatises on music theory and history were written by such men as the philosopher Al-Kindi (9th cent.) and the illustrious Al-Farabi (c.870-c.950), who wrote the most important treatise on music up to his time.

In the 11th cent. under the last Abbasid caliphs a strong Turkistan influence was brought into Arabian music by the Seljuk Turks, and a gradual decay began in the traditional art. With the destruction of Baghdad in 1258 came the end of specifically Arabian musical culture, and only a few late examples of this music are extant. The style was preserved in Egypt and Syria because the Arabic language was spoken there, but it had lost its vitality; even this vestige died when the Ottoman Turks overran Egypt in 1517.

Bibliography

See H. G. Farmer, A History of Arabian Music to the 13th Century (1929) and Historical Facts for the Arabian Musical Influence (1930).

Arabian horse, breed of light horse developed in Mesopotamia and N Africa, and probably the first true domesticated breed. Prized since earliest times for its superior beauty, spirit, speed, grace of movement, stamina, and intelligence, the Arabian has served as parental stock for such light-weight horses as the American saddlebred horse, quarter horse, Standardbred horse, and the Thoroughbred. Intercrossings of these and other light and draft horse breeds with Arabians is still common. The Arabian's most characteristic color is bay with white markings; grays, chestnuts, and browns are also common. It averages 14 to 15 hands (56-60 in./140-150 cm) high and weighs about 1,000 lb (450 kg).
Arabian art and architecture: see Islamic art and architecture.
Arabian Sea, ancient Mare Erythraeum, northwest part of the Indian Ocean, lying between Arabia and India. The Gulf of Aden, extended by the Red Sea, and the Gulf of Oman, extended by the Persian Gulf, are its principal arms. The submarine Carlsberg ridge, SE of Socotra Island, is the sea's southern boundary. The Indus River is the largest stream flowing into the sea. The Arabian Sea has long been an important trade route between India and the West; its chief ports are Aden, Yemen; Karachi, Pakistan; and Mumbai, India.
Arabian Nights: see Thousand and One Nights.
Arabian Gulf: see Persian Gulf.
Arabian Desert or Eastern Desert, c.86,000 sq mi (222,740 sq km), E Egypt, bordered by the Nile valley in the west and the Red Sea and the Gulf of Suez in the east. It extends along most of Egypt's eastern border and merges into the Nubian Desert in the south. The Arabian Desert is sparsely populated; most of its inhabitants are based around wells and springs. Today most of the desert can be accessed by roads. Since ancient times Egypt has used the porphyry, granite, limestone, and sandstone found in the desert mountains as building materials. Oil is produced in the north. The name Arabian Desert is also commonly applied to the desert of the Arabian Peninsula.

Earliest improved breed of horse, valued for its speed, stamina, beauty, intelligence, and gentleness. Its long history has been obscured by legend, but it was developed in Arabia by the 7th century AD. It has contributed its qualities to most modern breeds of light horses. It is compact and relatively small, with a small head, protruding eyes, wide nostrils, marked withers, and a short back. Its average height is about 15 hands (60 in. [152 cm]), its average weight 800–1,000 lbs (360–450 kg). Though many colours are possible, gray is the most common.

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Northwestern part of the Indian Ocean, lying between India and the Arabian Peninsula. It has an area of about 1,491,000 sq miles (3,862,000 sq km) and an average depth of 8,970 feet (2,734 m). The Gulf of Oman connects it with the Persian Gulf via the Strait of Hormuz, while the Gulf of Aden connects it with the Red Sea via the Strait of Mandeb. The Indus is the principal river draining into the Arabian Sea. Socotra, Lakshadweep, and other islands lie within it. Chief ports are Mumbai (Bombay), India; Karachi, Pak.; and Aden, Yemen. The sea has been part of the principal trade route between Europe and India for centuries.

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or Arabia

Peninsular region, southwest Asia. With its offshore islands, it covers about 1 million sq mi (2.6 million sq km). Constituent countries are Bahrain, Kuwait, Oman, Qatar, United Arab Emirates, Yemen, and, the largest, Saudi Arabia. It is generally arid and is covered almost entirely by the Arabian Desert. The modern economy is dominated by the production of petroleum and natural gas. The world's largest proven reserves of petroleum are in the Arabian Peninsula. It was the focal point for the origins and development of the Islamic faith in the 7th century AD. Political consolidation of the region was begun by the Prophet Muhammad, and it was the centre of the caliphate until 661, when that office passed to the Umayyad dynasty in Damascus. After 1517 much of the region was dominated by the Ottoman Empire, though the peninsula's people, who had remained largely tribal and nomadic, revolted repeatedly until World War I (1914–18), when the Ottoman Empire dissolved. Thereafter, individual nation-states followed their own histories, though many maintained close ties with European powers such as the United Kingdom.

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or Gulf War

(1990–91) International conflict triggered by Iraq's invasion of Kuwait in August 1990. Though justified by Iraqi leader Ssubdotaddām Hsubdotussein on grounds that Kuwait was historically part of Iraq, the invasion was presumed to be motivated by Iraq's desire to acquire Kuwait's rich oil fields and expand its power in the region. The United States, fearing Iraq's broader strategic intentions and acting under UN auspices, eventually formed a broad coalition, which included a number of Arab countries, and began massing troops in northern Saudi Arabia. When Iraq ignored a UN Security Council deadline for it to withdraw from Kuwait, the coalition began a large-scale air offensive (Jan. 16–17, 1991). Ssubdotaddām responded by launching ballistic missiles against neighbouring coalition states as well as Israel. A ground offensive by the coalition (February 24–28) quickly achieved victory. Estimates of Iraqi military deaths range up to 100,000; coalition forces lost about 300 troops. The war also caused extensive damage to the region's environment. The Iraqi regime subsequently faced widespread popular uprisings, which it brutally suppressed. A UN trade embargo remained in effect after the end of the conflict, pending Iraq's compliance with the terms of the armistice. The foremost term was that Iraq destroy its nuclear, biological, and chemical weapons programs. The embargo continued into the 21st century and ceased only after the Iraq War started in 2003.

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Arm of the Arabian Sea. It is about 615 mi (990 km) long and rarely exceeds a depth of 300 ft (90 m). It is connected with the Gulf of Oman and the Arabian Sea through the Strait of Hormuz. It contains the island kingdom of Bahrain and is bordered by Iran, the United Arab Emirates, Oman, Saudi Arabia, Qatar, Kuwait, and Iraq. It has long been a maritime trade route between the Middle East and South Asia; its modern economy is dominated by petroleum production.

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The Rubayn al-Khali sand desert, most of which lies within Saudi Arabia.

Desert region, Arabian Peninsula. It covers about 900,000 sq mi (2,330,000 sq km), occupying nearly the entire peninsula. It lies largely within Saudi Arabia but large portions extend into Jordan, Iraq, Kuwait, Qatar, the United Arab Emirates, Oman, and Yemen. Its relief is broken by a number of mountain ranges, with elevations reaching as high as 12,000 ft (3,700 m), and it is bounded on three sides by high escarpments. At least one-third of the desert is covered by sand, including the Rubayn al-Khali, considered to have one of the most inhospitable climates on Earth. There are no perennial bodies of water, though the Tigris-Euphrates river system lies to the northeast and the Wadi Hsubdotajr is located to the south, in Yemen. Humans have inhabited the area since Pleistocene times.

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