Thematische Bibliographien / Eastern Himalayan

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Auswahl der wissenschaftlichen Literatur zum Thema „Eastern Himalayan“

Autor: Grafiati

Veröffentlicht am 18. Mai 2024

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Zeitschriftenartikel zum Thema "Eastern Himalayan"

Kirisits, Thomas, Edwin Donaubauer, Heino Konrad, Sangay Dorji, Irene Barnes, Wolfgang Maier, Michael J. Wingfield, Norbu Gyeltshen und D. B. Chhetri. „Common Needle, Shoot, Branch and Stem Diseases of Conifer Trees in Bhutan“. Acta Silvatica et Lignaria Hungarica 3, Special Edition (01.06.2007): 241–45. http://dx.doi.org/10.37045/aslh-2007-0038.

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Bhutan is a small, landlocked, densely forested country in the South-Eastern Himalayas (FAO 1999, 2001). Forests are of immense importance for the ecology, economy and social well-being of this country and for the livelihood of its people. In mountainous areas at elevations between about 2100 and 4200 m asl., temperate conifer forests form the natural vegetation in this part of the Himalayas. These forests occupy about 24% of the total area of Bhutan and they consist mainly of Eastern Himalayan fir (Abies densa), Eastern Himalayan spruce (Picea spinulosa), Himalayan hemlock (Tsuga dumosa) and Himalayan Blue pine (Pinus wallichiana) (Grierson – Long 1983, Rosset 1999). Other conifers and various broadleaved tree species (Rhododendron spp., Betula spp., Populus spp., Acer spp., Sorbus spp. and Salix spp.) are often admixed to the aforementioned major conifer species or sometimes dominate forest stands on specific sites (Grierson – Long 1983, Rosset 1999). Another important conifer in Bhutan is Chir pine (Pinus roxburghii), which occurs mainly in sub-tropical and warm temperate forests (Grierson – Long 1983). This pine does, however, not form part of cold temperate conifer forests.

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Ojha, Lujendra, Ken L. Ferrier und Tank Ojha. „Millennial-scale denudation rates in the Himalaya of Far Western Nepal“. Earth Surface Dynamics 7, Nr. 4 (11.10.2019): 969–87. http://dx.doi.org/10.5194/esurf-7-969-2019.

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Abstract. The Himalayas stretch ∼3000 km along the Indo-Eurasian plate boundary. Along-strike variations in the fault geometry of the Main Himalayan Thrust (MHT) have given rise to significant variations in the topographic steepness, exhumation rate, and orographic precipitation along the Himalayan front. Over the past 2 decades, the rates and patterns of Himalayan denudation have been documented through numerous cosmogenic nuclide measurements in central and eastern Nepal, Bhutan, and northern India. To date, however, few denudation rates have been measured in Far Western Nepal, a ∼300 km wide region near the center of the Himalayan arc, which presents a significant gap in our understanding of Himalayan denudation. Here we report new catchment-averaged millennial-scale denudation rates inferred from cosmogenic 10Be in fluvial quartz at seven sites in Far Western Nepal. The inferred denudation rates range from 385±31 t km−2 yr−1 (0.15±0.01 mm yr−1) to 8737±2908 t km−2 yr−1 (3.3±1.1 mm yr−1) and, in combination with our analyses of channel topography, are broadly consistent with previously published relationships between catchment-averaged denudation rates and normalized channel steepness across the Himalaya. These data show that the denudation rate patterns in Far Western Nepal are consistent with those observed in central and eastern Nepal. The denudation rate estimates from Far Western Nepal show a weak correlation with catchment-averaged specific stream power, consistent with a Himalaya-wide compilation of previously published stream power values. Together, these observations are consistent with a dependence of denudation rate on both tectonic and climatic forcings, and they represent a first step toward filling an important gap in denudation rate measurements in Far Western Nepal.

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Deepani, Vijit, und Monika Saini. „Demographic Fluctuation among Himalayan Populations“. Indian Journal of Research in Anthropology 3, Nr. 2 (15.12.2017): 107–14. http://dx.doi.org/10.21088/ijra.2454.9118.3217.6.

