Baghlan is one of the thirty-four provinces of Afghanistan. It is in the north of the country; as of 2013, the province has a population of about 910,700. Its capital is Puli Khumri; the ruins of a Zoroastrian fire temple, the Surkh Kotal, are located in Baghlan. The lead nation of the local Provincial Reconstruction Team was Hungary, which operated from 2006 to 2015; the name Baghlan is derived from Bagolango or "image-temple", inscribed on the temple of Surkh Kotal during the reign of the Kushan emperor, Kanishka in the early 2nd century CE. The Chinese Buddhist monk Xuanzang traveled through Baghlan in the mid-7th Century CE, referred to it as the "kingdom of Fo-kia-lang". In the 13th Century CE, a permanent garrison of Mongol troops was quartered in the Kunduz-Baghlan area, in 1253 fell under the jurisdiction of Sali Noyan Tatar, appointed there by Möngke Khan. Sali Noyan's position was inherited by his son Uladu, grandson Baktut; these Turco-Mongol garrison troops formed the Qara'unas faction, by the 14th Century had allied with the Chaghataite Khanate.
Under the rule of Temür the Qara'unas were given to Chekü Barlas, to his son Jahānshāh. Forbes Manz notes that these Kunduz-Baghlan forces appear to have remained cohesive and influential throughout the Timurid period, though under different leaders and different names, up until the Uzbek invasion. By the Islamic year 900, the area was noted in the Baburnama. In the mid-20th Century, as Afghanistan became the target of international development from both the Western and Soviet world, agricultural-industrial projects were initiated in Baghlan; these included factories for the production of sugar for vegetable oil. Czech expertise figured into the development of Baghlans' coal-mining industry, centred at Baghlan's Karkar Valley, the only coal mine in Afghanistan to remain operational up through 1992; the modern Baghlan Province was created out of the former Qataghan Province in 1964. During the Soviet–Afghan War, the Soviets in 1982 established the Kayan military zone in southern Baghlan; the area was defended by 10,000 Ismaili militiamen, increasing to 18,000 by 1992, who sided with the Soviets due to differences with the Islamist opposition.
Afghan Ismailis overall were inclined to support the Communists, though a local Ismaili leader, Sayed Manuchehr, lead a partisan movement against the Communists until Ismaili leader Sayed Mansur Naderi accepted Soviet support. Large portions of Baghlan and neighbouring Samangan Province were under the sway of the Soviet-aligned Naderi clan, the hereditary Ismaili Sayeds of Kayan. Under their jurisdiction, was quiet and societally functional throughout the 1980s, with hospitals and administrative services, funded by the communist central government. Despite the Naderi's alliance with the Communists, they maintained positive relations with the Mujahideen as well, permitting them to move through the area provided they refrained from attacks. One of the Soviets' three primary bases in Afghanistan, was located in Baghlan Province, served as the "largest military supply and armoury centre of the Soviet troops in Afghanistan." As the 2001 Afghan War commenced, Ismaili leader Sayed Mansoor Naderi attempted to retake Baghlan from the Taliban.
Naderi was aligned with Uzbek warlord Abdul Rashid Dostum and his Jumbesh-e Milli party, the competing Tajik-dominated Jamiat-e Islami party was keen to seize control of Baghlan as Taliban power eroded. The Jamiat were able to seize the capital of Pul-i Khumri before Naderi, who despite his strong backing among the Afghan Ismailis and Shia Hazaras, was unable to rally enough supporters to control the province. Naderi failed to retake the capital in 2001 and 2003, in the latter event he negotiated a power-sharing agreement with the dominant Andarabi militias and made the Ismaili bastion of the Kayan Valley his base. On 13 June 2012, two earthquakes hit Afghanistan and there was a major landslide in Burka District of Baghlan Province; the village of Sayi Hazara was buried under up to 30 meters of rock. The town of Puli Khumri serves as the capital of the province. All law enforcement activities throughout the province are handled by the Afghan National Police; the provincial police chief represents the Ministry of the Interior in Kabul.
