Wari-Bateshwar Ruins
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Wari-Bateshwar Ruins
The Wari-Bateshwar (Bengali: উয়ারী-বটেশ্বর,''Uari-Bôṭeshshor'') ruins in Narsingdi, Dhaka Division, Bangladesh is one of the earliest urban archaeological sites in Bangladesh. Excavation in the site unearthed a fortified urban center, paved roads and suburban dwelling. The site was primarily occupied during the iron age, from 400 to 100 BCE, as evidenced by the abundance of punch-marked coins and Northern Black Polished Ware (NBPW) artifacts. The site also reveals signs of pit dwelling, a feature typically found in chalcolithic archaeological sites in the Indian sub-continent. Geography The site sprawls across Wari and Bateshwar, two adjacent villages in the Belabo Upazila of Narsingdi district, about 17 km North-west of the confluence of the rivers Old Brahmaputra and Meghna at the lower end of Sylhet basin. Borehole records show that the site lies on the remnants of a Pleistocene fluvial terrace about 15 metre above sea level and 6-8 metre a ...
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Narsingdi District
Narsingdi District ( bn, নরসিংদী জেলা) is a district in central Bangladesh. It is located 50 km north-east of Dhaka, capital (political), capital city of Bangladesh. It is a part of the Dhaka Division. The district is famous for its textile craft industry. Narsingdi is bordered by Kishoreganj District, Kishoreganj in the north and north-east, Brahmanbaria District, Brahmanbaria in the east and south-east, Narayanganj District, Narayanganj in the south and south-west and Gazipur District, Gazipur in the west. Subdivisions There are six upazilas, or subdivisions, in the Narsingdi district. * Belabo Upazila * Monohardi Upazila * Narsingdi Sadar Upazila * Palash Upazila * Raipura Upazila * Shibpur Upazila Demographics According to the 2011 Bangladesh census, Narsingdi district had a population was 2,224,944, of which 1,102,943 were males and 1,122,001 females. Rural population was 1,777,299 (79.88%) while the urban population was 447,645 (20.12%). Narsin ...
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Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ...
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Black And Red Ware
Black and red ware (BRW) is a South Asian earthenware, associated with the neolithic phase, Harappa, Bronze Age India, Iron Age India, the megalithic and the early historical period. Although it is sometimes called an archaeological culture, the spread in space and time and the differences in style and make are such that the ware must have been made by several cultures. In the Western Ganges plain (western Uttar Pradesh) it is dated to c. 1450–1200 BCE, and is succeeded by the Painted Grey Ware culture; whereas in the Central and Eastern Ganges plain (eastern Uttar Pradesh, Bihar, and Bengal) and Central India (Madhya Pradesh) the BRW appears during the same period but continues for longer, until c. 700–500 BCE, when it is succeeded by the Northern Black Polished Ware culture. In the Western Ganges plain, the BRW was preceded by the Ochre Coloured Pottery culture. The BRW sites were characterized by subsistence agriculture (cultivation of rice, barley, and legumes), and yiel ...
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Inamgaon
Inamgaon, in Maharashtra, is one of the largest Chalcolithic settlements in India. It has been estimated that at one time, about 1,000 people may have lived here. The settlement lasted for over 900 years (1500-600 BCE). Inamgaon is a post- Harappan agrarian village and archaeological site located in Maharashtra, western India. Situated along the right bank of the Ghod River, it is considered to be the 'regional centre' of the Bhima Valley. Inamgaon is one of the most intensively and extensively excavated and well reconstructed Chalcolithic sites of the Deccan plateau. By David Geography The village is located approximately to the east of the city of Pune. The region, situated within the lower reaches of the Ghod, is characterized by Cretaceous-Eocene Deccan Trap basalt. Archaeological site An ancient site, measuring approximately by , is located about north of Inamgaon. There are five mounds at the site. The largest mound is called 'Inamgaon I', and it has been extensivel ...
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Lime Mortar
Lime mortar or torching is composed of lime and an aggregate such as sand, mixed with water. The ancient Egyptians were the first to use lime mortars, which they used to plaster their temples. In addition, the Egyptians also incorporated various limes into their religious temples as well as their homes. Indian traditional structures built with lime mortar, which are more than 4,000 years old like Mohenjo-daro is still a heritage monument of Indus valley civilization in Pakistan. It is one of the oldest known types of mortar also used in ancient Rome and Greece, when it largely replaced the clay and gypsum mortars common to ancient Egyptian construction. With the introduction of Portland cement during the 19th century, the use of lime mortar in new constructions gradually declined. This was largely due to the ease of use of Portland cement, its quick setting, and high compressive strength. However, the soft and porous properties of lime mortar provide certain advantages when work ...