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Background: Himalayas constitute vast mountain range in Asia spreading over 2500 Km (from east to west) at a high altitude along the northern fringes of the Indian subcontinent. The population dynamics in Himalayan domain has been immensely influenced by the variations in climatic and topographic conditions. As a result, population trends in relation to several demographic parameters are observed as population growth varies across this immense geographical contour. Objective: The present study attempts to assess and compare several crucial demographic parameters of select population groups (tribes and caste groups) residing in Himalayan province so as to provide a comprehensive picture of their demographic profile. The variation in demographic variables has also been addressed in relation to socio-economic and biological attributes. Materials and Methods: Multiple demographic determinants viz., sex-ratio, index – of – ageing, age at marriage and menarche, crude birth rate, total fertility rate, crude death rate and infant mortality rate are utilized to address demographic diversity in Himalayan population groups. Results: The sex ratio has been observed to be higher among reported population groups in Central Himalayas in comparison to Western and Eastern Himalayas. The measures of fertility – CBR, GFR and TFR – depict high values in certain population groups of Central Himalayas (Johar Bhotia, Rang Bhotia and Raji) in comparison to Western and Eastern province. Contribution: The present paper provides a comprehensive picture of the demographic profile among select Himalayan population groups. This will aid to understand the trend in demographic characteristics in the Himalayan province.

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Priestley, Keith, Tak Ho und Supriyo Mitra. „The crustal structure of the Himalaya: A synthesis“. Geological Society, London, Special Publications 483, Nr. 1 (2019): 483–516. http://dx.doi.org/10.1144/sp483-2018-127.

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AbstractThis chapter examines the along-arc variation in the crustal structure of the Himalayan Mountain Range. Using results from published seismological studies, plus large teleseismic body-wave and surface-wave datasets which we analyse, we illustrate the along-arc variation by comparing the crustal properties beneath four representative areas of the Himalayan Mountain Range: the Western Syntaxis, the Garhwal–Kumaon, the Eastern Nepal–Sikkim, and the Bhutan–Northeastern India regions. The Western Syntaxis and the Bhutan–Northeastern India regions have a complicated structure extending far out in front of the main Range, whereas the Central Himalaya appear to have a much simpler structure. The deformation is more distributed beneath the western and eastern ends of the Range, but in general, the crust gradually thickens from c. 40 km on the southern side of the Foreland Basin to c. 80 km beneath the Tethys Himalaya. While the gross crustal structure of much of the Himalaya is becoming better known, our understanding of the internal structure of the Himalaya is still sketchy. The detailed geometry of the Main Himalayan Thrust and the role of the secondary structures on the underthrusting Indian Plate are yet to be characterized satisfactorily.

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Chetia, Hiranmoy, und Murali Krishna Chatakonda. „Record of Himalayan Marmot Marmota himalayana (Hodgson, 1841) (Rodentia: Sciuridae) from Arunachal Pradesh, India“. Journal of Threatened Taxa 15, Nr. 5 (26.05.2023): 23262–65. http://dx.doi.org/10.11609/jott.8402.15.5.23262-23265.

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In India, the Himalayan Marmot Marmota himalayana occurs in Ladakh, Himachal Pradesh, Uttarakhand, Sikkim, and Arunachal Pradesh. In this communication, we describe the single sighting of foraging and storing of grass by Himalayan Marmots in the eastern Himalayan landscape of western Arunachal Pradesh and address the threats that we noticed. Though the species occur in different areas of India, no systematic work has been done till now to assess their population status and distribution, let alone in the state of Arunachal Pradesh.

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Rai, Ishwari Datt, Gajendra Singh und Gopal Singh Rawat. „Anemone trullifolia and Berberis angulosa as new records to the flora of the western Himalaya, India“. Journal of Threatened Taxa 10, Nr. 5 (26.04.2018): 11679. http://dx.doi.org/10.11609/jott.3961.10.5.11679-11682.

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The western Himalaya represent an important and distinct botanical sub-region and biogeographic zone in the Himalayan Biodiversity Hotspot. There is a long history of floral exploration in this region as compared to the eastern Himalaya; however, recent additions of several species to western Himalayan flora reveal remote areas yet to be explored intensively. The present reports on Anemone trullifolia and Berberis angulosa from the subalpine-alpine areas of western Himalaya also emphasize the need for further exploration. In this article, a brief description of these species is presented along with distribution, ecology, phytogeographical notes and photographs are provided for easy identification.

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GAYEN, SUBRATA, und KAILASH CHANDRA. „A new distributional range of Abraxas antipusilla Inoue, 1995 (Lepidoptera: Geometridae) from Eastern Himalaya, India“. Zootaxa 5228, Nr. 2 (12.01.2023): 187–94. http://dx.doi.org/10.11646/zootaxa.5228.2.6.

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Based on Indian Himalayan expeditions, the species Abraxas antipusilla Inoue, 1995 is reported for the first time from Eastern Himalaya, India. After two decades, differential diagnoses of males and females are presented in comparison to Abraxas pusilla Butler, 1880. Redescriptions of male and female genitalia are given. An annotated summary on habitat preference and distributional ranges for both species is emphasized within the Indian Himalayan Region.

