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Tehran Plain
The Tehran Plain is a landscape formation in Iran delimited by the adjacent Alborz Mountain range. It is a site of prehistoric archaeological and geoscientific interest. Numerous faults and deformed quaternary units in the Tehran plain prove it is a region of ancient tectonic activity. Geology The Tehran Plain is a landscape formation in Iran. It consists of Neogene and Quaternary sediments.Angela Landgraf, Lucilla Benedetti, Regis Braucher, Didier Bourles et alPleistocene deformation and landscape evolution in the Tehran plain: results from tectonic geomorphology and TCN-dating.Geophysical Research Abstracts, Vol. 12, EGU2010-11196, 2010 EGU General Assembly, 2010 The North Tehran Fault thrust up Eocene rocks of the Alborz Mountain range. Geomorphologically three different zones can be described: In the western part, the plain has been deformed by thrusting, as can be seen by a segmented and internally deformed anticline and old and diverted channels on both sides. This process ha ... [...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] |
Middle Pleistocene
The Chibanian, widely known by its previous designation of Middle Pleistocene, is an Age (geology), age in the international geologic timescale or a Stage (stratigraphy), stage in chronostratigraphy, being a division of the Pleistocene Epoch within the ongoing Quaternary Period. The Chibanian name was officially ratified in January 2020. It is currently estimated to span the time between 0.770 annum, Ma (770,000 years ago) and 0.126 Ma (126,000 years ago), also expressed as 770–126 ka. It includes the transition in palaeoanthropology from the Lower Palaeolithic, Lower to the Middle Palaeolithic over 300 ka. The Chibanian is preceded by the Calabrian (stage), Calabrian and succeeded by the proposed Tarantian. The beginning of the Chibanian is the Brunhes–Matuyama reversal, when the Earth's magnetic field last underwent reversal. It ends with the onset of the Eemian interglacial period (Marine Isotope Stage 5). The term Middle Pleistocene was in use as a provisional or "quasi-fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Tehran 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] |
White Revolution
The White Revolution ( fa, انقلاب سفید ''Enqelāb-e Sefid'') or the Shah and People Revolution ( fa, انقلاب شاه و مردم ''Enqelāb-e Shāh o Mardom'') was a far-reaching series of reforms resulting in aggressive modernization in Iran launched on 26 January 1963 by the Shah, Mohammad Reza Pahlavi, which lasted until 1979. The reforms resulted in a great redistribution of wealth to Iran's working class, explosive economic growth in subsequent decades, rapid urbanization, and deconstruction of Iran's feudalist customs. The reforms were characterized by high economic growth rates, major investments in infrastructure, substantial growth in per capita wealth and literacy of Iranians. The economic growth and education advancement arguably paved the way for the Shah's military arms build-up and the establishment of Iran as a major geopolitical power in the Middle East. It consisted of several elements, including land reform, sale of some state-owned factories t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qasemabad, Pishva
Qasemabad ( fa, قاسم اباد, also Romanized as Qāsemābād and Qāsimābād) is a village in Asgariyeh Rural District, in the Central District of Pishva County Pishva County ( fa, شهرستان پیشوا) is in Tehran province, Iran. The capital of the county is the city of Pishva. At the 2006 census, the region's population (as Pishva District of Varamin County Varamin County ( fa, شهرس ..., Tehran Province, Iran. At the 2006 census, its population was 818, in 170 families. References Populated places in Pishva County {{Pishva-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blade (archaeology)
In archaeology, a blade is a type of stone tool created by striking a long narrow flake from a stone core. This process of reducing the stone and producing the blades is called lithic reduction. Archaeologists use this process of flintknapping to analyze blades and observe their technological uses for historical purposes. Blades are defined as being flakes that are at least twice as long as they are wide and that have parallel or subparallel sides and at least two ridges on the dorsal (outer) side. Blade cores appear and are different from regular flaking cores, as each core's conchoidal nature is suited for different types of flaking. Blades are created using stones that have a cryptocrystalline structure and easily be fractured into a smooth piece without fracturing. Blades became the favored technology of the Upper Palaeolithic era, although they are occasionally found in earlier periods. Different techniques are also required for blade creation; a soft punch or hammerstone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalcolithic
