Manuel Berberian

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Manuel Berberian
Manuel Berberian.jpg
Manuel Berberian in October 2010
Born (1945-10-27) October 27, 1945 (age 78)
NationalityIranian American
EducationPh.D. (University of Cambridge, UK)
Occupation(s)Earthquake seismology, Geophysics, Active tectonics, Archaeoseismology, environmental geoscience, Professor emeritus
Website http://manuelberberian.com/

Manuel Berberian is an Iranian-Armenian earth scientist. He was born on the 27th of October, 1945 into an immigrant Armenian family in Tehran. He specializes in earthquake seismology, active faulting and folding, active tectonics, continental tectonics, historical seismicity, archaeoseismicity, earthquake hazard minimization, geological mapping, and environmental science and engineering. [1]

Contents

Biography

Berberian was born on October 27, 1945, into an immigrant Armenian family in Tehran. The family had previously fled Armenia [ citation needed ] during the Armenian genocide. His mother is an Assyrian Christian from Rezaiyeh, a city in the Azerbaijani-speaking region of Northwest Iran. [2]

He attended primary school and high school in Iran, graduating in 1958 and 1964 respectively. He received a B.S. in geology with high honors from the University of Tehran in 1968. Since 1971 he has been engaged in scholarly research, He has taught at the University of Tehran, Tarbiat Modares University, Tehran and Ocean County College in New Jersey. He joined the Geological Survey of Tehran in 1971, and established the Tectonics and Seismotectonics Research Department. [2]

He married his wide Rose in Grenoble, France in 1976. She holds a master's degree in mineralogy from the University of Grenoble. They lived together in Tehran for two years before relocating to the United Kingdom [2]

Berberian received his Ph.D. in earthquake seismology and active tectonics from the University of Cambridge, United Kingdom, in June 1981. His dissertation advisors were Geoffrey King and Dan McKenzie. He completed his dissertation called "Continental Deformation in the Iranian Plateau", becoming the first Armenian and second Iranian graduate of the Earth Science Department of the University of Cambridge. (His wife was the first Iranian woman to complete a Ph. D. at Cambridge). [2]

Since 1990, Barberian, his wife and son are living in the United States.

Honors

2013: The First Iranian and First Armenian Earth Scientist ever honored by the Geological Society of America (GSA) during its 125th Anniversary Annual Conference Special Meeting Dedicated to his over 40-yr of research and contribution to the world Earth Science at Denver, Colorado, United States, in October 2013, Sessions 214 & 291, T188: Tethyan Evolution and Seismotectonics of Southwest Asia (GSA Structural Geology and Tectonics Division; GSA Quaternary Geology & Geomorphology Division; GSA Mineralogy, Geochemistry, Petrology, & Volcanology Division). [3]

2008: A new fossil species of Chondrichthyes (jawed fish) named in honor of Berberian in recognition of his contribution to the tectonic evolution of the Iranian Plateau. [4] [5] [6]

Related Research Articles

<span class="mw-page-title-main">Seismology</span> Scientific study of earthquakes and propagation of elastic waves through a planet

Seismology is the scientific study of earthquakes and the generation and propagation of elastic waves through the Earth or other planetary bodies. It also includes studies of earthquake environmental effects such as tsunamis as well as diverse seismic sources such as volcanic, tectonic, glacial, fluvial, oceanic microseism, atmospheric, and artificial processes such as explosions and human activities. A related field that uses geology to infer information regarding past earthquakes is paleoseismology. A recording of Earth motion as a function of time, created by a seismograph is called a seismogram. A seismologist is a scientist works in basic or applied seismology.

<span class="mw-page-title-main">1978 Tabas earthquake</span> 7.4 Mw earthquake in east-central Iran

The 1978 Tabas earthquake occurred on September 16 at 19:05:55 local time in central Iran. The shock measured 7.4 on the moment magnitude scale and had a maximum Mercalli intensity of IX+ (Violent). The death toll was in the range of 15,000–25,000, with severe damage occurring in the town of Tabas.

The Lamont–Doherty Earth Observatory (LDEO) is the scientific research center of the Columbia Climate School, and a unit of The Earth Institute at Columbia University. It focuses on climate and earth sciences and is located on a 189-acre campus in Palisades, New York, 18 miles (29 km) north of Manhattan on the Hudson River.

<span class="mw-page-title-main">Don L. Anderson</span> American geophysicist

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<span class="mw-page-title-main">1990 Manjil–Rudbar earthquake</span> 1990 severe earthquake centered in northeastern Iran

The 1990 Manjil–Rudbar earthquake occurred on Thursday, 21 June 1990 at 00:30:14 local time in the Caspian Sea region of northern Iran. The shock had a moment magnitude of 7.4 and a Mercalli Intensity of X (Extreme). Devastation occurred in a 20,000 km2 (7,700 sq mi) area, causing extensive damage in several cities. A large aftershock also added to the destruction. Between 35,000 and 50,000 people died in the earthquake; another 60,000–105,000 were injured.