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Gurung, Yuvraj. „A Review on Chironomidae (Diptera) of the Eastern Himalayan Region: An Insight into Distribution and Conservation“. UTTAR PRADESH JOURNAL OF ZOOLOGY 44, Nr. 24 (14.12.2023): 45–59. http://dx.doi.org/10.56557/upjoz/2023/v44i243808.

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The Chironomidae (Diptera) commonly known as “midges”, are the most widely distributed and frequently the most abundant group of insects in freshwater ecosystems. Chironomids larvae plays a key ecological role in the maintenance of aquatic ecosystem services, mainly in secondary production and energy flow dynamics [1]. They are the freshwater bio-monitoring indicators of pollution, habitat modifications, and natural changes of water quality [2,3], and is a model which helps to predict diversity and strength of food web of aquatic communities [4]. The objective of the study is to highlight the distribution pattern, biodiversity and the status of conservation of Eastern Himalaya region species of the family Chironomidae. The 'Himalayan Biodiversity Hotspot' is indeed a "store house of biodiversity" because of its rich spectrum of species of flora and fauna including insect species which have been remaining unexplored. This study is a descriptive analysis to assay the main trends on Chironomidae research in freshwater assessments like ecology, palaeolimnology, biogeography, cytology, developmental and eco-toxicological research in Eastern Himalaya region. Finally the review work helps to get a more comprehensive picture of fauna of chironomids in the Eastern Himalayas in relation to those reported earlier from other parts of the globe.

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Sahgal, Vinay Sahu, Ashish Kumar Asthana, und Deepa Srivastava. „On the Occurrence of Plagiobryum zieri (Dicks. ex Hedw.) Lindb. in Western Himalaya“. INTERNATIONAL JOURNAL OF PLANT AND ENVIRONMENT 6, Nr. 03 (25.07.2020): 222–24. http://dx.doi.org/10.18811/ijpen.v6i03.12.

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Plagiobryum zieri (Dicks. ex Hedw.) Lindb. inhabitant of higher altitude has been recorded for the first time from Uttarkashi, Uttarakhand of the Western Himalaya earlier known from Sikkim (Eastern Himalaya). About 25 species of Plagiobryum are known worldwide. A morpho-taxonomic account of Western Himalayan plants of Plagiobryum zieri is provided.

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Adhikari, Drona, Champak Babu Silwal und Lalu Prasad Paudel. „Review of the Geology of the Arun-Tamor Region, Eastern Nepal: Present Understndings, Controversies and Research Gaps“. Journal of Institute of Science and Technology 26, Nr. 2 (29.12.2021): 79–97. http://dx.doi.org/10.3126/jist.v26i2.41439.

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Systematic study of the eastern Nepal Himalaya was started after 1950 when Nepal opened up for foreigners. Thereafter, several geological studies have been carried out in the Arun-Tamor region of eastern Nepal Himalaya. The Tibetan-Tethys sedimentary sequence, the Higher Himalayan amphibolite to granulite facies metamorphic crystalline sequence, the Lesser Himalayan sedimentary and greenschist facies metasedimentary sequences, and the Siwalik foreland molassic sedimentary sequence are the four major tectonic units of this area. The individual nomenclature schemes of stratigraphic units, the correlational dispute, the positions and interpretations of regional geological structures are some examples that have created controversies regarding the lithostratigraphy and structural arrangements. The difference in age and genesis of the Main Central Thrust and its effects in the metamorphism of the eastern Nepal Himalaya are the exemplification of the contradiction in the interpretation of the tectonometamorphic history. There is a gap in research in the tectonics and episodic metamorphic evolution of the area owing to the bare approach in the microstructural and geochronological investigation. Future investigations should be focused on solving the above mentioned controversies and narrowing down the research gaps in tectonic and metamorphic evolution.

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Dissertationen zum Thema "Eastern Himalayan"

Streule, Michael. „The structural, metamorphic and magmatic evolution of the Greater Himalayan Sequence and Main Central Thrust, Eastern Nepal Himalaya“. Thesis, University of Oxford, 2009. http://ora.ox.ac.uk/objects/uuid:c7e9c6ba-0bcd-4526-903f-a48d629e0dd9.