The ANP is backed including the NATO-led forces. Abdul Sattar Bariz has been the governor of the province since October 2015; the population of Baghlan province was reported at 863,700 in the year 2013. Tajiks make up 50% of the population, followed by 20% Pashtuns, 5% Turkmens, 20% Hazaras, 5% Uzbeks, others. Most of the population speak Persian, followed by Pashto-speaking Pashtuns and some Tatars. Baghlan is home to a small community of Ismaili Muslims led by the Sayeds of Kayan; the percentage of households with clean drinking water increased from 19% in 2005 to 25% in 2011. The percentage of births attended to by a skilled birth attendant increased from 5.5% in 2005 to 22% in 2011. The overall literacy rate increased from 21% in 2005 to 24% in 2011; the overall net enrolment rate increased from 29% in 2005 to 62% in 2011. Baghlan's primary crops were cotton and sugar beets, industrial sugar production having begun under Czech supervision in the 1940s; the area produced grapes and pomegranates.
The primary livestock is Karakul sheep. The province produces silk, coal is mined in the Karkar Valley. Baghlan 2007 Baghlan sugar factory bom
An earthquake is the shaking of the surface of the Earth, resulting from the sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in size from those that are so weak that they cannot be felt to those violent enough to toss people around and destroy whole cities; the seismicity, or seismic activity, of an area is the frequency and size of earthquakes experienced over a period of time. The word tremor is used for non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground; when the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes can trigger landslides, volcanic activity. In its most general sense, the word earthquake is used to describe any seismic event—whether natural or caused by humans—that generates seismic waves. Earthquakes are caused by rupture of geological faults, but by other events such as volcanic activity, mine blasts, nuclear tests.
An earthquake's point of initial rupture is called its hypocenter. The epicenter is the point at ground level directly above the hypocenter. Tectonic earthquakes occur anywhere in the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane; the sides of a fault move past each other smoothly and aseismically only if there are no irregularities or asperities along the fault surface that increase the frictional resistance. Most fault surfaces do have such asperities and this leads to a form of stick-slip behavior. Once the fault has locked, continued relative motion between the plates leads to increasing stress and therefore, stored strain energy in the volume around the fault surface; this continues until the stress has risen sufficiently to break through the asperity allowing sliding over the locked portion of the fault, releasing the stored energy. This energy is released as a combination of radiated elastic strain seismic waves, frictional heating of the fault surface, cracking of the rock, thus causing an earthquake.
This process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the elastic-rebound theory. It is estimated that only 10 percent or less of an earthquake's total energy is radiated as seismic energy. Most of the earthquake's energy is used to power the earthquake fracture growth or is converted into heat generated by friction. Therefore, earthquakes lower the Earth's available elastic potential energy and raise its temperature, though these changes are negligible compared to the conductive and convective flow of heat out from the Earth's deep interior. There are three main types of fault, all of which may cause an interplate earthquake: normal and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas.
Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip. Reverse faults those along convergent plate boundaries are associated with the most powerful earthquakes, megathrust earthquakes, including all of those of magnitude 8 or more. Strike-slip faults continental transforms, can produce major earthquakes up to about magnitude 8. Earthquakes associated with normal faults are less than magnitude 7. For every unit increase in magnitude, there is a thirtyfold increase in the energy released. For instance, an earthquake of magnitude 6.0 releases 30 times more energy than a 5.0 magnitude earthquake and a 7.0 magnitude earthquake releases 900 times more energy than a 5.0 magnitude of earthquake. An 8.6 magnitude earthquake releases the same amount of energy as 10,000 atomic bombs like those used in World War II. This is so because the energy released in an earthquake, thus its magnitude, is proportional to the area of the fault that ruptures and the stress drop.
