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Elizavetpol Governorate
The Elizavetpol Governorate, also known after 1918 as the Ganja Governorate, was a province ('' guberniya'') of the Caucasus Viceroyalty of the Russian Empire, with its capital in Yelisavetpol (present-day Ganja). The area of the governorate stretched and was composed of 1,275,131 inhabitants in 1916. The Elizavetpol Governorate bordered the Erivan Governorate to the west, the Tiflis Governorate and Zakatal Okrug to the north, the Dagestan Oblast to the northeast, the Baku Governorate to the east, and Iran to the south. Geography The area of the governorate includes the southern slope of the main Caucasus range in the northeast, where Mount Bazardüzü and other peaks rise above the snow-line; the arid steppes beside the Kura river, reaching 1000 ft. of altitude in the west and sinking to 100–200 ft. in the east, where irrigation is necessary; and the northern slopes of the Transcaucasian escarpment and portions of the Armenian Highlands, which is intersected towards i ...
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Mount Bazardüzü
Mount Bazardüzü (, ; lez, Кичӏен сув ; russian: Базардюзю, ) is a mountain peak in the Greater Caucasus range on the border between Dagestan, Russia and Azerbaijan. At above sea level, it is the highest peak in both Dagestan and Azerbaijan, and is located in the Qusar region. The southernmost point of Dagestan (and therefore Russia) is located about seven kilometers southwest of the peak. Translated from Azerbaijani, Bazarduzu means “market square”, more precisely as a specific landmark - “turn to the market, bazaar”. In the Middle Ages in the Shahnabad Valley, located east of this peak, annual large multinational fairs were held. Climbing G. P. Baker and G. Yeld were the first men climbing the Mount in 1890 when the first ascent was recorded. Summer is considered the most appropriate period to climb the peak. There are two approaches to the Mount: one from the northeast and another from the southwest. In the northeast climbs can begin from the vi ...
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Transcaucasia
The South Caucasus, also known as Transcaucasia or the Transcaucasus, is a geographical region on the border of Eastern Europe and Western Asia, straddling the southern Caucasus Mountains. The South Caucasus roughly corresponds to modern Armenia, Georgia, and Azerbaijan, which are sometimes collectively known as the Caucasian States. The total area of these countries measures about . The South Caucasus and the North Caucasus together comprise the larger Caucasus geographical region that divides Eurasia. Geography The South Caucasus spans the southern portion of the Caucasus Mountains and their lowlands, straddling the border between the continents of Europe and Asia, and extending southwards from the southern part of the Main Caucasian Range of southwestern Russia to the Turkish and Armenian borders, and from the Black Sea in the west to the Caspian Sea coast of Iran in the east. The area includes the southern part of the Greater Caucasus mountain range, the entire Lesser C ...
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Jevanshir Uezd
The Jevanshir uezd was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire, with its center in Terter (present-day Tartar). Geography The Jevanshir uezd was made up of two parts, the northeastern lowland and the southwestern mountainous part of Jraberd. The area covered 4,818.4 square verst. The lower part, called Arran was hot and dry during summers which made the inhabitants move to mountainous areas for the duration of season. The winters were mild and short. The middle part of the uezd is located on the hills and is enriched with forests. The southern part is located high in the mountains. The highest peaks in mountainous ranges stretching from Gokcha are Murovdag (11,219 ft), Gozeldere-bashi (11,606 ft) and Ginal-dag (11,057 ft). A big part of Jevanshir uezd is within the Tartarchay basin, which starts high in the mountains near the border with the Nor Bayazet and Zangezur ''uezds'' and flows through uezd discharging into Kura. The impo ...
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Jebrail Uezd
The Jebrail uezd, also known after 1905 as the Karyagino uezd, was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire with its center in Jebrail (Jabrayil) from 1873 until its formal abolition in 1921 by the Soviet authorities. Geography The Jabrayil uezd was located in the southeastern part of Elizavetpol Governorate bordering its Shusha uezd to the north, Zangezur uezd to the west, Baku Governorate to the east, and Persia to the south. The area of the uezd was 2922.6 square verst. The northwestern part of the uezd is mountainous. Mount Ziyarat ( az, Ziyarət) or Dizapayt ( hy, Դիզափայտ) reaches 8,186 feet. The higher ground was usually used for pastures. The whole uezd was located within the Araz river basin. The tributaries of Araz, Kendalan, Kuru-chay, Chereken, Gozlu-chay and Hakari-chay were utilized for irrigation. History The territory of the uezd had previously formed a part of the Karabakh Khanate until 1813, when according to Gulistan Tre ...
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Aresh Uezd
The Aresh ''uezd'' was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire and later of the Azerbaijan Democratic Republic with its center in Aresh (present-day Agdash) from 1874 until its formal abolition in 1929 by Soviet authorities. Geography The Aresh ''uezd'' was located in the northeastern section of Elizavetpol Governorate, on the eastern bank of the Kura River, bordering the Baku Governorate to the east, the Nukha uezd to the north, the Elizavetpol uezd to the northwest and Jebrail uezd to the southwest. The area of the ''uezd'' was 2822.9 square verst. The territory of the county was mainly made up of lowlands. The county capital was initially in Uchkovakh, later being moved to Agdash, which was considered the largest cotton-trading center in the lowlands of Transcaucasia. History The territory of Aresh ''uezd'' was located in the Turyanchay River basin. The area was called ''Aresh'' ( az, Ərəş) in the Middle Ages and formed a part of Shirva ...