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Field observations of the Greater Himalayan Sequence in Eastern Nepal demonstrate a ductile, highly strained package of metamorphic rocks that show extensive evidence of crustal anatexis throughout. These can be distinguished from the Lesser Himalayan sequence below by a distinct reduction in metamorphic grade, an inverted metamorphic sequence and a high strain zone corresponding to the Main Central Thrust. Metamorphic studies are combined with geochronology to demonstrate a protracted period of crustal melting followed by rapid decompression from 18.7 Ma to 15.6 Ma. A metamorphic decompression rate is quantified at c.2mm/yr during this period. This is interpreted to represent exhumation of the Greater Himalayan Sequence by a process of ductile, channelised flow from the mid-crust beneath Tibet. Below a prominent band of kyanite gneiss, previously used to locate the Main Central Thrust, but here mapped within the Greater Himalayan Sequence, partial melting is still exhibited. Here monazites are dated at 10.6 Ma. In the Lesser Himalaya below, allanites record a similar 10.1 Ma event. This implies that following channel flow during the mid-Miocene, the channel widened in the lower-Miocene to incorporate a greater structural thickness. Following these two periods of exhumation and ductile extrusion, separated in time and space, Fission Track studies indicate that much slower, erosion driven exhumation proceeded, at <1 mm/yr. This rate increases slightly in the Pliocene, most likely in response to Northern Hemisphere glaciation; no difference in exhumation is seen across the Greater Himalayan Sequence with respect to the different, earlier, phases of ductile channel flow related exhumation. These results demonstrate the episodic nature of channel flow in the Himalaya and reconcile arguments about the position of the MCT in Eastern Nepal.

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Oliver, Lee. „The implications of metamorphism and weathering of the Lesser Himalayan formation in Eastern Nepal for climate change“. Thesis, University of Liverpool, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.275057.

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Holt, William Everett. „The active tectonics and structure of the Eastern Himalayan Syntaxis and surrounding regions“. Diss., The University of Arizona, 1989. http://hdl.handle.net/10150/184802.

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I determined the source parameters of 53 moderate-sized earthquakes in the region of the Eastern Himalayan Syntaxis through the joint inversion of regional and teleseismic distance long-period body waves. The average rates of deformation are determined by summing the moment tensors from both recent and historic earthquakes. Strike-slip movement on the Sagaing fault terminates in the north (just south of the syntaxis), where thrusting (northeast convergence) and crustal thickening are predominant. Slip vectors for thrust mechanisms in the Eastern Himalaya in general are not orthogonal to the Himalayan mountain front but show an oblique component of slip. A combination of thrust and strike-slip faulting (Molnar and Deng, 1984) for the great 1950 Assam earthquake is consistent with the rates of underthrusting in the entire Himalaya and the rate of spreading in Tibet (assuming that a 1950-type earthquake recurs every 400 years). An estimated 4-21 mm/yr of right-lateral motion between southeast Asia and the Burma subplate is absorbed within the zone of distributed shear between the Sagaing and Red River faults. A component of westward motion (3-7 mm/yr) of the western boundary of the distributed shear zone may cause some of the late Cenozoic compression and folding in the northern Indoburman Ranges. Distributed shear and clockwise rotation of blocks is also occurring in Yunnan north of the Red River Fault. The inversion of 130 regional distancewaveforms for average crustal thickness and upper mantle Pn velocity indicates an increase in Pn velocity, coincident with increase in crustal thickness, of about 0.20 km/s beneath the Tibetan Plateau. Impulsive Pn arrivals from paths that cross the Tibetan Plateau can be modeled with a positive upper mantle velocity gradient, indicating an upper mantle lid approximately 100-km-thick beneath southern Tibet. This "shield-like" structure supports a model in which Indian continental lithosphere has underthrust Tibet. The crustal shortening within Tibet 8 mm/yr is thus viewed as an upper crustal phenomenon in which the faults do not penetrate the deep crust or upper Mantle. The forces generated by the thick crust in Tibet may partly cause the strike-slip faulting and east-west convergence in Sichuan and the movement of upper crustal blocks in Yunnan.

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Buckingham, Heather Marie. „Evolution and late stage deformation of the Himalayan metamorphic core, Kanchenjunga region, eastern Nepal“. Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/51563.