Therefore, the longer the length and the wider the width of the faulted area, the larger the resulting magnitude. The topmost, brittle part of the Earth's crust, the cool slabs of the tectonic plates that are descending down into the hot mantle, are the only parts of our planet which can store elastic energy and release it in fault ruptures. Rocks hotter than about 300 °C flow in response to stress; the maximum observed lengths of ruptures and mapped faults are 1,000 km. Examples are the earthquakes in Chile, 1960; the longest earthquake ruptures on strike-slip faults, like the San Andreas Fault, the North Anatolian Fault in Turkey and the Denali Fault in Alaska, are about half to one third as long as the lengths along subducting plate margins, those along normal faults are shorter. The most important parameter controlling the maximum earthquake magnitude on a fault is however not the maximum available length, but the available width because the latter varies by a factor of 20. Along converging plate margins, the dip angle of the rupture plane is shallow about 10 de
Badakhshan Province is one of the 34 provinces of Afghanistan, located in the farthest northeastern part of the country between Tajikistan and northern Pakistan. It shares a 56.5-mile border with China. It is part of a broader historical Badakhshan region; the province contains 22 to 28 districts, over 1,200 villages, 904,700 people. Feyzabad serves as the provincial capital. Badakhshan is bordered by Gorno-Badakhshan Autonomous Province and Khatlon Province in Tajikistan to the north and east. In the east of the province a long spur called the Wakhan Corridor extends above northern Pakistan's Chitral and Northern Areas to a border with China; the province has a total area of 44,059 square kilometres, most of, occupied by the Hindu Kush and Pamir mountain ranges. Badakhshan was a stopover on the ancient Silk Road trading path, China has shown great interest in the province after the fall of the Taliban, helping to reconstruct roads and infrastructure. According to the World Wildlife Fund, Badakhshan contains temperate grasslands and shrublands, as well as Gissaro-Alai open woodlands along the Pamir River.
Common plants found in these areas include pistachio, walnut, apple and sagebrush. Montane grasslands and shrublands are existent in the province, with the Hindu Kush alpine meadow in the high mountains in the northern and southwestern regions; the Wakhan corridor contains two montane grassland and shrubland regions: the Karakoram-West Tibetan Plateau alpine steppe and in the Pamir Mountains and Kuh-e Safed Khers in Darwaz region. South of Fayzabad the terrain becomes dominated by xeric shrublands. Common vegetation includes thorny bushes, zizyphus and Amygdatus. Paropamisus xeric woodlands can be found in central areas. Common vegetation includes almond, pistachio and sea-buckthorn; the area has a long history like the rest of Afghanistan, dating to its conquering by the Achaemenid Empire and beyond. Badakhshan etymologically derives from an official title; the suffix of the name, -ān, means the region belonged to someone with the title badaxš. The territory was ruled by the Uzbek Khanate of Bukhara between the early 16th century and the mid-18th century.
It was given to Ahmad Shah Durrani by Murad Beg of Bukhara after a treaty of friendship was reached in or about 1750 and became part of the Durrani Empire. It was ruled by the Durranis followed by the Barakzai dynasty, was untouched by the British during the three Anglo-Afghan wars that were fought in the 19th and 20th centuries, it remained peaceful for about 100 years until the 1980s Soviet–Afghan War at which point the Mujahideen began a rebellion against the central Afghan government. During the 1990s, much of the area was controlled by forces loyal to Burhanuddin Rabbani and Ahmad Shah Massoud, who were de facto the national government until 1996. Badakhshan was the only province that the Taliban did not conquer during their rule from 1996 to 2001. However, during the course of the wars a non-Taliban Islamic emirate was established in Badakhshan by Mawlawi Shariqi, paralleling the Islamic Revolutionary State of Afghanistan in neighboring Nuristan. Rabbani, a Badakhshan native, Massoud, were the last remnants of the anti-Taliban Northern Alliance during the peak of Taliban control in 2001.
Badakhshan was thus one of the few provinces of the country that witnessed little insurgency in the Afghan wars - however during the 2010s Taliban insurgents managed to attack and take control of several districts in the province. On 26 October 2015, the 7.5 Mw Hindu Kush earthquake shook northern Afghanistan with a maximum Mercalli intensity of VIII. This earthquake destroyed 30,000 homes, left several hundred dead, more than 1,700 injured; the current Governor of the province is Shah Waliullah Adeeb. His predecessors were Baz Mohammad Ahmadi; the borders with neighboring Tajikistan and Pakistan are monitored by the Afghan Border Police. All law enforcement activities throughout the province are handled by the Afghan National Police. A provincial Police Chief is assigned to lead both the ANP and the ABP; the Police Chief represents the Ministry of the Interior in Kabul. The ANP is backed by the military, including the NATO-led forces. Fayzabad, the capital of Badakhshan province, sits on the Kokcha River and has an approximate population of 50,000.
