The Marib or Ma'rib or Ma'arib Dam (Arabic: سد مأرب) blocks the Wadi Adhanah (also Dhana or Adhana) in the valley of Dhana in the Balaq Hills, Yemen. The current dam is close to the ruins of the Great Dam of Ma'rib, dating from around the 8th century BCE. It was one of the engineering wonders of the ancient world and a central part of the south Arabian civilization around Marib.
There are also other important ancient dams in Yemen such as the Dam of Jufaynah, the Dam of Khārid, the Dam of Aḑra’ah, the Dam of Miqrān and the Dam of Yath’ān. Historically, Yemen has been recognized for the magnificence of its ancient water engineering. From the Red Sea coast to the limits of the Rub' al Khali desert are numerous ruins of small and large dams made of earth and stone.
The Great Dam of Ma'rib
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The site of the great Dam of Ma'rib (Arabic سدّ مأرب : sadd Ma'rib, or sudd Ma'rib), also called the Dam of 'Arim (Arabic سدّ العرم ): sadd al-ˁArim) is upstream (south-west) of the ancient city of Ma'rib, once the capital of the ancient Kingdom of Saba'. The Kingdom of Saba' was a prosperous trading nation, with control of the frankincense and spice routes in Arabia and Abyssinia. The Sabaeans built the dam to capture the periodic monsoon rains which fall on the nearby mountains and so irrigate the land around the city.
Recent archaeological findings suggest that simple earth dams and a canal network were constructed as far back as 2000 BCE. The Great Dam of Ma'rib certainly dates back to about the 8th century BCE and is considered the oldest known dam in the world, being counted as one of the most wonderful feats of engineering in the ancient world.
The medieval Arab geographer Yāqūt al-Ḥamawī describes it thus:
It is between three mountains, and the flood waters all flow to the one location, and because of that the water only discharges in one direction; and the ancients blocked that place with hard rocks and lead. The water from springs gathers there as well as floodwater, collecting behind the dam like a sea. Whenever they wanted to they could irrigate their crops from it, by just letting out however much water they needed from sluice gates; once they had used enough they would close the gates again as they pleased.
The date of the first construction of the Dam at Ma’rib goes back to somewhere between 1750 and 1700 BCE. The earliest inscription on the dam is one placed there at the time of its construction or repair of parts of the dam undertaken by Yithˁamar bin Samˁalī Yanūf, and the period of his reign is uncertain. The following repair was in the time of Yada 'Il Bayyin who reigned in 780-750 BCE. Renovations were then carried out by Dhamāḥ ‘Alī Dharāḥ, who reigned in 730-720 BCE. Then Karab’il Bayyin, son of Yathˁimar, who reigned from 720-710 BCE. All of these repairs were slight ones, essential maintenance, such as removing dirt, or opening water courses, or stopping up gaps. The Makrib Ali Yanouf Bin Dhamar Ali (c. 790 BCE) had his name carved into parts of the dam to mark the completion and repair of the dam.
The dam was of packed earth, triangular in cross section, 580 m in length and 4 meters high. It ran between two groups of rocks on either side of the river and was linked to the rock with substantial stonework. The dam's position allowed for a spillway and sluices between the northern end of the dam and the cliffs to the west. Around 500 BCE the dam height was increased to 7 meters, the upstream slope (the water face) was reinforced with a cover of stones, and irrigation was extended to include the southern side as well as the northern side.
After the end of the Kingdom of Saba', the dam fell under the control of the Ḥimyarites in around 115 BCE. They undertook a further reconstruction, creating a structure 14 meters high with extensive water works at both the northern and southern ends - with five spillway channels, two masonry-reinforced sluices, a settling pond, and a 1000 meter canal to a distribution tank. These extensive works were not actually finalized until 325 AD and allowed the irrigation of 25,000 acres (100 km²).
The Muslim historian al-Isfahānī (whose Annals were completed in 961 CE) maintains that the famous breach of the dam occurred some four hundred years before Islam, but Yāqūt al-Ḥamawī assigns it to the time of Abyssinian rule.
Ancient South Arabian sources report that in about 145 BCE, the dam suffered a major breach during the war between the people of Raydān and the Kingdom of Saba’, and that is the very breach that many scholars consider to have caused the great flood of ˁArim mentioned in the Quran; it is also mentioned in Arab proverbs which speak about the hands of Saba' having separated at that time. The fighting between the Raydānites and the Sabaeans delayed the repair of the dam, and this caused devastating losses of crops and fruit, leading large numbers of people to disperse in search of new land capable of supporting life, so huge migrations ensued. It is still uncertain though whether it was that particular breach that caused the ‘flood of ˁArim’ or not, since some migrations certainly took place in the 2nd or 3rd centuries CE, and they are also ascribed to the breaking of the Dam of Ma’rib. Generally speaking the dam was repaired twice shortly before the coming of Islam, once by Sharḥabīl Yaˁfar bin Abī Karab Yasˁad in 450 CE, and by Abrahah in 543 CE, and the inscriptions on the dam explain the costs of repair and the large number of workers involved.