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Understanding the recent history of the Himalayan orogen not only helps elucidates near-surface convergence accommodation processes, but also provides constraints for geometric modification of earlier midcrustal structures. New ⁴⁰Ar/³⁹Ar and fission track (FT) data from the former Himalayan metamorphic core exposed in the Kanchenjunga region of eastern Nepal help constrain the evolution and low temperature uplift history of this portion of the orogen. Within the Lesser Himalayan Sequence (LHS), new apatite FT dates, combined with existing apatite and zircon FT dates from the region, define general younging trends towards the north - up structural section - of ~2.9 to 1.3 Ma and ~6.2 to 4.6 Ma respectively. There appears to be a significant jump in apatite FT dates from 1.3 Ma to 2.4 Ma that is coincident with an abrupt change in existing muscovite ⁴⁰Ar/³⁹Ar ages from the Proterozoic to the Cenozoic. This break in ages is consistent with the mapped location of the Main Central thrust (MCT) fault in the area. In structurally lower rocks in the Greater Himalayan Sequence (GHS), north of the MCT, trends in both muscovite ⁴⁰Ar/³⁹Ar and apatite FT continue to decrease to the north. These trends are interpreted to be consistent with the exhumation and uplift of these rocks associated with the growth of a duplex system within the LHS developed through underplating. Cooling rates across the mapped area indicate fast cooling in the GHS in early to mid Miocene, coupled with very slow cooling in the LHS. In the late Miocene to Pleistocene, cooling rates slow down in the GHS and increase in the LHS, such that they are similar. This is consistent with development of late-stage duplexing within the LHS at this time and the coupled exhumation of the GHS. Biotite ⁴⁰Ar/³⁹Ar dates may indicate a complex history across the study area. Some biotite dates (~24-16 Ma) are older than nearby ²³²Th-²⁰⁸Pb monazite melt crystallization dates (~18-16 Ma). Previous studies have attributed similar old biotite dates to excess argon. It is possible, however, the old biotite dates indicate crystallization along the retrograde path prior to final melt crystallization.
Irving K. Barber School of Arts and Sciences (Okanagan)
Earth and Environmental Sciences, Department of (Okanagan)
Graduate

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Bera, Prasanta Kumar. „Phenotypic and molecular characterization of Siri (Bos indious) cattle breed from Eastern Sub-Himalayan region“. Thesis, University of North Bengal, 2017. http://ir.nbu.ac.in/hdl.handle.net/123456789/2611.

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Lahiri, Tapesh. „Characterisation of the soils of the Eastern Himalayan region together with an attempt of the separation of components of artificial and natural clay mixtures“. Thesis, University of North Bengal, 1989. http://hdl.handle.net/123456789/849.

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Choudhuri, Govinda. „Forest CPRs and usufructuary rights in a changing forest base : a case study of community adaptation in the Eastern Himalayan“. Thesis, University of North Bengal, 2010. http://hdl.handle.net/123456789/1375.

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Brezina, Cynthia A. „The detrital mineral record of Cenozoic sedimentary rocks in the Central Burma Basin : implications for the evolution of the eastern Himalayan orogen and timing of large scale river capture“. Thesis, University of St Andrews, 2015. http://hdl.handle.net/10023/6730.

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This study contributes to the understanding of major river evolution in Southeast Asia during the Cenozoic. In order to trace the evolution of a hypothesized palaeo-Yarlung Tsangpo-Irrawaddy River, this work undertakes the first systematic provenance study of detrital minerals from Cenozoic synorogenic fluvial and deltaic sedimentary rocks of the Central Burma Basin, employing a combination of high precision geochronology, thermochronology, and geochemistry analytical techniques on single grain detrital zircon and white mica. The dataset is compared to published isotopic data from potential source terranes in order to determine source provenance and exhumation history from source to sink. A Yarlung Tsangpo-Irrawaddy connection existed as far back as ca. 42 Ma and disconnection occurred at 18–20 Ma, based on provenance changes detected using a combination of U-Pb ages and εHf(t) values on detrital zircons, and ⁴ºAr/³⁹Ar dating on detrital micas. During the Eocene and Oligocene, units are dominated by U-Pb age and high positive εHf(t) values, characteristic of a southern Lhasa Gangdese magmatic arc source. An antecedent Yarlung Tsangpo-Irrawaddy River system formed the major river draining the eastern Himalaya at this time. A significant change in provenance is seen in the early Miocene, where detritus is predominantly derived from bedrock of the eastern Himalayan syntaxis, western Yunnan and Burma, a region drained by the modern Irrawaddy-Chindwin river system characterized by Cenozoic U-Pb ages and negative εHf(t) values. This is attributed to the disconnection of the Yarlung-Irrawaddy River and capture by the proto-Brahmaputra River, re-routing Tibetan Transhimalayan detritus to the eastern Himalayan foreland basin. Re-set zircon fission track ages of 14-8 Ma present in all units is used to infer post-depositional basin evolution related to changes in the stress regime accommodating the continued northward migration of India. The early Miocene initiation of the Jiali-Parlung-Gaoligong-Sagaing dextral shear zone and the continued northward movement of the coupled India-Burma plate aided in focusing deformation inside the syntaxis contributing to the disconnection of the Yarlung Tsangpo-Irrawaddy system, linking surface deformation and denudation with processes occurring at deeper crustal levels.

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Biswas, Saswati. „Impact of developmental agencies on the Eastern Himalayas with specific reference to the West Bengal Himalayas: a study of two villages“. Thesis, University of North Bengal, 1985. http://hdl.handle.net/123456789/211.