The chief commercial and administrative center of northeast Afghanistan and the Pamir region, Fayzabad has rice and flour mills. Fayzabad Airport serves the province with regular direct flights to Kabul; the percentage of households with clean drinking water increased from 13% in 2005 to 21% in 2011. The percentage of births attended to by a skilled birth attendant increased from 1.5% in 2003 to 2% in 2011. The overall literacy rate fell from 31% in 2005 to 26% in 2011; the overall net enrolment rate increased from 46% in 2005 to 68% in 2011. Despite massive mineral reserves, Badakhshan is one of the most destitute areas in the world. Opium poppy growing is the only real source of income in the province and Badakhshan has one of the highest rates of maternal mortality in the world, due to the complete lack of health infrastructure, inaccessible locations, bitter winters of the province. BORNA Institute of Higher Education being the first private university located on the bank of Kokcha river. Lapis lazuli has been mined in the Sar-e-Sang mines, located in the Kuran wa Munjan District of Badakhshan, for over 6,000 years.
The mines were the largest and most well-known source in ancient times. Most recent
Dushi district is located in the central part of Baghlan Province, Afghanistan. It lies on the major Kabul-Kunduz highway; the population of the district was estimated to be around 57,160 in 2004. Hazaras are around 88% of the population and make up the majority in the district, followed by small minorities of Tajiks and Pashtuns The centre of the district is Dushi. Dushi is home to an overhead power line carrying imported electricity from Turkmenistan and Uzbekistan; the 300 MegaWatt supply was the subject of a grant for expansion in 2013 from the Asian Development Bank. The line supplies the capital, Kabul. On April 13, 2018, Taliban insurgents used explosives to destroy a pylon, disrupting power supplies to the region. Districts of Afghanistan Map of Settlements United Nations, AIMS, May 2002
Afghanistan the Islamic Republic of Afghanistan, is a landlocked country located in South-Central Asia. Afghanistan is bordered by Pakistan in the south and east, its territory covers 652,000 square kilometers and much of it is covered by the Hindu Kush mountain range, which experiences cold winters. The north consists of fertile plains, while the south-west consists of deserts where temperatures can get hot in summers. Kabul serves as its largest city. Human habitation in Afghanistan dates back to the Middle Paleolithic Era, the country's strategic location along the Silk Road connected it to the cultures of the Middle East and other parts of Asia; the land has been home to various peoples and has witnessed numerous military campaigns, including those by Alexander the Great, Muslim Arabs, British and since 2001 by the United States with NATO-allied countries. It has been called "unconquerable" and nicknamed the "graveyard of empires"; the land served as the source from which the Kushans, Samanids, Ghaznavids, Khaljis, Hotaks and others have risen to form major empires.
The political history of the modern state of Afghanistan began with the Hotak and Durrani dynasties in the 18th century. In the late 19th century, Afghanistan became a buffer state in the "Great Game" between British India and the Russian Empire, its border with British India, the Durand Line, was formed in 1893 but it is not recognized by the Afghan government and it has led to strained relations with Pakistan since the latter's independence in 1947. Following the Third Anglo-Afghan War in 1919 the country was free of foreign influence becoming a monarchy under King Amanullah, until 50 years when Zahir Shah was overthrown and a republic was established. In 1978, after a second coup Afghanistan first became a socialist state and a Soviet Union protectorate; this evoked the Soviet–Afghan War in the 1980s against mujahideen rebels. By 1996 most of Afghanistan was captured by the Islamic fundamentalist group the Taliban, who ruled most of the country as a totalitarian regime for over five years.
