The Hauran (; also spelled Hawran or Houran) is a region that spans parts of southern Syria and northern Jordan. It is bound in the north by the Ghouta oasis, to the northeast by the al-Safa field, to the east and south by the Harrat al-Sham and to the west by the Golan Heights. Traditionally, the Hauran consists of three subregions: the Nuqrah and Jaydur plains, the Jabal al-Druze massif, and the Lajat volcanic field. The population of the Hauran is largely Arab, but religiously heterogeneous; most inhabitants of the plains are Sunni Muslims belonging to large agrarian clans, while Druze form the majority in the eponymous Jabal al-Druze and a significant Greek Orthodox and Greek Catholic minority inhabit the western foothills of Jabal al-Druze. The region's largest towns are Daraa, Ramtha, and Suwayda.
From the mid-1st century BC, the region was governed by the Roman Empire's Herodian and Nabatean client kings until it was formally annexed by the empire in the 2nd century AD. The Hauran prospered under Roman rule (106–395 AD) and its villages functioned as largely self-governing units, some of which developed into imperial cities. The region continued to prosper in the Byzantine era (395–634), during which different Arab tribes ruled the Hauran on Byzantium's behalf, including the Salihids (5th century) and Ghassanids (6th century) until the Muslim conquest in the mid-630s. For much of the Islamic era until Ottoman rule (1517–1917), the Hauran was divided into the districts of al-Bathaniyya and Ḥawrān, which corresponded to the Classical Batanea and Auranitis. Medieval Muslim geographers variously described these districts as prosperous, well-watered and well-populated.
Under the Romans, the grain of Batanea and the wine of Auranitis were important for imperial trade, and throughout its history, the Hauran was the major source of the Levant's grain. The region saw a decline in the 17th century until increased demand for Syrian grain and improved security led to the agricultural revival and re-population of the Hauran in the mid-19th century. The region also historically benefited as a key transit area on the traditional Hajj caravan route to Mecca and later the Hejaz railway. The Hauran remained Syria's breadbasket until being largely supplanted by northern Syria in the mid-20th century, which coincided with its separation from interdependent areas due to international borders and the Arab–Israeli conflict. Nonetheless, it persisted as an important agricultural and commercial transit area into the 2000s. During the Syrian Civil War, which was sparked in the Hauran in 2011, it became a major conflict zone between rebels and government forces in the Daraa Governorate campaign until the government reasserted control in 2018, only to later fall into rebel hands after the Southern Syria offensive and the Fall of the Assad regime.
The wide availability of basalt in the Hauran led to the development of a distinct vernacular architecture characterized by the exclusive use of basalt as a building material and a fusion of Hellenistic, Nabatean and Roman styles. The durability of basalt is credited for the Hauran's possession of one of the highest concentrations of well-preserved Classical-era monuments in the world. Hauran towns such as Bosra, Qanawat, Shahba, Salkhad, Umm al-Jimal and numerous others contain Roman temples and theaters, Byzantine-era churches and monasteries, and forts, mosques and bathhouses built by successive Muslim dynasties.
Geography Geographic definition
Though its geographic definition may vary, the Hauran generally consists of the following subregions: the Hauran plain, which forms the heart of the region; the mountains of Jabal Hauran (also known as 'Jabal al-Druze' or 'Jabal al-Arab') east of the plain; and the Lajat volcanic field to the north of Jabal Hauran. The region is bound to the north by the Ghouta and Marj plains around Damascus and to the south by the desert steppe of Jordan. Its western boundary is marked by the Ruqqad tributary, which separates it from the Golan Heights ( in Arabic). It is eastwardly bound by the al-Safa, al-Harra and al-Hamad desert-steppes. Geographer John Lewis Burckhardt, writing in 1812, defined it as follows: To the south of Jabal Kiswah and Jabal Khiyara begins the country of Hauran. It is bordered on the east by the rocky district of Lajat, and by the Jabal Hauran, both of which are sometimes comprised within the Hauran ... To the southeast, where Bosra and Ramtha are the farthest inhabited villages, the Hauran borders upon the desert. Its western limits are the chain of villages on the Hajj road, from Ghabaghib as far south as Ramtha ... Hauran comprises therefore part of Trachonitis and Iturea, the whole of Auranitis, and the northern districts of Batanea.
The plain of Hauran stretches between the Marj plain of Damascus southward into modern-day Jordan where it borders Jabal Ajlun to the southwest and the desert steppe to the south and southeast. To the west is the Golan plateau and to the east are the uplands of Jabal Hauran. The plain has historically been divided into the northern Jaydur and the southern Nuqrah. The former is identified with the ancient Iturea, while the latter is identified with the ancient Batanea ( in Arabic). The much larger Nuqrah extends northward to the approaches of al-Sanamayn, being bound to the east by the Lajat and Jabal Hauran. It forms the heart of the Hauran plain. is a relatively recent appellation, meaning 'the cavity' in Arabic. The Jaydur extends northwest from al-Sanamayn to the minor lava field located at the foothills of Mount Hermon ( in Arabic).
