Umm al Binni lake

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Umm al Binni Lake
LocationMaysan Governorate
Coordinates31°14′29″N 47°06′21″E / 31.24139°N 47.10583°E / 31.24139; 47.10583Coordinates: 31°14′29″N 47°06′21″E / 31.24139°N 47.10583°E / 31.24139; 47.10583
Lake typeformer lake
Basin countriesIraq
Max. length3.4 km (2.1 mi)
Max. depth3 m (9.8 ft)

Umm al Binni lake is a mostly dry lake within the Central Marshes in Maysan Governorate in southern Iraq. The 3.4 km (2.11 miles) wide lake is approximately 45 km northwest of the TigrisEuphrates confluence. Because of its shape, location, and other details, it has been conjectured to represent an impact crater.

Evidence as an impact crater[edit]

Using satellite imagery, Sharad Master suggests[1][2] the 3.4 km diameter dry lake may be an impact crater based on its nearly circular, slightly polygonal rim shape, and contrasting shape to other lakes in the region. As to its origin, he rules out karst topography, salt doming, tectonic deformation, and igneous intrusion as well as possible bombing or man-made origins. Some structures may initially be found through satellite remote sensing and later established as impact craters like the recently confirmed Santa Marta crater found by Master and J. Heymann.[3][4]

Details and historical context[edit]

Master estimates the age of the crater to be less than 5000 years old, or between 2000−3000 BC,[2] due to the deposition of sediments of the Tigris-Euphrates plain as a result of the 130–150 km seaward progradation[5] of the Persian Gulf during that time period.[1][2] Some relate this apparent impact site to the 2350 BC Middle East anomaly.[6][7] A lack of writings describing this event by well-known authors like Herodotus (484–425 BC) and Nearchus (360–300 BC) or later historians implies the impact may have occurred much earlier, between 2000−3000 BC.[2] During this time period, the Al Amarah region was approximately 10 m. deep under the Persian Gulf.[5] Impact-induced tsunamis would have devastated coastal Sumerian cities. This may provide an alternate origin of the 2.6 m sediment layer discovered during an excavation of the Sumerian city of Ur by Leonard Woolley in 1922-1934. Descriptive passages in The Epic of Gilgamesh (circa 1600–1800 BC) may describe such an impact and tsunami, suggesting a link to the Sumerian Deluge:[8][9]

...and the seven judges of Hell, the Annunaki, raised their torches, lighting the land with their livid flame. A stupor of despair went up to heaven when the god of the storm turned daylight into darkness, when he smashed the land like a cup. One whole day the tempest raged, gathering fury as it went, it poured over the people like tides of battle; a man could not see his brother nor the people be seen from heaven. Even the gods were terrified at the flood, they fled to the highest heaven, the firmament of Anu; they crouched against the walls, cowering like curs.[10]

Climate change and impact effects[edit]

It has been proposed that sudden climate changes and catastrophic events around 2200 BCE (including the collapse of the Sumerian civilisation) could be linked to a comet or asteroid impact.[11][12][13][14][15][16][1] Master[1][17] has conjectured that the alleged Umm al Binni impact could be responsible for this catastrophe, producing the energy equivalent to thousands of Hiroshima-sized bombs.

Using equations describing impact effects based on work from Collins et al.,[18] Shoemaker,[19] Glasstone & Dolan[20] and others, Hamacher[21] determined that an impacting bolide would have produced energy in the range of 190 to 750 megatons of TNT (for an asteroid and comet impact, respectively). For comparison, the Tunguska event was estimated to have an explosive force of about 10-15 megatons.

Hamacher's result is dependent on the impactor's density, size, and impact velocity. In order to produce an impact crater with the dimensions of Umm al Binni lake, a Ni-Fe asteroid (density = 7860 kg/m^3, v = 15 km/s) would have been around 100 m in diameter while a comet (density = 500 kg/m^3, v = 25 km/s) would have been between 200 and 300 m in diameter. The resulting impact effects would have caused massive devastation to an area thousands of square kilometres in size, but would not have been sufficient on its own to have caused the wide-scale damage seen at distances exceeding ~100 kilometers from the impact and thus could not be responsible for many of the more distant devastating effects on its own.

Although a large mount of circumstantial evidence has been published in the literature suggesting Umm al Binni is an impact crater, no on-site analysis has been done, primarily due to the current volatile and dangerous situation in Iraq. Therefore, Umm al Binni lake remains a possible, albeit unconfirmed, impact structure.

