Jawa, Jordan

Last updated
Jawa
Jawa, eastern Jordan.jpg
View of Jawa from the south
Jordan location map.svg
Archaeological site icon (red).svg
Shown within Jordan
Location Jordan
Region Mafraq Governorate
Coordinates 32°20′06″N37°00′12″E / 32.33500°N 37.00333°E / 32.33500; 37.00333

Jawa is the site of the oldest proto-urban development in Jordan, dating from the late 4th millennium BC (Early Bronze Age). It is located in one of the driest areas of the Black Desert (Harrat al-Shamah) of Eastern Jordan. [1]

Contents

Remains of dams have been found, the largest of which is a masonry gravity dam and the oldest known dam in the world. It was used as a protection from flash floods.

Discovery and history of investigation

Jawa was first reported by French explorer Antoine Poidebard, who flew over and photographed the site in 1931, mistaking it for Roman ruins. [2] Before and after Poidebard's discovery, several archaeological expeditions came close to but missed the site. Nelson Glueck visited it in 1947 but apparently failed to notice its significance, describing Jawa as a "small, filthy spring […] probably never more than a small police post." [3] Finally, in 1950, an expedition led by epigrapher F. V. Winnett reached the site and documented some of the inscriptions there. Amongst their number was Lankester Harding, who suggested that the remains were not Roman but in fact dated to the Early Bronze Age. [2]

Harding recommended the site to Svend Helms, who first visited the site in 1966 and directed excavations there between 1972 and 1976. [2] [4] In contrast to earlier assumptions about the site's lack of significance, Helms concluded that "Jawa is the best preserved fourth-millennium town yet discovered anywhere in the world: paradoxically in a place—the Black Desert—where it could hardly exist today and probably hardly when it was built." [1]

History

The town was built by a group of perhaps 2,000 migrants coming from the North or East. They had some understanding of urban life, as well as hydrology. It extended over 100,000 m2 [1] and consisted of a walled town and extensive earthworks to divert winter floods from the wadi into a series of reservoirs. This work would have had to be completed by the first winter after the group's arrival; otherwise they would not have survived the following summer. It is estimated the work would have taken a minimum workforce of 700. [5]

Jawa (2013) Jawa (Ruins).jpg
Jawa (2013)

It is located on the southern edge of an area of basalt which runs across Syria and eastern Jordan and is an attempt to harness the major water resources of Wadi Rajil: a dry river bed which floods irregularly during the winter months. [6] Wadi Rajil has a catchment area of 300 km2 reaching 35 km north into Jebel Druze. [7] The basalt allows very little water to soak into the ground. Any rainfall in the mountains results in violent short lived flash floods. The total annual flow down the wadi at Jawa is estimated to be 2,000,000 m3 per year arriving in a few dramatic winter floods with flows of 80–110 m3/s. Research suggests that the community at Jawa could survive on 3% of that total flow: if they could store it in sufficient quantities to last through the four dry summer months. [8] It would have to support their population of 2,000 to 5,000 as well as their large herds of sheep, goats and some cattle. Estimates based on bone counts indicate there may have been as many as 10,000 sheep and goats as well as 800 cattle. There were also 200 equids and 160 dogs. [9] From seed remains it is apparent that some of the water was also used for irrigation agriculture. The inhabitants ate barley, wheat, chickpeas, lentils and grapes. [10]

Based on the size and density of houses in the excavated areas, Helms estimated that the maximum population of the town was between 3,000 to 5,000. [11] He also considered it short-lived: occupied for perhaps as little as a single generation before it was violently destroyed. [12]

There is a fortified building located in the center of the ruins of the original town. It is believed to date from 2000 to 1500 BC, and is not associated with any contemporaneous stone structures. [13]

Water supply system

Jawa Dam
Jawa, eastern Jordan.jpg
Reliefkarte Jordanien.png
Red pog.svg
Location of Jawa Dam in Jordan
LocationJawa, Mafraq Governorate, Jordan
Coordinates 32°20′06″N37°00′12″E / 32.33500°N 37.00333°E / 32.33500; 37.00333
Construction began~3500 BC
Dam and spillways
Type of dam Gravity, masonry
ImpoundsWadi Rajil
Height4.5 m (15 ft)
Length80 m (260 ft)
Width (base)4.5–5 m (15–16 ft)
Reservoir
CreatesJawa Reservoir
Total capacity31,000 m3 (1,100,000 cu ft) est.