Topography
A common feature throughout the Hauran is the basaltic topography, though altitude and soil vary between the Hauran's subregions. The Nuqrah, Jaydur and Jabal Hauran consist of arable land derived from decomposed basaltic, volcanic rock. The Nuqrah is a relatively low plateau measuring roughly with an average elevation of above sea level. Its land is characterized by vast, contiguous tracts of fertile, basalt-derived soil. In contrast to the Nuqrah, the Jaydur's landscape is more fractured and rocky. Its average elevation ranges between above sea level, with some volcanic cones reaching above above sea level, including Tell al-Hara. In terms of its landscape and cinder cones, the Jaydur is a topographic continuation of the Golan Heights. The Jabal Hauran was formed by large lava flows into a roughly massif of volcanic hills, the highest point of which is over above sea level in the range's center. The Lajat comprises a topography of depressions, rifts and ridges with scattered arable patches, and is characterized by rocky soil and scarce vegetation. Its average elevation is between above sea level, though some of the area's volcanic cones are over with the highest over .
Climate Rainfall above the mark is characteristic throughout the Hauran, but otherwise climate and precipitation levels vary between its subregions. The relatively frequent rainfall and the abundance of water springs have historically allowed the Nuqrah and Jabal Hauran to become major grain-growing regions. The Hauran plain receives an average of rainfall, which allows the plains to support stable, grain-based agriculture. Jabal Hauran receives considerably greater rainfall, which supports more orchard and tree-based cultivation. Jabal Hauran is frequently covered by snow during the winter.
+ Monthly normal high and low temperatures (°C) for largest localities in the HauranCity Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec AnnualMax/Min Citation Bosra 12/2 13/3 17/5 22/8 27/12 31/15 32/16 32/16 31/15 27/12 20/8 14/3 23/10 Daraa 13/3 15/4 18/6 24/9 28/12 31/16 33/18 33/19 31/16 28/13 21/8 15/5 24/11 Nawa 13/4 15/4 18/6 22/9 28/13 31/16 32/18 33/18 31/16 28/13 21/9 15/5 24/11 Ramtha 14/4 15/4 18/7 22/10 27/14 31/17 32/19 32/19 30/17 27/14 22/9 15/5 24/11 Suwayda 10/2 12/3 15/5 20/8 25/11 29/14 30/16 31/16 29/14 26/12 19/8 13/4 22/9
History There are records of settlements in the Hauran in the Ancient Egyptian Amarna letters and the Book of Deuteronomy of the Hebrew Bible, when the region was generally known as the Bashan. Control of it was contested between the Aramean kingdom of Damascus and the Kingdom of Israel during the 9th and 8th centuries BC. It was ultimately conquered and pillaged by the Assyrian Empire, which held onto it from 732 to 610 BC. The area is mentioned in the description of the future borders of Israel in . Bashān later saw security and prosperity under Achaemenid rule; its settlements became better developed and culturally Aramized.
Hellenistic period During the Hellenistic period beginning in the mid-4th century BC, the Hauran was at first a possession of the Ptolemaic dynasty, which saw the region as a buffer zone separating their kingdom from Seleucid Damascus. Its sparse population consisted of semi-nomadic and nomadic groups such as the Itureans and Nabateans and the area remained largely undeveloped. The Seleucids conquered the Hauran following their victory over the Ptolemies in the Battle of Panium near Mount Hermon in 200 BC. During the decline of the Seleucid Empire, the Petra-based Nabatean Kingdom emerged to the Hauran's south. The Arab Nabateans expanded their presence to the southern Hauran towns of Bosra and Salkhad. By the end of the 2nd century BC, Seleucid control of the Hauran had become largely nominal and the region became a contested area between the Nabataean Kingdom, the Jerusalem-based Hasmonean dynasty and the Iturean principality based in the northern Golan and southern Mount Lebanon.
Roman era Herodian period
By 63 BC the Roman Empire extended its influence to all of Syria and initially charged local princes with keeping order in Auranitis (Jabal Hauran), Batanea (Nuqrah) and Trachonitis (Lajat). However, the districts remained largely in the hands of nomadic tribes. To supplement their meager income, these nomads often raided nearby settlements as far as Damascus, and robbed pilgrims traversing the region. When Zenodorus, a prince entrusted with the Hauran districts' security, collaborated with the nomads, the Romans transferred the districts to their Judean client king, Herod the Great in 23 BC.
After Herod quelled resistance in the Hauran during the early years of his rule, the brigandage of the nomads largely ceased. Their rebellion resumed in 12 BC and two years later Herod renewed his efforts to bring the nomads to heel. This resulted in an alliance formed between the nomads of Trachonitis and Auranitis with the Nabateans in Transjordan, which defeated Herod's Idumean troops. Herod ultimately stabilized the area after establishing permanent colonies and a network of forts in the less vulnerable Batanea district, from which Herod's forces could keep order without fear of attack by the nomads of Auranitis and Trachonitis. Through the establishment of security, land distribution and early tax incentives, Batanea prospered under Herod and his successors and became Syria's main source of grain. Auranitis began to similarly prosper during the reign of Philip, Herod's successor in the Hauran.
Post-annexation