The archaeology of the Ma'rib Dam shows the effects of siltation behind dams in antiquity, and measures to extend the operational life of the reservoir. The Ma'rib dam impounded floodwater to enable irrigation of downstream oases. Over several centuries, silts entrained in the irrigation water accumulated on the irrigated fields up to 15 m high. This caused loss of slope and conveyance, and the dam was raised to compensate. In addition to small operational openings for irrigation water withdrawals, large openings on the upstream side of the dam were probably used during construction to pass the water of the river, but may also have been used for periodical flushing of accumulated sediments. These examples show that the engineers of the time were keenly aware of reservoir siltation problems and were able to successfully extend the operational lifetime of the reservoirs by structural enhancements and probable sediment flushing. The same problems of siltation encountered in the ancient dam was also faced in the construction of the new dam.
Despite the increases in height, the dam suffered numerous breaches (recorded major incidents occurred in 449, 450, 542 and 548) and the maintenance work became increasingly onerous; the last recorded repairs took place in 557.
Local tales report that the final breach of the dam had been predicted by a king called ‘Imrān who was also a soothsayer, and later by the wife of the king of the area. In legend the breach was caused by large rats gnawing at it with their teeth and scratching it with their nails. In 570 or 575, the dam was again overtopped, and this time left unrepaired. The breaching and destruction of the Dam of Ma’rib was a historical event, and was alluded to in the Quran:
لَقَدْ كَانَ لِسَبَإٍ فِي مَسْكَنِهِمْ آيَةٌ ۖ جَنَّتَانِ عَن يَمِينٍ وَشِمَالٍ ۖ كُلُوا مِن رِّزْقِ رَبِّكُمْ وَاشْكُرُوا لَهُ ۚ بَلْدَةٌ طَيِّبَةٌ وَرَبٌّ غَفُورٌ، فَأَعْرَضُوا فَأَرْسَلْنَا عَلَيْهِمْ سَيْلَ الْعَرِمِ وَبَدَّلْنَاهُم بِجَنَّتَيْهِمْ جَنَّتَيْنِ ذَوَاتَيْ أُكُلٍ خَمْطٍ وَأَثْلٍ وَشَيْءٍ مِّن سِدْرٍ قَلِيلٍ
" There was for [the tribe of] Saba' in their dwelling place a sign: two [fields of] gardens on the right and on the left. [They were told], "Eat from the provisions of your Lord and be grateful to Him. A good land [have you], and a forgiving Lord. But they turned away [refusing], so We sent upon them the flood of the dam, and We replaced their two [fields of] gardens with gardens of bitter fruit, tamarisks and something of sparse lote trees."
The consequent failure of the irrigation system provoked the migration of up to 50,000 people from Yemen to other areas of the Arabian Peninsula, and even to Syria and Iraq.
The Dam and the Location of the Lost City of Ubar
Soil surveys show that the location of the dam may have been near the city of Ubar. During mapping for the Wadi al Jubal Archaeological Project in Yemen, USGS Geologists Overstreet and Grolier mapped anthrosols of pre-Islamic age east of the Ma'rib dam site (15 degrees 24’N, 45 degrees 18’E). These soils were the result of agriculture supported by irrigation enabled by water impounded by the dam, areas which were abandoned after dam failure. During analysis of Landsat Thematic Mapper satellite images of Yemen and Oman for the Mahra Archaeological Project, we noted that these anthrosols had a distinctive image expression. Many anthrosol sites were noted, most, but not all, of them previously documented. Undocumented possible anthrosol sites include an area east of Shisr in Oman, the archaeological site discovered by us to be responsible for some features of the Lost City of Ubar legends. Included in legendary accounts of the Ubar region are reports of fertile oases, and areas that have known the plow. Based on demonstrated reliability of aspects of carefully interpreted legendary accounts, we postulate that we may have located the area of desert agriculture that may have existed to support the frankincense caravansary of Ubar. The possible anthrosol area is located at approximately 18 degrees 10’N, 53 degrees 54’E, and will be the subject of study in a future expedition.
The current dam
A new dam was then built more recently, close to the location of the old one, at the expense of Shaykh Zayed Bin Sulṭān Āl Nayhān, the late ruler of the United Arab Emirates, whose tribe resettled from Ma'rib to the present UAE some time in the 17th century. The opening ceremony took place in 1986 in the presence of His Highness Shaykh Zayed.