The Copper Age, also called the Chalcolithic (; from grc-gre, χαλκός ''khalkós'', " copper" and ''líthos'', " stone") or (A)eneolithic (from Latin ''aeneus'' "of copper"), is an archaeological period characterized by regular human manipulation of copper, but prior to the discovery of bronze alloys. Modern researchers consider the period as a subset of the broader Neolithic, but earlier scholars defined it as a transitional period between the Neolithic and the Bronze Age. The archaeological site of Belovode, on Rudnik mountain in Serbia, has the world's oldest securely dated evidence of copper smelting at high temperature, from (7000 BP). The transition from Copper Age to Bronze Age in Europe occurred between the late 5th and the late In the Ancient Near East the Copper Age covered about the same period, beginning in the late and lasting for about a millennium before it gave rise to the Early Bronze Age. Terminology The multiple names resu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stone Tool
A stone tool is, in the most general sense, any tool made either partially or entirely out of stone. Although stone tool-dependent societies and cultures still exist today, most stone tools are associated with prehistoric (particularly Stone Age) cultures that have become extinct. Archaeology, Archaeologists often study such prehistoric societies, and refer to the study of stone tools as lithic analysis. Ethnoarchaeology has been a valuable research field in order to further the understanding and cultural implications of stone tool use and manufacture. Stone has been used to make a wide variety of different tools throughout history, including arrowheads, spearheads, hand axes, and Quern-stone, querns. Stone tools may be made of either ground stone or Lithic reduction, knapped stone, the latter fashioned by a flintknapper. Knapped stone tools are made from cryptocrystalline materials such as chert or flint, radiolarite, chalcedony, obsidian, basalt, and quartzite via a process ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Choga Mami
Choga Mami is a Samarran settlement site in Diyala province in Eastern Iraq in the Mandali region. It shows the first canal irrigation in operation at about 6000 BCE. The site, about 70 miles northeast of Baghdad, has been dated to the late 6th millennium BCE. It was occupied in several phases from the Samarran culture through the Ubaid. Buildings were rectangular and built of mud brick, including a guard tower at the settlement's entrance. Irrigation supported livestock (cattle, sheep and goats) and arable (wheat, barley and flax) agriculture. One important aspect of the site therefore is the evidence that it yields for chronological relationships between North and South Mesopotamian cultures, at least in the area of Mandali, and for connections with Iran. The introduction of irrigation, new types of grain, foreign ceramic styles and domestic cattle are all located in the Choga Mami phase, a late manifestation of the Samarran Period in lowland Mesopotamia. This chronological ide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tepe Pardis
Tepe may refer to: *the Persian word for ' tell', a type of earthen mound *''tepe'', a common element in Persian-language toponyms; see *Tepe, Bismil, a village in Turkey *Tepe, Dicle, a village in Turkey *Tepe, Iran, a village in Markazi Province, Iran *Tepe, Slovenia, a settlement in the Litija Municipality in Slovenia *Tépe Tépe is a village in Hajdú-Bihar county, in the Northern Great Plain region of eastern Hungary. Geography It covers an area of and has a population Population typically refers to the number of people in a single area, whether it be ..., a village and municipality in Hungary * Göbekli Tepe, an archaeological site in Turkey *A type of interdental brush See also * Tappeh (other), places in Iran {{dab, geodis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Neolithic
In the archaeology of Southwest Asia, the Late Neolithic, also known as the Ceramic Neolithic or Pottery Neolithic, is the final part of the Neolithic period, following on from the Pre-Pottery Neolithic and preceding the Chalcolithic. It is sometimes further divided into Pottery Neolithic A (PNA) and Pottery Neolithic B (PNB) phases. The Late Neolithic began with the first experiments with pottery, around 7000 BCE, and lasted until the discovery of copper metallurgy and the start of the Chalcolithic around 4500 BCE. Southern Levant The Neolithic of the Southern Levant is divided into Pre-Pottery and Pottery or Late Neolithic phases, initially based on the sequence established by Kathleen Kenyon at Jericho. In the Mediterranean zone, the Pottery Neolithic is further subdivided into two subphases and several regional cultures, although the extent to which these represent real cultural phenomena is debated: * Pottery Neolithic A (PNA) or Late Neolithic 1 (LN1) ** Ya ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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