There are remains of three dams across Wadi Rajil at Jawa, part of an extensive water supply system that included other smaller dams, channels, and deflectors across the wadi to support the town. Two are deflection dams meant to channel water into a number of reservoirs. The third was an attempt at a reservoir dam, completely blocking the flow of the flood. It appears not to have survived more than one season. The other two probably ceased to function within a generation.

The largest is a masonry gravity dam, and the oldest known dam in the world, with recent carbon-14 dating putting initial construction between 3500-3400 BC. [14] [15] [16] [17] It was designed to divert water into three depressions to the west of the settlement. The feed canal was also used to fill a natural cave. The dam itself was built at an angle across the curve of the wadi. It may not have reached from bank to bank. It is speculated that even if the structure only withstood the flood for a short time, some water would have been diverted to the reservoirs.[ citation needed ]

The largest reservoir had a double wall, 80 metres long and 4–5 metres high, in-filled with sand and ash. Excavators found traces of revetments and a rudimentary apron on the up-stream face. [15] [18] [19] An attempt to build a larger wall to expand the capacity of the reservoirs beside the town was not completed. The small amount of rainfall, perhaps 150 mm per year, which fell on local micro-catchments, was also harnessed by a long series of primitive canals leading to the reservoirs. This would have been a significant contribution in maintaining water levels between floods. [20]

See also

Related Research Articles

<span class="mw-page-title-main">Geography of Iraq</span>

The geography of Iraq is diverse and falls into five main regions: the desert, Upper Mesopotamia, the northern highlands of Iraq, Lower Mesopotamia, and the alluvial plain extending from around Tikrit to the Persian Gulf.

<span class="mw-page-title-main">Dam</span> Barrier that stops or restricts the flow of surface or underground streams

A dam is a barrier that stops or restricts the flow of surface water or underground streams. Reservoirs created by dams not only suppress floods but also provide water for activities such as irrigation, human consumption, industrial use, aquaculture, and navigability. Hydropower is often used in conjunction with dams to generate electricity. A dam can also be used to collect or store water which can be evenly distributed between locations. Dams generally serve the primary purpose of retaining water, while other structures such as floodgates or levees are used to manage or prevent water flow into specific land regions.

<span class="mw-page-title-main">Diversion dam</span>

A diversion dam is a dam that diverts all or a portion of the flow of a river from its natural course. Diversion dams do not generally impound water in a reservoir; instead, the water is diverted into an artificial water course or canal, which may be used for irrigation or return to the river after passing through hydroelectric generators, flow into a different river or be itself dammed forming an onground or groundwater reservoir or a storm drain.

<span class="mw-page-title-main">Tuolumne River</span> River from Yosemite to the San Joaquin Valley, California

The Tuolumne River flows for 149 miles (240 km) through Central California, from the high Sierra Nevada to join the San Joaquin River in the Central Valley. Originating at over 8,000 feet (2,400 m) above sea level in Yosemite National Park, the Tuolumne drains a rugged watershed of 1,958 square miles (5,070 km2), carving a series of canyons through the western slope of the Sierra. While the upper Tuolumne is a fast-flowing mountain stream, the lower river crosses a broad, fertile and extensively cultivated alluvial plain. Like most other central California rivers, the Tuolumne is dammed multiple times for irrigation and the generation of hydroelectricity.

<span class="mw-page-title-main">Sevier River</span> River in central Utah, United States

The Sevier River is a 400-mile (640 km)-long river in the Great Basin of southwestern Utah in the United States. Originating west of Bryce Canyon National Park, the river flows north through a chain of high farming valleys and steep canyons along the west side of the Sevier Plateau before turning southwest and terminating in the endorheic basin of Sevier Lake in the Sevier Desert. It is used extensively for irrigation along its course, with the consequence that Sevier Lake is usually dry.

The Columbia River Treaty is a 1961 agreement between Canada and the United States on the development and operation of dams in the upper Columbia River basin for power and flood control benefits in both countries. Four dams were constructed under this treaty: three in the Canadian province of British Columbia and one in the U.S. state of Montana.

