Jordan Valley (Middle East) in the context of "Pella, Jordan"

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⭐ Core Definition: Jordan Valley (Middle East)

The Jordan Valley (Arabic: غَوْر الأُرْدُنّ, romanizedGhawr al-Urdunn; Hebrew: עֵמֶק הַיַרְדֵּן, romanizedEmek HaYarden) forms part of the larger Jordan Rift Valley. Unlike most other river valleys, the term "Jordan Valley" often applies just to the lower course of the Jordan River, from the spot where it exits the Sea of Galilee in the north, to the end of its course where it flows into the Dead Sea in the south. In a wider sense, the term may also cover the Dead Sea basin and the Arabah valley, which is the rift valley segment beyond the Dead Sea and ending at Aqaba/Eilat, 155 km (96 mi) farther south.

The valley, in the common, narrow sense, is a long and narrow trough, 105 km (65 mi) long if measured "as the crow flies", with a width averaging 10 km (6.2 mi) with some points narrowing to 4 km (2.5 mi) over most of the course, before widening out to a 20 km (12 mi) delta when reaching the Dead Sea. Due to meandering, the length of the river itself is 220 km (140 mi). This is the valley with the lowest elevation in the world, beginning at −212 m (−696 ft) below sea level (BSL) and terminating at less than −400 m (−1,300 ft) BSL. On both sides, to the east and west, the valley is bordered by high, steep escarpments rising from the valley floor by between 1,200 m (3,900 ft) to 1,700 m (5,600 ft).

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👉 Jordan Valley (Middle East) in the context of Pella, Jordan

Pella (Greek: Πέλλα, Arabic: فحل) was an ancient city in what is now northwest Jordan, and contains ruins from the Neolithic, Chalcolithic, Bronze Age, Iron Age, Canaanite, Hellenistic and Islamic periods. It is located near a rich water source within the eastern foothills of the Jordan Valley, close to the modern village of Ṭabaqat Faḥl (Arabic: طبقة فحل) some 27 km (17 mi) south of the Sea of Galilee (Lake Tiberias). The site is situated 130 km (81 mi) north of Amman: a drive of about two hours (due to the difficult terrain), and an hour southwest by car from Irbid, in the north of the country. Pella's ruins – predominantly temples, churches, and housing – have been partially excavated by teams of archaeologists; they attract thousands of tourists annually but especially in spring, during which time the area is awash with spring flowers.

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Jordan Valley (Middle East) in the context of Mudbrick

Mudbrick or mud-brick, also known as unfired brick, is an air-dried brick, made of a mixture of mud (containing loam, clay, sand and water) mixed with a binding material such as rice husks or straw. Mudbricks are known from 9000 BCE.

From around 5000–4000 BCE, mudbricks evolved into fired bricks to increase strength and durability. Nevertheless, in some warm regions with very little timber available to fuel a kiln, mudbricks continued to be in use. Even today, mudbricks are the standard of vernacular architecture in some warmer regions- mainly in parts of Africa and western Asia. In the 20th century, the compressed earth block was developed using high pressure as a cheap and eco-friendly alternative to obtain non-fired bricks with more strength than the simpler air-dried mudbricks.

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Jordan Valley (Middle East) in the context of Jezreel Valley

The Jezreel Valley (Biblical Hebrew: עמק יזרעאל, romanized: ʿĒmeq Yizrəʿēl, LXX Koine Ιεζραελ), or Marj ibn Amir (Arabic: مرج ابن عامر, romanizedMarj ibn ʿĀmir, lit.'Cultivated Meadow') is a large fertile plain and inland valley in the Northern District of Israel. It is bordered to the north by the highlands of the Lower Galilee, to the south by the highlands of Samaria, to the west and northwest by the Mount Carmel range, and to the east by the Jordan Valley, with Mount Gilboa marking its southern extent. The largest settlement in the valley is the city of Afula, which lies near its center.