James Anthony Jackson CBE FRS is Professor of Active Tectonics and head of Bullard Laboratories, Department of Earth Sciences, Cambridge University. He made his name in geophysics, using earthquake source seismology to examine how continents are deformed. His central research focus is to observe the active processes shaping our continents.

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The 1962 Buin Zahra earthquake occurred on September 1 in the area of Buin Zahra, Qazvin Province, Iran. The shock had a Richter magnitude of 7.1 and resulted in 12,225 fatalities. Qazvin Province lies in an area of Iran that experiences large earthquakes. The 1962 event originated on one of many faults in the area, called the Ipak Fault. The fault is believed to have been reactivated multiple times.

The 1909 Borujerd earthquake also known as Silakhor earthquake occurred in Silakhor plain, Persia on January 23. Around 8,000 fatalities were caused directly from the magnitude 7.3 earthquake. An indefinite number of aftershocks continued for six months after the main shock. The section on this fault ruptured was the same as the main rupture zone of the 2006 Borujerd earthquake.

<span class="mw-page-title-main">Jack Oliver (scientist)</span> American scientist

John "Jack" Ertle Oliver was an American scientist. Oliver, who earned his PhD at Columbia University in 1953, studied earthquakes and ultimately provided seismic evidence supporting plate tectonics. In the 1960s, Oliver and his former graduate student, Bryan Isacks, set up seismographic stations in the South Pacific to record earthquake activity, and the data collected led to the insight that part of the ocean floor was being pushed downward.

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<span class="mw-page-title-main">Walter D. Mooney</span> Research seismologist and geophysicist

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Gurban Jalal Yetirmishli — doctor of geological-mineralogical sciences, corr. member of Azerbaijan National Academy of Sciences (ANAS).
General director of Republican Seismic Survey Center of ANAS head of seismology division

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The 1979 Ghaenat earthquakes were a series of large earthquakes in Qaen County, Khorasan Province, northeast Iran, near the Afghanistan border. The first mainshock, known as the Korizan earthquake with a surface wave magnitude (Ms ) of 6.6 and moment magnitude (Mw ) of 6.8, struck on November 14, while the Ms  7.1 or Mw  7.2 Koli-Boniabad earthquake struck on November 27. The two mainshocks were assigned a maximum Modified Mercalli intensity of VIII (Severe) and X (Extreme), respectively. The earthquakes caused extensive damage throughout northeastern Iran, killing an estimated 297 to 440 people and left at least 279 injured.

The 1997 Bojnurd earthquake occurred on 4 February at 14:07 IRST in Iran. The epicenter of the Mw 6.5 earthquake was in the Kopet Dag mountains of North Khorasan, near the Iran–Turkmenistan border, about 579 km (360 mi) northeast of Tehran. The earthquake is characterized by shallow strike-slip faulting in a zone of active faults. Seismic activity is present as the Kopet Dag is actively accommodating tectonics through faulting. The earthquake left 88 dead, 1,948 injured, and affected 173 villages, including four which were destroyed. Damage also occurred in Shirvan and Bojnord counties. The total cost of damage was estimated to be over US$ 30 million.

The 1977 Khurgu earthquake struck southern Iran near Bandar Abbas in Hormozgan province on the morning of March 22. The earthquake measuring moment magnitude (Mw ) 6.7 struck at a depth of 12.5 km (7.8 mi). Thirty five villages were heavily damaged including over 20 which were destroyed. There were 152–167 people killed and 556 injured.

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References

  1. "Manuel Berberian". Independent Academia.
  2. 1 2 3 4 Sorkhabi, R. "Manuel Berberian: An appreciation and bibliography of his lifelong contribution to geoscience: Tectonic Evolution, Collision, and Seismicity of Southwest Asia In Honor of Manuel Berberian's Forty-Five Years of Research". The Geological Society of America. doi:10.1130/2016.2525(02).
  3. "GSA Annual Meeting and Exposition, 125-year Anniversary". GSA 2013. Denver, CO, United States: 259, 290. Oct 2013.
  4. Ginter, M.; Hampe, O.; Duffin, C.J. Schultze, H.-P (ed.). Handbook of Paleoichthyology. p. 168.
  5. Ginter, M.; Liano, J.-C.; Valenzuela-Rios (2008). "New data on Chondrichthyan microremains from the Givetian of the Renanué section in the Anagonian Pyrenees (Spain)". Acta Geologica (58): 165–172.
  6. Hairapetian, V.; Ginter, M.; Yazdi, M. (2008). "Early Fransian sharks from Central Iran". Acta Geologica Polonica. 58 (2): 173–179.