The Taliban were forcibly removed by the NATO-led coalition, a new democratically-elected government political structure was formed, but they still control a significant portion of the country. Afghanistan is a unitary presidential Islamic republic with a population of 31 million composed of ethnic Pashtuns, Tajiks and Uzbeks, it is a member of the United Nations, the Organisation of Islamic Cooperation, the Group of 77, the Economic Cooperation Organization, the Non-Aligned Movement. Afghanistan's economy is the world's 108th largest, with a GDP of $64.08 billion. The name Afghānistān is believed to be as old as the ethnonym Afghan, documented in the 10th-century geography book Hudud ul-'alam; the root name "Afghan" was used in reference to a member of the ethnic Pashtuns, the suffix "-stan" means "place of" in Persian. Therefore, Afghanistan translates to land of the Afghans or, more in a historical sense, to land of the Pashtuns. However, the modern Constitution of Afghanistan states that "he word Afghan shall apply to every citizen of Afghanistan."
Excavations of prehistoric sites by Louis Dupree and others suggest that humans were living in what is now Afghanistan at least 50,000 years ago, that farming communities in the area were among the earliest in the world. An important site of early historical activities, many believe that Afghanistan compares to Egypt in terms of the historical value of its archaeological sites; the country sits at a unique nexus point where numerous civilizations have interacted and fought. It has been home to various peoples through the ages, among them the ancient Iranian peoples who established the dominant role of Indo-Iranian languages in the region. At multiple points, the land has been incorporated within large regional empires, among them the Achaemenid Empire, the Macedonian Empire, the Indian Maurya Empire, the Islamic Empire. Many empires and kingdoms have risen to power in Afghanistan, such as the Greco-Bactrians, Hephthalites, Kabul Shahis, Samanids, Ghurids, Kartids, Timurids and the Hotak and Durrani dynasties that marked the political origins of the modern state.
Archaeological exploration done in the 20th century suggests that the geographical area of Afghanistan has been connected by culture and trade with its neighbors to the east and north. Artifacts typical of the Paleolithic, Neolithic and Iron ages have been found in Afghanistan. Urban civilization is believed to have begun as early as 3000 BCE, the early city of Mundigak may have been a colony of the nearby Indus Valley Civilization. More recent findings established that the Indus Valley Civilisation stretched up towards modern-day Afghanistan, making the ancient civilisation today part of Pakistan and India. In more detail, it extended from what today is northwest Pakistan to northwest India and northeast Afghanistan. An Indus Valley site has been found on the Oxus River at Shortugai in northern Afghanistan. There are several smaller IVC colonies to be found in Afghanistan as well. After 2000 BCE, successive waves of semi-nomadic
A drought or drouth is a natural disaster of below-average precipitation in a given region, resulting in prolonged shortages in the water supply, whether atmospheric, surface water or ground water. A drought may be declared after as few as 15 days, it can have a substantial impact on the ecosystem and agriculture of the affected region and harm to the local economy. Annual dry seasons in the tropics increase the chances of a drought developing and subsequent bush fires. Periods of heat can worsen drought conditions by hastening evaporation of water vapour. Many plant species, such as those in the family Cactaceae, have drought tolerance adaptations like reduced leaf area and waxy cuticles to enhance their ability to tolerate drought; some others survive dry periods as buried seeds. Semi-permanent drought produces arid biomes such as grasslands. Prolonged droughts have caused humanitarian crisis. Most arid ecosystems have inherently low productivity; the most prolonged drought in the world in recorded history occurred in the Atacama Desert in Chile.
Mechanisms of producing precipitation include convective and orographic rainfall. Convective processes involve strong vertical motions that can cause the overturning of the atmosphere in that location within an hour and cause heavy precipitation, while stratiform processes involve weaker upward motions and less intense precipitation over a longer duration. Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice. Droughts occur in areas where normal levels of rainfall are, in themselves, low. If these factors do not support precipitation volumes sufficiently to reach the surface over a sufficient time, the result is a drought. Drought can be triggered by a high level of reflected sunlight and above average prevalence of high pressure systems, winds carrying continental, rather than oceanic air masses, ridges of high pressure areas aloft can prevent or restrict the developing of thunderstorm activity or rainfall over one certain region.