The new dam is 38 m high, 763 m long, built of earth across the Wadi Dhana at wadi bed at the new dam site consists of alluvial sand and gravel material 30–50 m thick. Seepage emanates from this dam that does not threaten its structure,but does lose water. As a way of capturing the seepage, consideration is being given to rebuilding the ancient Ma'rib dam, both as a functioning structure, and also as a historic monument and tourist attraction. The complexity and volume of work involved in this project make it necessary that several organizations work together under the aegis of UNESCO, using financial contributions from international organizations., creating a storage capacity of 398 million cubic meters. The dam site is located 3 km upstream of the ruins of the old Ma'rib dam. The new dam, like the old, was designed to store water for irrigating the Ma'rib plains. However, the
Newly constructed dams in Yemen, such as Batis Dam and Ma'rib, are used to collect water for the population. A newspaper wrote in July 2010: "The water level in the Ma'rib Dam has risen to 45 million cubic meters as a result of the heavy rainfall in various areas of Yemen in the past two days. Under-Secretary of Ma'rib province, Ali Muhammad al-Fatimid, was briefed Tuesday on the amount of water flowing into the dam and the maintenance of drainage channels and sub systems. The Deputy Director of the Ma'rib Dam Project, Engineer Ahmed al-Arifi, said the water level in the dam on Tuesday rose to 45 million cubic meters, while the water level last April rose to 100 million cubic meters. The gate of the main channel for groundwater was opened in the valley of Ubaida for three months, where the quantity of water flowing amounted to 80 million cubic meters."
Ma'rib Dam was built without an environmental impact assessment study, and some of the effects of the dam were not anticipated. In 1995 and 1996 its impact on water quality, agriculture and groundwater recharge and socioeconomics was studied. Lake water could become overly laden with plant nutrients when floods are weak and algae growth is not controlled. Introducing Tilapia nilotica provided biological control of algae growth. The dam positively affected agriculture and groundwater within the designed irrigation scheme, but negatively affected them beyond it. The dam also negatively affected health conditions in the lands downstream, while increasing conflicts over water distribution. It positively affected women by allowing them to work in agriculture and participate in decision-making. The dam raised income levels of farmers and encouraged tourism.
- chp 2 Donald Routledge Hill, A history of engineering in classical and medieval times Routledge, 1996
- Ocean highways: geographical record, ed. C.R. Markham. Ocean highways; geographical review. Vol. 1
- Yāqūt al-Ḥamawī: Mu’jam al-Buldān.
- In his eighth volume of the Annals.
- Yāqūt al-Ḥamawī: Mu'jam al-Buldān. Vol. 4, pg. 383.
- The inscription by Abrahah was first published by Eduard Glaser, in the journal Mitteilungen der vorderasiatischen Gesellschaft, Berlin, 1897. Pp. 360-488.
- Jürgen D. Garbrecht and Guenther K. H. Garbrecht. 2004. Siltation Behind Dams in Antiquity. ASCE. Water Resources and Environmental History. Page(s): 35-43. Water resources and environmental history (proceedings of conference June 27-July 1, 2004, Salt Lake City, Utah; sponsored by Environmental and Water Resources Institute (EWRI) of ASCE, EWRI National History & Heritage Committee, Utah Section of ASCE, and West Consultants, Inc.). ISBN 0-7844-0738-X.
- Moric, Peter. 1997. “Questioning the Need for Spillways.” Wilmington Publishing Ltd, Wilmington House, Church Hill, Wilmington, Dartford, Kent, UK. International Water Power & Dam Construction. Volume: 49, no. 1, page(s): 24-24-26. Abstract: The design of the dam project is discussed focusing on the necessity for spillways and how to determine their overall design. Challenges encountered, factors considered during the design process are discussed and the implications of rare flood conditions are described. ISSN: 0306-400X.
- Translation by Sahih International.
- Blom, Ronald G., Crippen, Robert E. and Zarins, Juris. 1998 “Possible Ancient Anthrosols Near Lost City of Ubar Site in Oman; Geological Society of America, 1998 Annual Meeting.” Abstracts with Programs - Geological Society of America. Geological Society of America, Boulder, CO. Volume 30, Issue 7, Pages 123. ISSN: 0016-7592.
- Ganchikov, VG and Munavvarov, ZI. 1991. “The Marib Dam (History and the Present Time).” Hydrotechnical Construction HYCOAR. Vol. 25, No. 4. October. Volume p 242-248, Pages 1991. (Translated from Gidrotekhnicheskoe Stroitel'stvo, No. 4, pp. 50–55, April 1991) ISSN: 1930-630X.
- “High water levels in Ma'rib and Batis Dams.” 2010. Yemen Today. July 14, 2010.
- Basahi, I. A. A. 2000. “Marib Dam: The Importance of Environmental and Health Impact Studies for Development Projects.” East. Mediterr. Health J. Volume 6, Issue 1, Pages 106-117. ISSN: 1020-3397.
- A Study of the Marib Dam and Its Sluice System (115 B.C. - 575 A.D.)
- Link to Ancient Marib Dam on Google Maps
- Alessandro de Maigret. Arabia Felix, translated Rebecca Thompson. London: Stacey International, 2002. ISBN 1-900988-07-0
- Andrey Korotayev. Ancient Yemen. Oxford: Oxford University Press, 1995. ISBN 0-19-922237-1.
- Hadden, Robert Lee. 2012. The Geology of Yemen: An Annotated Bibliography of Yemen's Geology, Geography and Earth Science. Alexandria, VA: US Army Corps of Engineers, Army Geospatial Center.