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Talysh Mountains
Talysh Mountains ( tly, Tolışə Bandon, script=Latn, fa, کوههای تالش, Kuhhâye Tâleš; az, Talış dağları) is a mountain range in far southeastern Azerbaijan and far northwestern Iran within Ardabil Province and Gilan Province. They are a northwestern subrange of the Alborz Mountains that run along the southern Caspian Sea on the Iranian Plateau. Geography The Talysh Mountains extend southeastward from the Lankaran Lowland in southeastern Azerbaijan to the lower part of the Sefid Rud (''White River'') in northwestern Iran. A few peaks rise above 10,000 ft (3,000 m). Geology Geologically, the Talish Mountain Range is made mainly of the Late Cretaceous volcano-sedimentary deposits with a strip of Paleozoic rocks and a band of Triassic and Jurassic rocks in the southern parts, both in a north-west-southeast direction. Ecology The maximum annual precipitation in the Talysh Mountains is between 1,600 mm to 1,800 mm, which along the Lankaran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Geoscience Database Of Iran
The National Geoscience Database of Iran or in brief NGDIR is a scientific and research government agency in Iran which works in the field of Geology of Iran and centrally manages Geoscience data. This center was established in 1999 in the field of data collection authority with the aim of managing, preserving and sharing Geoscience data. History The core of the National Geoscience Database of Iran (NGDIR) was established in 1999 at the Geological Survey and Mineral Exploration of Iran and its main activities until 2000 is limited to collecting mineral information in the library of the organization and creating the first mineral database and collection and unification of map information in the Geological Survey and Mineral Exploration of Iran. In the same year, the creating of Geoscience Database task was assigned to the Ministry of Industries and Mines (Iran). Since then, the National Geoscience Database of Iran's structure became more independent and thematic development ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yardimli District
Yardimli District ( az, Yardımlı rayonu) is one of the 66 districts of Azerbaijan. It is located in the south-east of the country and belongs to the Lankaran-Astara Economic Region. The district borders the districts of Jalilabad, Masally, Lerik, and the Ardabil Province of Iran. Its capital and largest city is Yardimli. As of 2020, the district had a population of 68,000. History The district was called the village Vargaduz, part of Lankaran Uyezd from 1920 to 1930. Since 1930, it has been renamed the Vargaduz district. It has been named Yardimli region since 1938 and the center of the district was Yardimli. Geography The rayon borders upon Iran (length of the state border in the south and west is equal to 96 km) and Lerik District (40 km), Masally District (11 km), Jalilabad District (20 km) of Azerbaijan. Yardimli is located within the mountainous region in the southern-eastern part of Azerbaijan, within 39 ° -38 ° north longitude, 48 ° -49 ° ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lerik District
Lerik District ( az, Lerik rayonu, tly, Lik rəyon, script=Latn) is one of the 66 districts of Azerbaijan. It is located in the south-east of the country and belongs to the Lankaran-Astara Economic Region. The district borders the districts of Yardimli, Masally, Lankaran, Astara and the Ardabil Province of Iran. Its capital and largest city is Lerik. As of 2022, the district had a population of 87,000. It is located between the Talysh Mountains and the agricultural plain of the Lankaran Lowland. History Lerik district was established in August 1930. It was called ''Zuvand District'' until January 1938. 29 municipalities operate in the district. The district includes a city and 162 villages with a total area of 1084 square kilometer. In accordance with the presidential decree dated June 13, 2008, the settlement of Lerik was granted the status of a city. The territory of the Lerik district is one of the oldest settlements in Azerbaijan. There exist some caves which are consi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lankaran District
Lankaran District (, tly, Lankon rəyon, script=Latn) is one of the 66 districts of Azerbaijan. It is located in the south-east of the country and belongs to the Lankaran-Astara Economic Region. The district borders the districts of Astara, Lerik, Masally, and Neftchala. Its capital and largest city is Lankaran, although the city is technically not part of the district and is subordinate to the Republic. As of 2022, the district had a population of 232,000. History Archaeological excavations indicate that people have lived in the region since at least the Bronze Age (3rd or 2nd millennia BC). The area around Lankaran has fertile soil, rich water reserves and a humid subtropical climate with a maximum annual precipitation of 1,600 to 1,800 mm, the highest precipitation in Azerbaijan, leading to abundant agriculture, cattle-breeding, gardening, fishing, bee-keeping and silk production. Blacksmith, copper-smith, pottery and other trades have long been well established to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Astara District
Astara District ( az, Astara rayonu, tly, Ostoro rəyon, script=Latn) is one of the 66 districts of Azerbaijan. It is located in the south-east of the country and belongs to the Lankaran-Astara Economic Region. The district borders the districts of Lankaran, Lerik, as well as the Ardabil and Gilan provinces of Iran. Its capital and largest city is Astara. As of 2020, the district had a population of 110,000. History Ancient history A famous mathematician, astronomer and geographer Alexandria Claudius Ptolomey (AD 100 – c. 170) was one of the oldest researchers who also visited the territory of Azerbaijan. He compiled a map of the Caspian Sea in the second century, has given a clear overview on the geographical names, objects and settlements located on its shores. The names of many cities and villages belonging to Albania, as well as the name “Astara” (Greek: Astarata) are found on this map. Another scholar of the ancient world, Strabon also pointed out the name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Gilan Province
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Ardabil Province
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Iran
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Azerbaijan
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alborz (mountain Range)
The Alborz ( fa, البرز) range, also spelled as Alburz, Elburz or Elborz, is a mountain range in northern Iran that stretches from the border of Azerbaijan along the western and entire southern coast of the Caspian Sea and finally runs northeast and merges into the smaller Aladagh Mountains and borders in the northeast on the parallel mountain ridge Kopet Dag in the northern parts of Khorasan. All these mountains are part of the much larger Alpide belt. This mountain range is divided into the Western, Central, and Eastern Alborz Mountains. The Western Alborz Range (usually called the Talysh) runs south-southeastward almost along the western coast of the Caspian Sea. The Central Alborz (the Alborz Mountains in the strictest sense) runs from west to east along the entire southern coast of the Caspian Sea, while the Eastern Alborz Range runs in a northeasterly direction, toward the northern parts of the Khorasan region, southeast of the Caspian Sea. Mount Damavand, the highest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caspian Tiger
The Caspian tiger was a ''Panthera tigris tigris'' population native to eastern Turkey, northern Iran, Mesopotamia, the Caucasus around the Caspian Sea, Central Asia to northern Afghanistan, and the Xinjiang region in western China. Until the Middle Ages, it was also present in Ukraine and southern Russia. It inhabited sparse forests and riverine corridors in this region until the 1970s. This population was regarded as a distinct subspecies and assessed as extinct in 2003. Results of a phylogeographic analysis evinces that the Caspian and Siberian tiger populations shared a common continuous geographic distribution until the early 19th century. Some Caspian tigers were intermediate in size between Siberian and Bengal tigers. It was also called Balkhash tiger, Hyrcanian tiger, Turanian tiger, and Mazandaran tiger ( fa, ). Taxonomy ''Felis virgata'' was a scientific name used by Johann Karl Wilhelm Illiger in 1815 for the greyish tiger in the area surrounding the Caspian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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