1139 Ganja Earthquake
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1139 Ganja Earthquake
The 1139 Ganja earthquake is one of the worst seismic events in history. It affected the Seljuk Empire and Kingdom of Georgia; modern-day Azerbaijan and Georgia. The earthquake had an estimated magnitude of 7.7 or 7.0–7.3 . An estimated but controversial death toll of 230,000–300,000 came as a consequence of this event. Tectonic setting Azerbaijan and Georgia is located in an area of high seismic activity as both countries are situated in the collision zone between the Eurasian and Arabian Plates. The collision zone consists of an accreted island arc that collided after the closure of the Tethys Ocean, continental blocks, and sediments from the Mesozoic and Tertiary eras. The area is separated into three geographical regions; Lesser Caucasus, Kura Basin and Greater Caucasus. Seismic activity in the Lesser Caucasus is typically associated with strike-slip faults with vertical dip angles. In the Greater Caucasus, seismic activity correspond to thrust faulting. Extending 100 ...
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Seljuk Empire
The Great Seljuk Empire, or the Seljuk Empire was a high medieval, culturally Turco-Persian tradition, Turko-Persian, Sunni Islam, Sunni Muslim empire, founded and ruled by the Qiniq (tribe), Qïnïq branch of Oghuz Turks. It spanned a total area of from Anatolia and the Levant in the west to the Hindu Kush in the east, and from Central Asia in the north to the Persian Gulf in the south. The Seljuk Empire was founded in 1037 by Tughril (990–1063) and his brother Chaghri Beg, Chaghri (989–1060), both of whom co-ruled over its territories; there are indications that the Seljuk leadership otherwise functioned as a triumvirate and thus included Seljuk dynasty, Musa Yabghu, the uncle of the aforementioned two. From their homelands near the Aral Sea, the Seljuks advanced first into Greater Khorasan, Khorasan and into the Iranian plateau, Iranian mainland, where they would become largely based as a Persianate society. They then moved west to conquer Baghdad, filling up the power va ...
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Mercalli Intensity Scale
The Modified Mercalli intensity scale (MM, MMI, or MCS), developed from Giuseppe Mercalli's Mercalli intensity scale of 1902, is a seismic intensity scale used for measuring the intensity of shaking produced by an earthquake. It measures the effects of an earthquake at a given location, distinguished from the earthquake's inherent force or strength as measured by seismic magnitude scales (such as the "" magnitude usually reported for an earthquake). While shaking is caused by the seismic energy released by an earthquake, earthquakes differ in how much of their energy is radiated as seismic waves. Deeper earthquakes also have less interaction with the surface, and their energy is spread out across a larger volume. Shaking intensity is localized, generally diminishing with distance from the earthquake's epicenter, but can be amplified in sedimentary basins and certain kinds of unconsolidated soils. Intensity scales empirically categorize the intensity of shaking based on the effect ...
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Caucasus Mountains
The Caucasus Mountains, : pronounced * hy, Կովկասյան լեռներ, : pronounced * az, Qafqaz dağları, pronounced * rus, Кавка́зские го́ры, Kavkázskiye góry, kɐfˈkasːkʲɪje ˈɡorɨ * tr, Kafkas Dağları, * fa, كوه هاى قفقاز are a mountain range at the intersection of Asia and Europe. Stretching between the Black Sea and the Caspian Sea, they are surrounded by the Caucasus region and are home to Mount Elbrus, the list of elevation extremes by region, highest peak in Europe at above sea level. The Caucasus Mountains include the Greater Caucasus in the north and Lesser Caucasus in the south. The Greater Caucasus runs west-northwest to east-southeast, from the Western Caucasus, Caucasian Natural Reserve in the vicinity of Sochi, Russia on the northeastern shore of the Black Sea to Baku, Azerbaijan on the Caspian Sea. The Lesser Caucasus runs parallel to the Greater about south. The Greater and Lesser Caucasus ranges are co ...
