Hula Valley in the context of "Korazim Plateau"

The Golan Heights, or simply the Golan, is a basaltic plateau at the southwest corner of Syria. It is bordered by the Yarmouk River in the south, the Sea of Galilee and Hula Valley in the west, the Anti-Lebanon mountains with Mount Hermon in the north and Wadi Raqqad in the east. It hosts vital water sources that feed the Hasbani River and the Jordan River. Two thirds of the area was depopulated and occupied by Israel following the 1967 Six-Day War and then effectively annexed in 1981. The international community largely considers the area Israeli-occupied Syrian territory. The United States recognized it as part of Israel in 2019 during the first Trump administration. In 2024, Israel occupied parts of the remaining one third of the area.

The earliest evidence of human habitation on the Golan dates to the Upper Paleolithic period. It was home to the biblical Geshur, and was later incorporated into Aram-Damascus, before being ruled by several foreign and domestic powers, including the Assyrians, Babylonians, Persians, Itureans, Hasmoneans, Romans, Ghassanids, several caliphates, and the Mamluk Sultanate. It was ruled by the Ottoman Empire from the 16th century until its collapse, and subsequently became part of the French Mandate in Syria and the State of Damascus in 1923. When the mandate terminated in 1946, it became part of the newly independent Syrian Arab Republic, spanning about 1,800 km (690 sq mi).

The Jordan Rift Valley, also Jordan Valley (Modern Hebrew: בקעת הירדן Bik'at Hayarden, Biblical Hebrew: בִּקְעָת הַיַרְדֵּן, romanized: Biqʿāṯ hay-Yardēn, Arabic: الغور, romanized: al-Ghawr), is an elongated endorheic basin located in modern-day Israel, Jordan, and Palestine. This geographic region includes the entire length of the Jordan River from its sources, through the Hula Valley, the Korazim Plateau, the Sea of Galilee, the Jordan Valley, all the way to the Dead Sea, the lowest land elevation on Earth – and then continues through the Arabah depression, the Gulf of Aqaba whose shorelines it incorporates, until finally reaching the Red Sea proper at the Straits of Tiran.

The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run for about 1,000 km from the Marash triple junction (a junction with the East Anatolian Fault in southeastern Turkey) to the northern end of the Red Sea Rift (just offshore of the southern tip of the Sinai Peninsula). The fault system forms the transform boundary between the African plate to the west and the Arabian plate to the east. It is a zone of left lateral (sinistral) displacement, signifying the relative motions of the two plates. Both plates are moving in a general north-northeast direction, but the Arabian plate is moving faster, resulting in the observed left lateral motions along the fault of approximately 107 km at its southern end. A component of extension is also present in the southern part of the transform, which has contributed to a series of depressions, or pull-apart basins, forming the Gulf of Aqaba, Dead Sea, Sea of Galilee, and Hula basins. A component of shortening affects the Lebanon restraining bend, leading to uplift on both sides of the Beqaa valley. There is local transtension in the northernmost part of the fault system, forming the Ghab pull-apart basin. The southern part of the fault system runs roughly along the political border of Lebanon and Israel on its western side, and southern Syria and Jordan on the eastern side.

Jabal Amil (Arabic: جبل عامل, romanized: Jabal ʿĀmil; also spelled Jabal Amel and historically known as Jabal Amila) is a cultural and geographic region in Southern Lebanon largely associated with its long-established, predominantly Twelver Shia Muslim inhabitants. Its precise boundaries vary, but it is generally defined as the mostly highland region on either side of the Litani River, between the Mediterranean Sea in the west and the Wadi al-Taym, Beqaa and Hula valleys in the east.

The Shia community in Jabal Amil is thought to be one of the oldest in history. In the 10th century, several Yemeni tribes with Shi'ite inclinations, including the 'Amila tribe, had established themselves in the region. 'Amili oral tradition and later writings assert that a companion of the Islamic prophet Muhammad and an early supporter of Ali, Abu Dharr al-Ghifari (d. AD 651), introduced Shi'ism to the area. Although there is frequent occurrence of this account in many religious sources, it is largely dismissed in academia, and historical sources suggest Shia Islam largely developed in Jabal Amil between the mid-8th and 10th centuries (750–900). Twelver Shia tradition in southern Lebanon credits the Amila, as the progenitors of the community, by having sided with the faction of Ali in the mid-7th century.