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Rangpo River
River Rangpo is a river in the Indian state of Sikkim. A tributary of the Teesta River, it originates from Menmecho Lake near Dzuluk and flows through Rongli and Pakyong subdivision villages in Pakyong District towards Rorathang, Kumrek and Rangpo. The river demarcates the border between Pakyong District of Sikkim and Kalimpong district of West Bengal from Rorathang to Rangpo. At the town of Rangpo the river joins river Teesta. River Rangpo is the third largest river of Sikkim after Teesta and Rangeet. Atal Setu Bridge the longest roadway bridge of sikkim lies over River Rangpo. The river runs through Pakyong District of Sikkim and a few parts of the Kalimpong District of West Bengal. This tributary flows mainly from east to west with a variable channel pattern including braided, meandering, straight, gorge and blocked lake. Landslides are very common along the river bank as cliff-like bedrocks are significantly exposed along the river valley wall. During Monsoon season e ...
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India
India, officially the Republic of India (Hindi: ), is a country in South Asia. It is the seventh-largest country by area, the second-most populous country, and the most populous democracy in the world. Bounded by the Indian Ocean on the south, the Arabian Sea on the southwest, and the Bay of Bengal on the southeast, it shares land borders with Pakistan to the west; China, Nepal, and Bhutan to the north; and Bangladesh and Myanmar to the east. In the Indian Ocean, India is in the vicinity of Sri Lanka and the Maldives; its Andaman and Nicobar Islands share a maritime border with Thailand, Myanmar, and Indonesia. Modern humans arrived on the Indian subcontinent from Africa no later than 55,000 years ago., "Y-Chromosome and Mt-DNA data support the colonization of South Asia by modern humans originating in Africa. ... Coalescence dates for most non-European populations average to between 73–55 ka.", "Modern human beings—''Homo sapiens''—originated in Africa. Then, int ...
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Pakyong
Pakyong is the district headquarters of Pakyong District in the Indian state of Sikkim, located in the foothills of the Himalayas. It holds many Government Offices. Pakyong Airport is the only airport of Sikkim. The "National Research Centre for Orchids" ( ICAR Institute) is also located here. There is a missionary run school called St. Xavier's, which ranked as one of the top two schools in Sikkim during the 1990s. Notable among its alumni are the Padma Shri awardee footballer Baichung Bhutia, who captain India. History The existence of British bunkers at British Killa suggests the presence of armed bunkers sometime in the past. The name ''Pakyong'' comes from the Lepcha words ''pa yong'' meaning "bamboo of the bow", as it was a common practise of the Lepchas to name a place after the essential items found at a place. On 24 September 2018, Prime Minister Narendra Modi inaugurated Pakyong Airport. Regular air service started on 4 October 2018. Geography Loca ...
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Tareythang
Tareythang is a small village located in Pakyong sub division at the Pakyong District of Sikkim state in India. This village is about 1250 m above sea level with a sub-tropical climate. It is 12 kilometers away from Pakyong. In electoral roll of 2011, Tareythang comes under the Assembly Constituency of Chujachen. Etymology The legends of the village says that the name Tareythang comes from two words 'Tarey' which means the Tarey Bhir and the word 'Thang' means the plain land. It means the plain land under Tarey bhir is called as Tareythang. Population Composition Nepali-speaking people comprising Bahun, Chettri, Darjee and Sunar constitutes the majority of the population at Tareythang. Economy People are mainly engaged in primary sector like house farming, Agriculture, pitty business, Horticulture etc. People engaged in agriculture produce as their main crops every year is Paddy (Dhaan), Maize (Makkai), Broom Plant (Kuccho), millet (Kodho), Ginger (Adhuwa), vegetables prod ...
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Bering, Sikkim
Bering or Biring is a small village at Pakyong sub-division in the Pakyong District of Sikkim. It is 13 km away towards east from Pakyong Market. This small village is inhabited by Sharma, Chettri, Limboo, Rai communities. In the lower belt Sharma are in majority - Ghimire, Bastola, Bhattarai, Thapa, Kharka, Budathoki, Gotamey, Bogoti Khatiwara etc. are among the subcaste living in this area. Agriculture is the main occupation of the people of this area. Ginger, Amliso, are the main cash crop of this area. Paddy, maize, Millet, wheat are the cereal crop. Nearest town from this village is Pakyong in west and Rongli in east. This village falls under Pakyong Block development Office. Etymology The name Biring has multiple definitions. Some say that it's a corrupted version of Bu ring, a Bhutia word where bu stands for snake and ring stands for long. Others disagree. They believe Biring is a Lepcha word which means "full of bamboo", as this area was once densely packed with ba ...