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Citadel
A citadel is the core fortified area of a town or city. It may be a castle, fortress, or fortified center. The term is a diminutive of "city", meaning "little city", because it is a smaller part of the city of which it is the defensive core. In a fortification with bastions, the citadel is the strongest part of the system, sometimes well inside the outer walls and bastions, but often forming part of the outer wall for the sake of economy. It is positioned to be the last line of defence, should the enemy breach the other components of the fortification system. The functions of the police and the army, as well as the army barracks were developed in the citadel. History 3300–1300 BC Some of the oldest known structures which have served as citadels were built by the Indus Valley civilisation, where citadels represented a centralised authority. Citadels in Indus Valley were almost 12 meters tall. The purpose of these structures, however, remains debated. Though the structures foun ...
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Archaeological Excavation
In archaeology, excavation is the exposure, processing and recording of archaeological remains. An excavation site or "dig" is the area being studied. These locations range from one to several areas at a time during a project and can be conducted over a few weeks to several years. Excavation involves the recovery of several types of data from a site. This data includes artifacts (portable objects made or modified by humans), features (non-portable modifications to the site itself such as post molds, burials, and hearths), ecofacts (evidence of human activity through organic remains such as animal bones, pollen, or charcoal), and archaeological context (relationships among the other types of data).Kelly&Thomas (2011). ''Archaeology: down to earth'' (4th ed.). Belmont, Calif.: Wadsworth, Cengage Learning. Before excavating, the presence or absence of archaeological remains can often be suggested by, non-intrusive remote sensing, such as ground-penetrating radar. Basic informat ...
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Jahangir Nagar University
Jahangirnagar University ( JU) is a publicly funded university located in Savar, Dhaka, Bangladesh. It is the only fully residential university in Bangladesh. It operated as a project until 1973, when the 'Jahangirnagar Muslim University Act' was amended as the 'Jahangirnagar University Act'. In 2019, the university had 17,212 students, 836 teachers, and 2,018 other employees. It has been ranked third several times in national public university rankings. JU is the fourth oldest generalized public university in Bangladesh. Also, it has fourth largest university campus in Bangladesh. History Jahangirnagar University was formally launched on 12 January 1971 under the Jahangirnagar Muslim University Ordinance, 1970 and this day is observed as ''University Day''. Initially, it was named ''Jahangirnagar Muslim University'', and the plan was to operate the university like Aligarh Muslim University. But after the independence of Bangladesh, its name changed to ''Jahangirnagar Univers ...
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Hanif Pathan
Muhammad Hanif Pathan (6 April 1901 - 1989) was a Bangladeshi folklorist and antiquarian. He is best known for publicizing the Wari-Bateshwar ruins, an ancient fort city and archaeological site of Bangladesh dating back to 450 BC. He is credited as the highest number of proverbs collector in Bangladesh. Early life Pathan was born on 6 April 1901 (23 Choitro 1307) ‍at the village of Deewanchar, Raipura of the then Bengal Presidency of British India (now Bangladesh) to his maternal house. His ancestral residence was in Bateshwar village of Belabo Upazila Belabo ( bn, বেলাবো) is an upazila of the Narsingdi District of Bangladesh, located in the Dhaka Division. Here the 2,500-year-old civilisation of Wari-Bateshwar has been discovered. It is believed that it was a port city with foreign .... He passed the Normal Examination (professional training institute for the teachers) from Dhaka Normal School in 1921. He then began his career as a school teacher and was involve ...
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1762 Arakan Earthquake
The 1762 Arakan earthquake occurred at about 17:00 local time on 2 April, with an epicentre somewhere on the coast from Chittagong (modern Bangladesh) to Arakan in modern Burma. It had an estimated magnitude of as high as 8.8 on the moment magnitude scale and a maximum estimated intensity of XI (''Extreme'') on the Mercalli intensity scale. It triggered a local tsunami in the Bay of Bengal and caused at least 200 deaths. The earthquake was associated with major areas of both uplift and subsidence. It is also associated with a change in course of the Brahmaputra River to from east of Dhaka (Old Brahmaputra River) to to the west via the Jamuna River. Tectonic setting The eastern part of Bangladesh and the southwestern part of Burma lie along the highly oblique convergent boundary between the Indian Plate and the Eurasian Plate. The degree to which this deformation is partitioned into zones of thrust tectonics (accommodating that part of the motion perpendicular to the boundary) and ...
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Peat
Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of , which is the average depth of the boreal orthernpeatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. ''Sphagnum'' moss, also called peat moss, is one of th ...
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Avulsion (river)
In sedimentary geology and fluvial geomorphology, avulsion is the rapid abandonment of a river channel and the formation of a new river channel. Avulsions occur as a result of channel slopes that are much less steep than the slope that the river could travel if it took a new course. Deltaic and net-depositional settings Avulsions are common in river deltas, where sediment deposits as the river enters the ocean and channel gradients are typically very small. This process is also known as delta switching. Deposition from the river results in the formation of an individual deltaic lobe that pushes out into the sea. An example of a deltaic lobe is the bird's-foot delta of the Mississippi River, pictured at right with its sediment plumes. As the deltaic lobe advances, the slope of the river channel becomes lower, as the river channel is longer but has the same change in elevation. As the slope of the river channel decreases, it becomes unstable for two reasons. First, water under the ...
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