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Brown, Kerry Lucinda. „Dīpaṅkara Buddha and the Patan Samyak Mahādāna in Nepal: Performing the Sacred in Newar Buddhist Art“. VCU Scholars Compass, 2014. http://scholarscompass.vcu.edu/etd/3635.

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Every four years, in the middle of a cold winter night, devotees bearing images of 126 Buddhas, Bodhisattvas, and other important deities assemble in the Nepalese city of Patan for an elaborate gift giving festival known as Samyak Mahādāna (“The Perfect Great Gift”). Celebrated by Nepal’s Newar Buddhist community, Samyak honors one of the Buddhas of the historical past called Dīpaṅkara. Dīpaṅkara’s importance in Buddhism is rooted in ancient textual and visual narratives that promote the cultivation of generosity through religious acts of giving (Skt. dāna). During Samyak, large images of Dīpaṅkara Buddha ceremoniously walk in procession to the event site, aided by a man who climbs inside the wooden body to assume the legs of the Buddha. Once arranged at the event, Dīpaṅkara is honored with an array of offerings until dusk the following day. This dissertation investigates how Newar Buddhists utilize art and ritual at Samyak to reenact and reinforce ancient Buddhist narratives in their contemporary lives. The study combines art historical methods of iconographic analysis with a contextual study of the ritual components of the Samyak Mahādāna to analyze the ways religious spectacle embeds core Buddhist values within in the multilayered components of art, ritual, and communal performance. Principally, Samyak reaffirms the foundational Buddhist belief in the cultivation of generosity (Skt. dāna pāramitā) through meritorious acts of giving (Skt. dāna). However, the synergy of image and ritual performance at Samyak provides a critical framework to examine the artistic, religious, and ritual continuities of past and present in the Newar Buddhist community of the Kathmandu Valley. An analysis of the underlying meta-narrative and conceptualization of Samyak suggests the construction of a dynamic visual narrative associated with sacred space, ritual cosmology, and religious authority. Moreover, this dissertation demonstrates the role of Samyak Mahādāna in constructing Buddhist identity in Nepal, as the festival provides an opportunity to examine how Newar Buddhists utilize art, ritual, and performance to reaffirm their ancient Buddhist heritage.

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Bücher zum Thema "Eastern Himalayan"

Seṇṭāra phara Kamiunikeśāna ayāṇḍa Kalcārāla Ayākśāna (Calcutta, India) und Seminar on Eastern Himalayan Culture (1997 : Darjeeling, India), Hrsg. Glimpses of the eastern Himalayan culture. Calcutta: Centre for Communication and Cultural Action, 1999.

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B, Alfred J. R., und Zoological Survey of India, Hrsg. Status of Himalayan marmot, Marmota himalayana (Hodgson, 1841), in eastern Ladakh, Jammu & Kashmir, India. Kolkata: Zoological Survey of India, 2006.

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The Limbus: A South Eastern Himalayan kirata people. Kolkata: Sopan Publisher, 2011.

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Burrows, Lionel. Grammar of the Ho language: An Eastern Himalayan dialect. London: Trubner & Co., 2004.

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G, Verghese B., Iyer Ramaswamy R und Centre for Policy Research (New Delhi, India), Hrsg. Harnessing the eastern Himalayan rivers: Regional cooperation in South Asia. Delhi: Konark Publishers, 1993.

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Dutta, H. N., und Imotemsu Ao. Eastern Himalayan domestic architecture: With special reference to the North East India. Dimapur, Nagaland: Heritage Publishing House, 2017.

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G, Verghese B., Centre for Policy Research (New Delhi, India), Bangladesh Unnayan Parishad und Institute for Integrated Development Studies (Kathmandu, Nepal), Hrsg. Converting water into wealth: Regional cooperation in harnessing the eastern Himalayan rivers. Delhi: Konark Publishers, 1994.

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Fang, Jing. Potential threats from climate change to human wellbeing in the Eastern Himalayan Region. Kathmandu: International Centre for Integrated Mountain Development, 2010.

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Guangwei, Chen, und International Centre for Integrated Mountain Development., Hrsg. Biodiversity in the Eastern Himalayas: Conservation through dialogue : summary reports of workshops on biodiversity conservation in the Hindu Kush-Himalayan Ecoregion. Kathmandu: International Centre for Integrated Mountain Development, 2002.

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Cederlöf, Gunnel, und Willem van Schendel. Flows and Frictions in Trans-Himalayan Spaces. Nieuwe Prinsengracht 89 1018 VR Amsterdam Nederland: Amsterdam University Press, 2022. http://dx.doi.org/10.5117/9789463724371.

