Monday, May 2, 2016

eranir7

The Indian Independence Movement encompassed activities and ideas aiming to end the East India Company rule (1757–1858) and the British Raj (1858–1947) in the Indian subcontinent.
The very first organised militant movements were in Bengal, but they later took movement in the then newly formed Indian National Congress with prominent moderate leaders seeking only their basic right to appear for Indian Civil Service examinations, as well as more rights, economic in nature, for the people of the soil. The early part of the 20th century saw a more radical approach towards political self-rule proposed by leaders such as the Lal, Bal, Pal and Aurobindo Ghosh. The last stages of the self-rule struggle from the 1920s onwards saw Congress adopt Mohandas Karamchand Gandhi's policy of nonviolence and civil resistance,Muhammad Ali Jinnah's constitutional struggle for the rights of minorities in India, and several other campaigns. Activists Netaji Subhas Chandra Bose and Bhagat Singh preached armed revolution to achieve self-rule. Poets and writers such as Rabindranath TagoreSubramaniya BharathiAllama IqbalJosh Malihabadi,Mohammad Ali JouharBankim Chandra Chattopadhyay and Kazi Nazrul Islam used literature, poetry and speech as a tool for political awareness. Feminists such as Sarojini Naidu and Begum Rokeya promoted the emancipation of Indian women and their participation in national politics. Babasaheb Ambedkarchampioned the cause of the disadvantaged sections of Indian society within the larger self-rule movement. The period of the Second World War saw the peak of the campaigns by the Quit India movement led by Mahatma Gandhi and the Indian National Army movement led by Netaji Subhas Chandra Bose.
The Indian self-rule movement was a mass-based movement that encompassed various sections of society. It also underwent a process of constant ideological evolution.[1] Although the basic ideology of the movement was anti-colonial, it was supported by a vision of independent capitalist economic development coupled with a secular, democratic, republican, and civil-libertarian political structure.[2] After the 1930s, the movement took on a strong socialist orientation, due to the increasing influence of left-wing elements in the Congress as well as the rise and growth of the Communist Party of India.[1] The All-India Muslim League was formed in 1906 as a separate Muslim party which later in 1940 called for separate state of Pakistan. The work of these various movements led ultimately to the Indian Independence Act 1947, which ended the suzerainty in India and the creation of Pakistan. India remained a Dominion of the Crown until 26 January 1950, when the Constitution of India came into force, establishing the Republic of India; Pakistan was a dominion until 1956, when it adopted its first republican constitution. In 1971, East Pakistan declared independence as the People's Republic of Bangladesh.


eranir6

The National Museum of Natural History (NMNH) was a museum focusing on nature, located in New Delhi, India. Established in 1972 and opened in 1978, the museum functioned under the Ministry of Environment and Forests of the government of India.[1] The museum was situated on Barakhamba Road at Tansen Marg in central New Delhi,[2] across from the Embassy of Nepal, near the Connaught Place metro station.[3] On 26 April 2016, the museum building and its entire collection were destroyed by a fire.[4]



eranir5

landform is a natural feature of 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. Typical landforms include hillsmountainsplateauscanyonsvalleys, as well as shoreline features such as bayspeninsulas, and seas, including submerged features such as mid-ocean ridgesvolcanoes, and the great ocean basins.


eranir4

Mount Kusatsu-Shirane (草津白根山 Kusatsu Shirane-san?) is a 2160-meter active volcano in Kusatsu, GunmaJapan. It is called Kusatsu Shirane to differentiate it from the Mount Nikkō-Shirane on the other side of Gunma Prefecture. The summit of Kusatsu-Shirane volcano, located immediately north of Asama volcano, consists of a series of overlapping pyroclastic cones and three crater lakes. The largest of these is Yu-gama, an acidic turquoise-colored lake with rafts of yellow sulfur floating on its surface.



eranir3

complex volcano, also called a compound volcano, is mixed landform consisting of related volcanic centers and their associated lava flows and pyroclastic rock.[1] They may form due to changes in eruptive habit or in the location of the principal vent area on a particular volcano.[2] Stratovolcanoes can also form a large caldera that gets filled in by a lava dome, or else multiple small cinder coneslava domes and craters may develop on the caldera's rim.[2][3]
Although a comparatively unusual type of volcano, they are widespread in the world and in geologic history. Metamorphosed ash flow tuffs are widespread in the Precambrian rocks of northern New Mexico, which indicates that caldera complexes have been important for much of Earth's history. Yellowstone National Park is on three partly covered caldera complexes. The Long Valley Caldera in eastern California is also a complex volcano; the San Juan Mountains in southwestern Colorado are formed on a group of Neogene-age caldera complexes, and most of the Mesozoic and Cenozoic rocks of NevadaIdaho, and eastern California are also caldera complexes and their erupted ash flow tuffs. The Bennett Lake Caldera in British Columbia and the Yukon Territory is another example of a Cenozoic (Eocene) caldera complex.


eranir2

This article is about the volcano in Chile. For other uses, see Wallatiri (disambiguation).
Guallatire and Punata[1]) is a 6,071-metre-high (19,918 ft) volcano in Chile. It is located southwest of the Nevados de Quimsachata volcanic group. It is a stratovolcano with fumaroles around the summit, which may be either a lava dome or a pyroclastic cone. The lower flanks of the volcano are covered by lava flows and lava domes.
Guallatiri has been active in historical times with a number of eruptions, the last in 1960. Fumarolic and seismic activity is ongoing. The volcano is covered by an ice cap.


eranir1

This article is about the volcano in Chile. For other uses, see Wallatiri (disambiguation).
Guallatiri
1990-00-00 SCN 0750 2.jpg
Fumarole activity in the crater of Guallatiri
Highest point
Elevation6,071 m (19,918 ft) [1]
Coordinates18°25′00″S 69°05′30″WCoordinates18°25′00″S 69°05′30″W[2]
Geography
Guallatiri is located in the northern part of Chile
Guallatiri is located in the northern part of Chile
Guallatiri
Location of Guallatiri in Chile
LocationPutreParinacota provinceArica y ParinacotaChile[3]
Geology
Age of rockPleistocene-Holocene
Mountain typeVolcano
Volcanic fieldNevados de Quimsachata
Last eruption1960
Guallatiri (also known as Huallatiri, Huallatire, Guallatire and Punata[1]) is a 6,071-metre-high (19,918 ft) volcano in Chile. It is located southwest of the Nevados de Quimsachata volcanic group. It is a stratovolcano with fumaroles around the summit, which may be either a lava dome or a pyroclastic cone. The lower flanks of the volcano are covered by lava flows and lava domes.
Guallatiri has been active in historical times with a number of eruptions, the last in 1960. Fumarolic and seismic activity is ongoing. The volcano is covered by an ice cap.