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Zangezur Uezd
The Zangezur uezd was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire with its administrative center in Gerusy (present-day Goris) from 1868 until its formal abolition and partition between the Soviet republics of Armenia and Azerbaijan in 1921. The area of the Zangezur uezd corresponded to most of the contemporary Syunik province of Armenia, and Lachin, Gubadly, Zangilan, and Shusha districts of Azerbaijan. Geography Almost the entirety of the area is mountainous with many gorges and valleys of the Lesser Caucasus mountain range. The altitude ranges from 10,000–12,855 feet at Mount Kaputjugh, a mountain range which forms the natural boundary between the governorates of Elizavetpol and Erivan. The rivers of the Zangezur uezd are located within the Aras River basin—The Bargushad, Chaundurchay, , and Megrichay rivers played important roles in the irrigation system of the ''uezd''. History Historically, the Zangezur region was part of the Syunik pro ...
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Kazakh Uezd
The Kazakh uezd was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire and later of the Azerbaijan Democratic Republic with its center in Kazakh (present-day Qazax) from 1868 until its formal abolition in 1929 by the Soviet authorities of the Azerbaijan SSR. The area of the Kazakh uezd forms a large part of the modern-day Tavush Province and a small northeastern part of the Gegharkunik Province of Armenia, also forming most of the area of the Agstafa, Tovuz and Qazax districts of Azerbaijan. Geography The Kazakh uezd was located in the northwestern part of Elizavetpol Governorate, bordering the Tiflis Governorate in the north, the Erivan Governorates in the southwest, and the Elizavetpol uezd in the east. The area of the uezd was 6024.2 square versts. The southwestern part of the uezd was mountainous, whereas the northeastern part mainly consisted of lowlands. Two-thirds of uezd was covered by Sevan or Shah-dagh mountain range of Lesser Caucasus which forme ...
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Shusha Uezd
The Shusha uezd was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire, and then of the Ganja Governorate of Azerbaijan Democratic Republic with its center in Shusha in 1840–1921. Geography The Shusha uezd was located in the southeastern portion of Elizavetpol Governorate, bordering the contiguous Jevanshir uezd on the north, the Jebrail uezd to the south, the Zangezur uezd to the west and the Baku Governorate in the east. The area covered 4,316 square verst, or . The uezd was normally divided into the mountainous, submountanous and lowland parts. The mountains covered the southwestern part of the uezd and were part of the Lesser Caucasus range, reaching as high as above sea level. The gorges and valleys towards the northeast made up the submountainous areas of the uezd. The lowland part of the uezd is rich with rivers. The Khachinchay river formed the natural boundary between the Shusha and the Javanshir uezds. History The territories of Shusha uezd once ...
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Nukha Uezd
The Nukha uezd was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire and later of the Azerbaijan Democratic Republic with its center in Nukha (present-day Shaki) from 1868 until its formal abolition in 1921 by the Soviet authorities of the Azerbaijan SSR. Geography The Nukha uezd was located in the far northeastern part of the Elizavetpol Governorate, bordering the Dagestan Oblast to the north, the Baku Governorate to the east, the Zakatal Okrug to the west, and the Aresh uezd to the south. The administrative center of the Nukha uezd was the city of Nukha. The northern part of the uezd was largely mountainous and laid along the Greater Caucasus mountain range, where the altitude reaches as high as 14-15 thousand feet in altitude. The notable peaks of the district included Mount Bazardüzü (14,722 ft) and Tkhfan Dag (13,764 ft) whose valleys were enriched with many rivers. The southern part of the region possessed the best conditions for agricultu ...
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Elizavetpol Uezd
The Elizavetpol uezd, also known as the Ganja uezd after 1918, was a county (''uezd'') of the Elizavetpol Governorate of the Russian Empire, and later of the Azerbaijan Democratic Republic and Azerbaijan SSR until its formal abolition in 1929. The area of the Elizavetpol uezd corresponds to the modern-day Gadabay, Shamkir, Dashkasan, Goygol, and Samukh districts of Azerbaijan. Geography The Elizavetpol uezd was located in the northern part of Elizavetpol Governorate, bordering the Tiflis Governorate to the north, the Kazakh uezd to the west, the Aresh uezd to the east and Jevanshir uezd to the south. The administrative center of the uezd was the city of Yelisavetpol (Ganja). The area of the ''uezd'' was 8,726 square verst and was divided into two parts: the northeastern lowlands steppes, irrigated by Kura River and its tributaries and southwestern mountainous part, watered by Kura's right bank tributaries. The lowland part was split by the Kura and Alazani rivers, the latter ...
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Aras (river)
, az, Araz, fa, ارس, tr, Aras The Aras (also known as the Araks, Arax, Araxes, or Araz) is a river in the Caucasus. It rises in eastern Turkey and flows along the borders between Turkey and Armenia, between Turkey and the Nakhchivan exclave of Azerbaijan, between Iran and both Azerbaijan and Armenia, and, finally, through Azerbaijan where it flows into the Kura river. It drains the south side of the Lesser Caucasus Mountains while the Kura drains the north side of the Lesser Caucasus. The river's total length is and its watershed covers an area of . The Aras is one of the longest rivers in the Caucasus. Names In classical antiquity, the river was known to the Greeks as Araxes ( gr, Ἀράξης). Its modern Armenian name is ''Arax'' or ''Araks'' ( hy, Արաքս). Historically it was also known as ''Yeraskh'' ( xcl, Երասխ) and its Old Georgian name is ''Rakhsi'' (). In Azerbaijani, the river's name is ''Araz''. In Persian and Kurdish its name is (''Aras''), an ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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