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Gandzak, Armenia
Gandzak ( hy, Գանձակ) is a village in the Gavar Municipality of the Gegharkunik Province of Armenia. The village is located on the eastern side of the Gavar river, 3 km southwest from the regional center Gavar, at an average height of 1,980 meters above sea level. Etymology The village was previously known as ''Batikian'' and ''Batikyan'', in honor of Batik Batikian The May Uprising ( hy, Մայիսյան ապստամբություն, translit=Mayisyan apstambutyun) was a coup d'état attempt by the Armenian Bolsheviks that started in Alexandropol (modern-day Gyumri) on May 10, 1920. It was eventually suppr ... (1892–1920), a Communist activist. History The village contains the 4th- or 5th-century half-ruined basilica of St. Astvatsatsin, and the domed 9th- or 10th-century St. Gevorg Church, in ancient times it had a domed hall. In the 19th century, Armenian migrants from Western Armenia covered the destroyed roofs with the logs. Gallery Gandzak 07.jpg, Sc ...
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Kingdom Of Syunik
Kingdom of Syunik ( hy, Սյունիքի թագավորություն), also known as the Kingdom of Baghk and sometimes as the Kingdom of Kapan, was a medieval dependent Armenian kingdomArmenia and Iran
// "''In 1162, eastern Armenia was attacked by the atabeg Īldegoz of Azerbaijan. In 1170, with a new invasion, the Armenian Kingdom of Siunikʿ was terminated.''"
Armenia
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Holy Bible
The Bible (from Koine Greek , , 'the books') is a collection of religious texts or scriptures that are held to be sacred in Christianity, Judaism, Samaritanism, and many other religions. The Bible is an anthologya compilation of texts of a variety of forms originally written in Hebrew, Aramaic, and Koine Greek. These texts include instructions, stories, poetry, and prophecies, among other genres. The collection of materials that are accepted as part of the Bible by a particular religious tradition or community is called a biblical canon. Believers in the Bible generally consider it to be a product of divine inspiration, but the way they understand what that means and interpret the text can vary. The religious texts were compiled by different religious communities into various official collections. The earliest contained the first five books of the Bible. It is called the Torah in Hebrew and the Pentateuch (meaning ''five books'') in Greek; the second oldest part was a coll ...
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Psalm 103
Psalm 103 is the 103rd psalm of the Book of Psalms, beginning in English in the King James Version: "Bless the , O my soul". The Book of Psalms is part of the third section of the Hebrew Bible, and a book of the Christian Old Testament. In Latin, it is known as "Benedic anima mea Domino". The psalm is a hymn psalm. In the slightly different numbering system used in the Greek Septuagint and Latin Vulgate translations of the Bible, this psalm is Psalm 102. The first verse (the sub-heading in most English translations) attributes the psalm to King David. The psalm forms a regular part of Jewish, Catholic, Lutheran, Anglican and other Protestant liturgies. The psalm has been paraphrased in hymns, and has often been set to music. Background and themes Baptist preacher and biblical commentator Charles Spurgeon suggests that the psalm was written in David's later life, as seen by the psalmist's focus on the frailty of life and his "higher sense of the preciousness of pardon, because ...
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Job 9
Job 9 is the ninth chapter of the Book of Job in the Hebrew Bible or the Old Testament of the Christian Bible.Holman Illustrated Bible Handbook. Holman Bible Publishers, Nashville, Tennessee. 2012. The book is anonymous; most scholars believe it was written around 6th century BCE. This chapter records the speech of Job, which belongs to the Dialogue section of the book, comprising Job 3:1– 31:40. Text The original text is written in Hebrew language. This chapter is divided into 35 verses. Textual witnesses Some early manuscripts containing the text of this chapter in Hebrew are of the Masoretic Text, which includes the Aleppo Codex (10th century), and Codex Leningradensis (1008). Fragments containing parts of this chapter in Hebrew were found among the Dead Sea Scrolls including 4Q100 (4QJob; 50–1 BCE) with extant verse 27. There is also a translation into Koine Greek known as the Septuagint, made in the last few centuries BC; some extant ancient manuscripts of this ve ...