<span class="mw-page-title-main">Marib Dam</span> Dam and archaeological site in Yemen

The Marib Dam is a modern dam blocking the wadi or valley of Adhanah in the Balaq Hills, located in the Ma'rib Governorate in Yemen. The current dam was built in the 1980s and is close to the ruins of the ancient dam, first built in the 8th century BC. It was one of the engineering wonders of the ancient world and a central part of the Sabaean and Himyarite kingdoms around Ma'rib.

<span class="mw-page-title-main">Dworshak Dam</span> Dam in Idaho

Dworshak Dam is a concrete gravity dam in the western United States, on the North Fork of the Clearwater River in north central Idaho. In Clearwater County, the dam is located approximately four miles (6 km) northwest of Orofino and impounds the Dworshak Reservoir for flood control and hydroelectricity generation. By capacity, the reservoir is the largest in Idaho and fourth-largest in the Pacific Northwest.

<span class="mw-page-title-main">Reservoir</span> Storage space for water

A reservoir is an enlarged lake behind a dam, usually built to store fresh water, often doubling for hydroelectric power generation.

<span class="mw-page-title-main">Auburn Dam</span> Dam in Near Auburn, California

Auburn Dam was a proposed concrete arch dam on the North Fork of the American River east of the town of Auburn, California, in the United States, on the border of Placer and El Dorado Counties. Slated to be completed in the 1970s by the U.S. Bureau of Reclamation, it would have been the tallest concrete dam in California and one of the tallest in the United States, at a height of 680 feet (210 m) and storing 2,300,000 acre-feet (2.8 km3) of water. Straddling a gorge downstream of the confluence of the North and Middle Forks of the American River and upstream of Folsom Lake, it would have regulated water flow and provided flood control in the American River basin as part of Reclamation's immense Central Valley Project.

<span class="mw-page-title-main">Kenney Dam</span> Dam in British Columbia, Canada

The Kenney Dam is a rock-fill embankment dam on the Nechako River in northwestern British Columbia, built in the early 1950s. The impoundment of water behind the dam forms the Nechako Reservoir, which is also commonly known as the Ootsa Lake Reservoir. The dam was constructed to power an aluminum smelter in Kitimat, British Columbia by Alcan, although in the late 1980s the company increased their economic activity by selling excess electricity across North America. The development of the dam caused various environmental problems along with the displacement of the Cheslatta T'En First Nation, whose traditional land was flooded.

<span class="mw-page-title-main">Headwater Diversion Plan (Jordan River)</span> Arab League plan to divert sources of the Jordan River away from Israel

The Headwater Diversion Plan was an Arab League plan to divert two of the three sources of the Jordan River, and prevent them from flowing into the Sea of Galilee, in order to thwart Israel's plans to use the water of the Hasbani and Banias in its National Water Carrier project for out-of-Basin irrigation. The plan was approved by the Arab League in 1964 but Israel prevented the project's development by conducting airstrikes in Syrian territory in April 1967.

<span class="mw-page-title-main">Zarqa River</span> Jordanian river near Amman, tributary of the lower Jordan River

The Zarqa River is the second largest tributary of the lower Jordan River, after the Yarmouk River. It is the third largest river in the region by annual discharge and its watershed encompasses the most densely populated areas east of the Jordan River. The Zarqa rises in springs near Amman, and flows through a deep and broad valley into the Jordan, at an elevation 1,090 metres (3,580 ft) lower.

The Harbaqa Dam or Kharbaqa Dam was a Roman era Palmyrene gravity dam in the Syrian desert about 70 kilometres (43 mi) southwest from Palmyra on the road to Damascus. The dam, built of rubble, concrete, and dressed with ashlar stones, dates to the first or second century AD. The dam later was used as a water supply for the Umayyad palace of Qasr al-Hayr al-Gharbi.

<span class="mw-page-title-main">Sadd el-Kafara</span> Ancient dam

Sadd el-Kafara was a masonry embankment dam on Wadi al-Garawi 10 km southeast of Helwan in Cairo, Egypt. The dam was built in the first half of the third millennium BC by the ancient Egyptians for flood control and is the second oldest dam of the world, After dam of marib in Yemen. Never completed, the dam was under construction for 10–12 years before being destroyed by a flood. It was rediscovered by Georg Schweinfurth in 1885.