Once a region is within drought, feedback mechanisms such as local arid air, hot conditions which can promote warm core ridging, minimal evapotranspiration can worsen drought conditions. Within the tropics, distinct and dry seasons emerge due to the movement of the Intertropical Convergence Zone or Monsoon trough; the dry season increases drought occurrence, is characterized by its low humidity, with watering holes and rivers drying up. Because of the lack of these watering holes, many grazing animals are forced to migrate due to the lack of water in search of more fertile lands. Examples of such animals are zebras and wildebeest; because of the lack of water in the plants, bushfires are common. Since water vapor becomes more energetic with increasing temperature, more water vapor is required to increase relative humidity values to 100% at higher temperatures. Periods of warmth quicken the pace of fruit and vegetable production, increase evaporation and transpiration from plants, worsen drought conditions.
Drier and hotter weather occurs in parts of the Amazon River Basin and Central America during El Niño events. Winters during the El Niño are warmer and drier than average conditions in the Northwest, northern Midwest, northern Mideast United States, so those regions experience reduced snowfalls. Conditions are drier than normal from December to February in south-central Africa in Zambia, Zimbabwe and Botswana. Direct effects of El Niño resulting in drier conditions occur in parts of Southeast Asia and Northern Australia, increasing bush fires, worsening haze, decreasing air quality dramatically. Drier-than-normal conditions are in general observed in Queensland, inland Victoria, inland New South Wales, eastern Tasmania from June to August; as warm water spreads from the west Pacific and the Indian Ocean to the east Pacific, it causes extensive drought in the western Pacific. Singapore experienced the driest February in 2014 since records began in 1869, with only 6.3 mm of rain falling in the month and temperatures hitting as high as 35 °C on 26 February.
The years 2005 had the next driest Februaries, when 8.4 mm of rain fell. Human activity can directly trigger exacerbating factors such as over farming, excessive irrigation and erosion adversely impact the ability of the land to capture and hold water. In arid climates, the main source of erosion is wind. Erosion can be the result of material movement by the wind; the wind can cause small particles to be therefore moved to another region. Suspended particles within the wind may impact on solid objects causing erosion by abrasion. Wind erosion occurs in areas with little or no vegetation in areas where there is insufficient rainfall to support vegetation. Loess is a homogeneous nonstratified, friable coherent calcareous, fine-grained, pale yellow or buff, windblown sediment, it occurs as a widespread blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick. Loess stands in either steep or vertical faces. Loess tends to develop into rich soils. Under appropriate climatic conditions, areas with loess are among the most agriculturally productive in the world.
Loess deposits are geologically unstable by nature, will erode readily. Therefore, windbreaks are planted by farmers to reduce the wind erosion of loess. Wind erosion
Puli Khumrī spelled Pul-i-Khumri or Pol-e Khomri, is a city in northern Afghanistan. It is the capital of Baghlan Province and as of 2002 had a population of 60,000; the spoken language is Persian and the vast majority in this city are Tajiks and Pashtun. The city of Puli Khumri has a population of 221,274, it has a total land area of 3,752 Hectares. The total number of dwellings in this city are 24,586. With an influence from the local steppe climate, Puli Khumri features a cold semi-arid climate under the Köppen climate classification; the average temperature in Puli Khumri is 15.9 °C. July is the hottest month of the year with an average temperature of 28.5 °C. The coldest month January has an average temperature of 3.0 °C. Puli Khumri is a transit hub in northeastern Afghanistan. Agricultural lands account for the largest land use, with the majority of that land in Districts 3, 5 and 6. Districts 1 and 2 have the highest dwelling densities but District 5 is home to the most dwelling units. Puli Khumri has a diverse housing stock consisting of regular and hillside houses as well as apartment buildings.
There are two dams in Puli Khumri. Afghanistan's first cement factory was built in 1954 in Puli Khumri with financial support from Czechoslovakia, it is owned and operated by Afghan Invest Co. and operated by Ahmad Javid Jaihoon. The limestone is mined from the hill behind the factory. There is a coal mine outside of the city in the village Kan-kan, but the production system is archaic. Agriculture is important because of the rain and temperature. Hungary headed a Provincial Reconstruction Team in the city until March 2013. Electrical transmission lines built from Puli Khumri are now bringing a steady supply of electricity to Kabul. Baghlan Province