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Flows and Frictions in Trans-Himalayan Spaces traces movements and connections in a region known for its formidable obstacles to mobility. Eight original essays and a conceptual introduction engage with questions of networks and interconnection between people across a bordered landscape. Mobility among the extremely varied ecologies of south-western China, Myanmar and north-eastern India, with their rugged terrain, high mountains, monsoon-fed rivers and marshy lowlands, is certainly subject to friction. But today, harsh political realities have created hard borders and fractured this trans-Himalayan terrain. However, the closely researched chapters in this book demonstrate that these borders have not prevented an abundance of movements, connections and flows. Mobility has always coexisted with friction here, but this coexistence has been unsettled, giving this space its historical shape and its contemporary dynamism. Introducing the concept of the ‘corridor’ as an analytical framework, this collection investigates mobility and flows in this unique socio-political landscape.

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Buchteile zum Thema "Eastern Himalayan"

Sinha, Awadhesh C. „State formation among the Eastern Himalayan Kingdoms1“. In Federation of Himalayan Kingdoms, 27–52. London: Routledge India, 2022. http://dx.doi.org/10.4324/9780429400186-3.

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Sinha, Awadhesh C. „State formation and issues of Greater Nepal in the Eastern Himalayas“. In Federation of Himalayan Kingdoms, 9–26. London: Routledge India, 2022. http://dx.doi.org/10.4324/9780429400186-2.

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Mishra, Anupam. „Extension Strategies for Climate Resilient Agriculture in Eastern Himalayan“. In Transformation of Agri-Food Systems, 155–71. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-8014-7_13.

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Kumar, Devendra, und Aseesh Pandey. „Vegetation Structure Along an Elevation Gradient at the Treeline Ecotone of Eastern Himalayan Forests in Sikkim“. In Ecology of Himalayan Treeline Ecotone, 247–65. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-4476-5_10.

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Mohapatra, Jakesh, C. P. Singh, Priyadarshini Gurung, Bandan Gajmer, Narpati Sharma, Dhiren G. Shrestha und Himanshu A. Pandya. „Mapping the Spatial Patterns of Biodiversity Along the Alpine Treeline Ecotone in the Eastern Himalaya Using Information Theory“. In Ecology of Himalayan Treeline Ecotone, 169–89. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-4476-5_7.

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Komor, Puspa. „Dairy Farming in the Eastern Himalayan Foothills: Perspectives from the Lower Dibang Valley, India“. In Environmental Change in the Himalayan Region, 201–18. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-03362-0_11.

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Hasanuzzaman, Md, Pravat Kumar Shit und Aznarul Islam. „Role of Active Tectonism and Geomorphic Drivers on Channel Oscillation of the Raidak-I River in the Eastern Himalayan Foothills, India“. In Himalayan Neotectonics and Channel Evolution, 345–65. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-95435-2_13.

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Chakrabarti, Chandreyee Goswami, Belligraham Narzary, John C. Weber, Prasun Jana, Somhrita Bhattacharjee und Manoj Jaiswal. „Preliminary Study of the Manabhum Anticline: A Possible Key to Better Understanding the Quaternary Tectonics of the Eastern Himalayan Syntaxial Zone“. In Himalayan Neotectonics and Channel Evolution, 239–60. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-95435-2_9.

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Lama, Sonam, und Ramkrishna Maiti. „Morphotectonics of the Chel River Basin, Eastern Himalaya, India: Insights from Shuttle Radar Topography Mission Digital Elevation Model- Based Geomorphic Indices“. In Himalayan Neotectonics and Channel Evolution, 367–96. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-95435-2_14.

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Roy, Lopamudra, Somasis Sengupta, Sayantan Das und Arindam Sarkar. „Evaluating the Relative Tectonic Response of the Fluvial Systems Using Multicriteria Entropy Method: A Case Study of the Rangit Catchment, Eastern Himalayas, India“. In Himalayan Neotectonics and Channel Evolution, 315–43. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-95435-2_12.

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Konferenzberichte zum Thema "Eastern Himalayan"

Das, Saurabh, Swastika Chakraborty, Nirmal Rai, Aritra Dhar, Arnav Sadhu, Baishali Gautam, Pooja Verma, Anindita Singh, Chimila Sherpa und Madhura Chakraborty. „Eastern Himalayan Glaciar Hazard Analysis Using UAV-A Brief Approach“. In 2019 URSI Asia-Pacific Radio Science Conference (AP-RASC). IEEE, 2019. http://dx.doi.org/10.23919/ursiap-rasc.2019.8738483.