Ruwaished is a town in the far east of Jordan. Administratively it belongs to Mafraq Governorate. It has a population of 14,400. Ruwaished is the farthest Jordanian settlement to the east. The Karameh Border Crossing between Jordan and Iraq administratively belongs to the Ruwaished Department.

<span class="mw-page-title-main">Upper Wardha Dam</span> Dam in Maharashtra, India

The Upper Wardha Dam is an earthfill straight gravity dam across the Wardha River, a tributary of the Godavari River, near Simbhora village in Morshi taluk in Amravati district in the Indian state of Maharashtra. The dam provides multipurpose benefits of irrigation, drinking water supply, flood control and hydropower generation.

<span class="mw-page-title-main">Sweetwater Dam</span> Dam in San Diego County, California

The Sweetwater Dam is a dam across the Sweetwater River in San Diego County, California. It is located approximately 12 miles (19 km) east of San Diego, 9 miles (14 km) and borders Bonita to the southwest and La Presa to the northeast. The 108-foot (33 m)-high masonry arch dam impounds 960-acre (390 ha) Sweetwater Reservoir.

The Potomac River basin reservoir projects were U.S. Army Corps of Engineers programs that sought to regulate the flow of the Potomac River to control flooding, to assure a reliable water supply for Washington, D.C., and to provide recreational opportunities. Beginning in 1921 the Corps studied a variety of proposals for an ambitious program of dam construction on the Potomac and its tributaries, which proposed as many as sixteen major dam and reservoir projects. The most ambitious proposals would have created a nearly continuous chain of reservoirs from tidewater to Cumberland, Maryland. The 1938 program was focused on flood control, on the heels of a major flood in 1936. The reformulated 1963 program focused on water supply and quality, mitigating upstream pollution from sewage and coal mine waste.

<span class="mw-page-title-main">Qasr Burqu'</span> Archaeological site in the desert of Jordan

Qasr Burqu' is a set of ruins and an archaeological site in the badia of eastern Jordan and is the site of one of the earliest of the Umayyad desert castles.

References

  1. 1 2 3 Helms, Svend (1981) Jawa. Lost City of the Black Desert. Methuen. ISBN   0-416-74080-4. p.4
  2. 1 2 3 Steiner, Margreet (1984). "Review of Jawa: Lost City of the Black Desert by Svend W. Helms". Zeitschrift des Deutschen Palästina-Vereins. 100: 179–181. JSTOR   27931230.
  3. Helms, pp. 15-16
  4. Ibrahim, Moawiyah (1975). "Archaeological Excavations in Jordan: 1975" (PDF). Annual of the Department of Antiquities of Jordan (in Arabic): 18–19.
  5. Helms p.77
  6. Helms, Svend (1981) Jawa. Lost City of the Black Desert. Methuen. ISBN   0-416-74080-4. pp.17-35
  7. Helms. p.147
  8. Helms. pp.148,165,151
  9. Helms. p.189. Analysis by Ilse Kohler
  10. Helm. p.247. Analysis by G.H. Willcox
  11. Helms. p.130–131
  12. Helms. p.201–205
  13. Helms. p.6
  14. Müller-Neuhof, Bernd; Betts, AVG (2015). "Jawa, Northeastern Jordan: the first 14C dates for the early occupation phase". Zeitschrift für Orient-Archäologie. 8: 124–131.
  15. 1 2 Fahlbusch, H. (2009-02-01). "Early dams". Proceedings of the Institution of Civil Engineers - Engineering History and Heritage. 162 (1): 13–18. doi:10.1680/ehh2009.162.1.13. ISSN   1757-9430 via Institution of Civil Engineers.
  16. "Key Developments in the History of Gravity Dams". SimScience. Archived from the original on August 31, 2011. Retrieved 20 September 2018.
  17. Gujja, Biksham; Diwata Olalia Hunzike (April 2000). "The Impact of Dams on Life in Rivers". A WWF Research Report. WWF International. Retrieved 20 July 2010.
  18. Wieland, Martin; Qingwen Ren; John S. Y. Tan (2004). New developments in dam engineering: proceedings of the 4th International Conference on Dam Engineering. Taylor & Francis Group. p. 899.
  19. Helms. pp.174,175
  20. Helms. pp.181,182