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Jordan Valley (Middle East) in the context of Jund al-Urdunn

Jund al-Urdunn (Arabic: جُـنْـد الْأُرْدُنّ, translation: "The military district of Jordan") was one of the five districts of Bilad al-Sham (Islamic Syria) during the early Islamic period. It was established under the Rashidun and its capital was Tiberias throughout its rule by the Umayyad and Abbasid caliphates. It encompassed southern Mount Lebanon, the Galilee, the southern Hauran, the Golan Heights, and most of the eastern Jordan Valley (especially in the north).

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Jordan Valley (Middle East) in the context of Wadi al-Taym

Wadi al-Taym (Arabic: وادي التيم, romanizedWādī al-Taym), also transliterated as Wadi el-Taym, is a wadi (dry river) that forms a large fertile valley in Lebanon, in the districts of Rachaya and Hasbaya on the western slopes of Mount Hermon. It adjoins the Beqaa Valley running north to south towards the Jordan Valley where it meets the northwest corner of Lake Huleh. Watered by the Hasbani river, the low hills of Wadi al-Taym are covered with rows of silver-green olive trees with the population in the area being predominantly Druze and Sunni, with a high number of Christians, mostly Greek Orthodox. Wadi al-Taym is generally considered the "birthplace of the Druze faith".

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Jordan Valley (Middle East) in the context of Emek HaYarden Regional Council

Emek HaYarden Regional Council (Hebrew: מועצה אזורית עמק הירדן, Mo'atza Azorit 'Emeq HaYarden, lit. Jordan Valley Regional Council) is a regional council comprising much of the western shore of the Sea of Galilee, the southern parts of its eastern shore, and the northern part of the Jordan Valley all the way to Beit She'an in the south.

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Jordan Valley (Middle East) in the context of Iraq al-Amir

'Iraq al-Amir or Araq el-Amir (Arabic:عراق الأمير - literally, "Caves of the Prince") is the name shared by a town and nearby caves, within the municipality of Amman in the Jordan Valley. Located about 15 km southwest of the town of Wadi as-Seer, it has a population of about 6000 people, mostly members of the Abbadi tribe. It is located on hills with high and medium altitude, in an area with many springs and famous for its olive trees and other forest trees.

There are many caves in the hills which were inhabited during the Copper Age. There are also remarkable Roman-Byzantine architectural remains. It is a large cave church – closed because of on-going excavations –, and a second church built outside right in front of it. The entrance of the cave can be identified by a façade decorated with a pediment with crosses. The site is called Mugharat al-Kaniseh (Cave of the Church) by the local community.

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Jordan Valley (Middle East) in the context of Salt, Jordan

As-Salt (Arabic: السلط As-Salt), also known as Salt, is an ancient trading city and administrative centre in west-central Jordan. It is on the old main highway leading from Amman to Jerusalem. Situated in the Balqa highland, about 790–1,100 metres above sea level, the city is built in the crook of three hills, close to the Jordan Valley. One of the three hills, Jabal al-Qal'a, is the site of a 13th-century ruined fortress. It is the capital of Balqa Governorate of Jordan.

The Greater Salt Municipality has about 107,874 inhabitants (2018).

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Jordan Valley (Middle East) in the context of Mud brick

A mudbrick (or mud-brick), also called an unfired brick, is an air-dried brick composed of a mixture of mud (containing loam, clay, sand, and water) with a binding material, such as rice husks or straw. Mudbricks are known to be used since 9000 BCE.

From around 5000–4000 BCE, mudbricks evolved into fired bricks to increase strength and durability. Nevertheless, in some warm regions with very little timber available to fuel a kiln, mudbricks continued to be in use. Even today, mudbricks are the standard of vernacular architecture in some warmer regions- mainly in parts of Africa and western Asia. In the 20th century, the compressed earth block was developed using high pressure as a cheap and eco-friendly alternative to obtain non-fired bricks with more strength than the simpler air-dried mudbricks.

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