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Gordon, Stacia M., Carolina L. Zamora, Rick Kauffman, Rebecca Gonzales-Clayton und Sean P. Long. „TWO-STAGE EXHUMATION OF THE HIMALAYAN METAMORPHIC CORE: INSIGHTS FROM GREATER HIMALAYAN ROCKS IN CENTRAL AND EASTERN BHUTAN“. In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-351190.

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Zamora, Carolina L., Stacia M. Gordon, Sean P. Long, Andrew R. C. Kylander-Clark und C. S. McDonald. „EXHUMATION AND COOLING HISTORY OF GREATER HIMALAYAN ROCKS IN THE EASTERN HIMALAYA: A U-PB AND 40AR/39AR THERMOCHRONOLOGY STUDY FROM CENTRAL AND EASTERN BHUTAN“. In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285232.

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Huntington, Katharine W., Karl A. Lang und Michael D. Turzewski. „INTERACTIONS OF FLUVIAL EROSION, CLIMATE AND TECTONICS IN THE EASTERN HIMALAYAN SYNTAXIS“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304324.

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Zazubec, Alysha, Nandini Kar, Nandini Kar, Maggie Williams, Maggie Williams, Arijit Debnath, Arijit Debnath et al. „PALEOCLIMATE ANALYSIS OF THE NEOGENE EASTERN HIMALAYAN SIWALIK DEPOSITS THROUGH BIOMARKER PROXIES“. In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-393100.

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Lalrochunga, David, Collin Z. Renthlei, Arun Kumar Sarma, Adikanda Parida und Shibabrata Choudhury. „GIS-Based Image Processing for Farmland Site Selection: An Eastern Himalayan Region Perspective“. In 2024 14th International Conference on Cloud Computing, Data Science & Engineering (Confluence). IEEE, 2024. http://dx.doi.org/10.1109/confluence60223.2024.10463283.

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Lihter, Iva, Kyle P. Larson und John M. Cottle. „PETROCHRONOLOGICAL EVOLUTION OF THE HIMALAYAN METAMORPHIC CORE IN THE MAKALU-ARUN REGION, EASTERN NEPAL“. In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356375.

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Shi, Xuhua, Ray J. Weldon, Ray J. Weldon, Jing Liu-Zeng, Jing Liu-Zeng, Weerachat Wiwegwin, Weerachat Wiwegwin et al. „UNIFORM LATE QUATERNARY SLIP RATE ALONG THE JINGHONG FAULT, SE OF THE EASTERN HIMALAYAN SYNTAXIS“. In 115th Annual GSA Cordilleran Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019cd-329094.

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Verma, A., O. P. Mishra und J. Lei. „Pn Velocity and Anisotropic Tomography of the Uppermost Mantle under North-Eastern Indian Himalayan Orogenic Belt“. In 79th EAGE Conference and Exhibition 2017. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701489.

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Ghosh, Kausik, Francisco Munoz-Arriola und Tapan Chakraborty. „THE IMPACT OF RIVER REGULATION ON STREAMFLOW AND SEDIMENT DYNAMICS IN THE EASTERN HIMALAYAN RIVER BASIN“. In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355053.

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Berichte der Organisationen zum Thema "Eastern Himalayan"

Leduc, B., und J. Fang. Potential Threats from Climate Change to Human Wellbeing in the Eastern Himalayan Region; Climate Change Impact and Vulnerability in the Eastern Himalayas - Technical Report 6. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2010. http://dx.doi.org/10.53055/icimod.538.

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Pradhan, Nawraj, Dilip Chetry, Frank Momberg, Lily Shrestha, Naw May Lay Thant, Huang Zhipang, Nakul Chettri und Yi Shaoliang. Primates of the Far Eastern Himalaya. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2021. http://dx.doi.org/10.53055/icimod.785.

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Guangwei, C. Biodiversity in the Eastern Himalayas: Conservation through Dialogue. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2002. http://dx.doi.org/10.53055/icimod.382.

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Pathak, D., und P. K. Mool. Climate Change Impacts on Hazards in the Eastern Himalayas; Climate Change Impact and Vulnerability in the Eastern Himalayas - Technical Report 5. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2010. http://dx.doi.org/10.53055/icimod.519.

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Sharma, E., N. Chettri, M. Eriksson, P. K. Mool, F. Jing, A. B. Shrestha und K. Tse-ring. Climate Change Impacts and Vulnerability in the Eastern Himalayas. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2009. http://dx.doi.org/10.53055/icimod.497.

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Shrestha, A. B., A. K. Gosain und S. Rao. Modelling Climate Change Impact on the Hydrology of the Eastern Himalayas; Climate Change Impact and Vulnerability in the Eastern Himalayas - Technical Report 4. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2010. http://dx.doi.org/10.53055/icimod.534.

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