See also[edit]

External links[edit]


  1. ^ a b c d Master, S. (2001) A Possible Holocene Impact Structure in the Al Amarah Marshes, Near the Tigris-Euphrates Confluence, Southern Iraq, Meteoritics & Planetary Science 36: A124
  2. ^ a b c d Master, S. (2002) Umm al Binni lake, a possible Holocene impact structure in the marshes of southern Iraq: Geological evidence for its age, and implications for Bronze-age Mesopotamia. In: Leroy, S. and Stewart, I.S. (Eds.), Environmental Catastrophes and Recovery in the Holocene, Abstracts Volume, Department of Geography, Brunel University, Uxbridge, West London, UK, 29 August - 2 September 2002, pp. 56–57
  3. ^ Master, S.; Heymann, J (2000). A Possible New Impact Structure near Gilbués in Piauí Province, Northeastern Brazil, Meteoritics & Planetary Science, vol. 35, Supplement, p.A105
  4. ^ A. P. Crósta and M. A. Vasconcelos (2013). Confirmation Of The Impact Origin Of The Santa Marta Crater, Brazil, 76th Annual Meteoritical Society Meeting
  5. ^ a b Larsen, C.E. and Evans, G. (Brice W.C. Ed.), (1978) The Holocene Geological History of the Tigris-Euphrates-Karun Delta in The Environmental History of the Near and Middle East Since the Last Ice Age. Academic Press, London. pp. 227–244
  6. ^ Courty M-A (1998) Causes and effects of the 2350 BC Middle East anomaly evidenced by micro-debris fallout, surface combustion and soil explosion. In: Peiser BJ, Palmer T, Bailey ME (eds) Natural catastrophes during Bronze Age civilisations: archaeological, geological, astronomical and cultural Perspectives. British Archaeol Reports S728, Archaeopress, Oxford
  7. ^ Google search
  8. ^ Matthews, R. (2001) Meteor clue to end of Middle-East civilisations, Telegraph Online Magazine
  9. ^ Britt, R.R. (2001) Comets, meteors and myth: New evidence for toppled civilisations and Biblical tales, Posted 13 November 2001
  10. ^ Sanders, N.K. (1960) The Epic of Gilgamesh, Penguin Books, London
  11. ^ Master, S. and Woldai, T., (2006 - in press) Umm al Binni structure, southern, as a postulated late Holocene meteorite impact crater: new satellite imagery, and proposals for future research. In: Bobrowsky, P. and Rickmann, H. (Eds.), Comet/Asteroid Impacts and Human Society, Springer-Verlag, Heidelberg
  12. ^ Bjorkman, J.K., (1973) Meteors and Meteorites in the Ancient Near East, Meteoritics 8(2): 91
  13. ^ Weiss, H., Courty, M.-A., Wetterstrom, W., Guichard, F., Senior, L., Meadow, R. and Curnow, A. (1993) The genesis and collapse of Third Millennium North Mesopotamian civilization, Science 261, pp. 995–1004
  14. ^ Courty, M.A., (1997) Causes And Effects of the 2350 BC Middle East Anomaly Evidenced By Micro-debris Fallout, Surface Combustion and Soil Explosion, Society for Interdisciplinary Studies Conference: Natural Catastrophes during Bronze Age Civilizations, July 11–13, 1997 Cambridge, UK.
  15. ^ Peiser, B. (1997) Comets and Disaster in the Bronze Age, British Archaeology 30: 6-7
  16. ^ Napier, W., (1997) Cometary Catastrophes, Cosmic Dust and Ecological Disasters in Historical Times: The Astronomical Framework, Society for Interdisciplinary Studies Conference: Natural Catastrophes during Bronze Age Civilizations, July 11–13, 1997 in Cambridge, UK
  17. ^ Master, S. and Woldai, T., (2004) The Umm al Binni structure in the Mesopotamian marshlands of southern Iraq, as a postulated late Holocene meteorite impact crater, Economic Geology Research Institute Information Circular, October 2004, University of Witwatersrand - Johannesburg
  18. ^ Collins, G. S.; Melosh, H. J.; Marcus, R. A. (2005) Earth Impact Effects Program: A Web-based computer program for calculating the regional environmental consequences of a meteoroid impact on Earth, Meteoritics & Planetary Science 40: 817
  19. ^ Shoemaker, E.M. (1983) Asteroid and comet bombardment of the Earth, Annual Review of Earth and Planetary Sciences 1(1): 461-494
  20. ^ Glasstone, S. and Dolan, P. J., (1977) Effects of Nuclear Weapons 3rd Edition, Washington D.C.: United States, Department of Defense and Department of Energy
  21. ^ Hamacher, D.W. (2005), The Umm Al Binni Structure and Bronze Age Catastrophes, The Artifact: Publications of the El Paso Archaeological Society, vol 43, pp 115–138