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Chujachen
Chujachen is a large village located above Rongli Bazar, Pakyong District, numbering 816 households per a 2011 census. It resides at latitude 27.21 and longitude 88.68. History Meaning of the village name Chujachen means above pani dhara. The village origin By Norbu or Nopu Bhutiardsikkim.org/Files/VDAP%20Reports/.../Chujachen%20GPU.pdf In 1951 a primary School was established and later upgraded to a Senior secondary in 1984. Chujachen data According to the 2011 census, Chujachen's demographics are as follows: Notable people *Tulsiram Sharma Kashyap Tulsiram Sharma 'Kashyap' (11 February 1939 – 8 February 1998) was an Indian writer and politician in the Nepali language from Sikkim, India. He is a recipient of Sahitya Academy Award in Nepali for his 'Aama' (poetry) in 1990. He is the sec ... * Krishna Bahadur Rai * Mohan Gurung References Villages in Pakyong district {{Sikkim-geo-stub ...
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Lake Menmecho
Menmecho Lake is a mountain lake located in Gangtok district in the state of Sikkim, India. It lies on the way to the Jelep Pass and is situated at a distance of ahead of the Lake Tsomgo. It is the source of the river Rangpo chu, a tributary of the Teesta River. The waters of the lake are sourced by melting snow in summer, and the monsoon in the wet season. The lake is noted for its trout Trout are species of freshwater fish belonging to the genera '' Oncorhynchus'', ''Salmo'' and ''Salvelinus'', all of the subfamily Salmoninae of the family Salmonidae. The word ''trout'' is also used as part of the name of some non-salmoni ..., and has a large fish farm nearby with a guesthouse. Menmecho is closed to tourists. Gallery File:MenmoiTso lake.. the Cottage to stay.jpg, MenmoiTso lake.. the Cottage to stay File:MenmoiTso lake..the jungle trail towards the lake.jpg, MenmoiTso lake..the jungle trail towards the lake File:MenmoiTso lake..the distance first look.jpg, MenmoiTs ...
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Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave ...
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Landslides
Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as a heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable. Causes Landslides occur when the slope (or a portion of it) undergoes some processes that change its condition from stable to unstable. This is essentially due to a decrease in the shear strength of ...
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Gorge
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ...
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Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ...
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Braided River
A braided river, or braided channel, consists of a network of river channels separated by small, often temporary, islands called braid bars or, in English usage, ''aits'' or ''eyots''. Braided streams tend to occur in rivers with high sediment loads or coarse grain sizes, and in rivers with steeper slopes than typical rivers with straight or meandering channel patterns. They are also associated with rivers with rapid and frequent variation in the amount of water they carry, i.e., with "flashy" rivers, and with rivers with weak banks. Braided channels are found in a variety of environments all over the world, including gravelly mountain streams, sand bed rivers, on alluvial fans, on river deltas, and across depositional plains. Description A braided river consists of a network of multiple shallow channels that diverge and rejoin around ephemeral ''braid bars''. This gives the river a fancied resemblance to the interweaved strands of a braid. The braid bars, also known as channel ...
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Channel (geography)
In physical geography, a channel is a type of landform consisting of the outline of a path of relatively shallow and narrow body of water or of other fluids (e.g., lava), most commonly the confine of a river, river delta or strait. The word is cognate to canal, and sometimes takes this form, e.g. the Hood Canal. Formation Channel initiation refers to the site on a mountain slope where water begins to flow between identifiable banks.Bierman, R. B, David R. Montgomery (2014). Key Concepts in Geomorphology. W. H. Freeman and Company Publishers. United States. This site is referred to as the channel head and it marks an important boundary between hillslope processes and fluvial processes. The channel head is the most upslope part of a channel network and is defined by flowing water between defined identifiable banks. A channel head forms as overland flow and/or subsurface flow accumulate to a point where shear stress can overcome erosion resistance of the ground surface. Channel he ...
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