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Armenians
Armenians ( hy, հայեր, ''hayer'' ) are an ethnic group native to the Armenian highlands of Western Asia. Armenians constitute the main population of Armenia and the ''de facto'' independent Artsakh. There is a wide-ranging diaspora of around five million people of full or partial Armenian ancestry living outside modern Armenia. The largest Armenian populations today exist in Russia, the United States, France, Georgia, Iran, Germany, Ukraine, Lebanon, Brazil, and Syria. With the exceptions of Iran and the former Soviet states, the present-day Armenian diaspora was formed mainly as a result of the Armenian genocide. Richard G. Hovannisian, ''The Armenian people from ancient to modern times: the fifteenth century to the twentieth century'', Volume 2, p. 421, Palgrave Macmillan, 1997. Armenian is an Indo-European language. It has two mutually intelligible spoken and written forms: Eastern Armenian, today spoken mainly in Armenia, Artsakh, Iran, and the former Soviet ...
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Mkhitar Gosh
Mkhitar Gosh ( hy, Մխիթար Գոշ; 1130–1213) or Mkhitar the Thinbearded was an Armenian scholar, writer, public figure, thinker, and priest. He was one of the representatives of the Armenian Renaissance. Biography He was born in the city of Gandzak . He got his early education from public institutions. When he reached his adolescence he decided to dedicate his life to the church. In order to learn theology more thoroughly, Gosh traveled to Cilicia, to the Black Mountains (Սև լեռներ) and studied orthodox theology under the local priests. Upon his return, he, along with the princes' Zakare and Ivane Zakarian financial help, built the Ghetik (Գետիկ) church. He wrote a code of laws including civil and Canon law that was used in both Greater Armenia and Cilicia. It was also used in Poland, by order of king Sigismund the Old, as the law under which the Armenians of Lviv and Kamianets-Podilskyi lived from 1519 until the region fell under Austrian rule in 1772. He a ...
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1931 Zangezur Earthquake
The 1931 Zangezur earthquake occurred on April 27 at with a moment magnitude of 6.5. The earthquake was located in the Zangezur Mountains near the boundary between southwestern Armenia and Azerbaijan's exclave, the Nakhichivan Autonomous Republic. Both territories were part of the Soviet Union at that time. Tectonic setting The Pambak-Sevan-Sunik Fault extends in the NW–SE direction. The fault can be traced continuously for 400 km and consists of four major segments. The 1931 Zangezur earthquake was located in the area of the Sunik-Zanghezour segment, which is about 120 km long. The fault was also the source of the magnitude 7.5+ 1139 Ganja earthquake; the largest and most destructive seismic event in the Caucasus. Earthquake The earthquake was located near the border between the Syunik Province of Armenia (''Zangezur'' is an alternative name for the region of Syunik Province) and the Nakhichivan Autonomous Republic of Azerbaijan. Up to 2,890 were reported dead. In ...
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Paleoseismology
Paleoseismology looks at geologic sediments and rocks, for signs of ancient earthquakes. It is used to supplement seismic monitoring, for the calculation of seismic hazard. Paleoseismology is usually restricted to geologic regimes that have undergone continuous sediment creation for the last few thousand years, such as swamps, lakes, river beds and shorelines. In this typical example, a trench is dug in an active sedimentation regime. Evidence of thrust faulting can be seen in the walls of the trench. It becomes a matter of deducting the relative age of each fault, by cross-cutting patterns. The faults can be dated in absolute terms, if there is dateable carbon, or human artifacts. Many notable discoveries have been made using the techniques of paleoseismology. For example, there is a common misconception that having many smaller earthquakes can somehow 'relieve' a major fault such as the San Andreas Fault, and reduce the chance of a major earthquake. It is now known (u ...
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