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Статті в журналах з теми "Himalaya Mountains Region – History"

1

Shen, Hong, та Christopher J. Poulsen. "Precipitation <i>δ</i><sup>18</sup>O on the Himalaya–Tibet orogeny and its relationship to surface elevation". Climate of the Past 15, № 1 (29 січня 2019): 169–87. http://dx.doi.org/10.5194/cp-15-169-2019.

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Abstract. The elevation history of the Himalaya–Tibet orogen is central to understanding the evolution and dynamics of both the India–Asia collision and the Asian monsoons. The surface elevation history of the region is largely deduced from stable isotope (δ18O, δD) paleoaltimetry. This method is based on the observed relationship between the isotopic composition of meteoric waters (δ18Op, δDp) and surface elevation, and the assumption that precipitation undergoes Rayleigh distillation under forced ascent. Here we evaluate how elevation-induced climate change influences the δ18Op–elevation relationship and whether Rayleigh distillation is the dominant process affecting δ18Op. We use an isotope-enabled climate model, ECHAM-wiso, to show that the Rayleigh distillation process is only dominant in the monsoonal regions of the Himalayas when the mountains are high. When the orogen is lowered, local surface recycling and convective processes become important, as forced ascent is weakened due to weaker Asian monsoons. As a result, the δ18Op lapse rate in the Himalayas increases from around −3 to above −0.1 ‰ km−1, and has little relationship with elevation. On the Tibetan Plateau, the meridional gradient of δ18O decreases from ∼1 to ∼0.3 ‰ ∘−1 with reduced elevation, primarily due to enhanced sub-cloud reevaporation under lower relative humidity. Overall, we report that using δ18Op or δDp to deduce surface elevation change in the Himalayan–Tibetan region has severe limitations and demonstrate that the processes that control annual-mean precipitation-weighted δ18Op vary by region and with surface elevation. In summary, we determine that the application of δ18O paleoaltimetry is only appropriate for 7 of the 50 sites from which δ18O records have been used to infer past elevations.
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2

Kundu, Jagadish, Kripamoy Sarkar, Ebrahim Ghaderpour, Gabriele Scarascia Mugnozza, and Paolo Mazzanti. "A GIS-Based Kinematic Analysis for Jointed Rock Slope Stability: An Application to Himalayan Slopes." Land 12, no. 2 (February 2, 2023): 402. http://dx.doi.org/10.3390/land12020402.

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GIS-based kinematic stability analysis in rock slopes is a rare practice in geological engineering despite its immense potential to delineate unstable zones in a mountainous region. In this article, we have used a GIS-based modified technique to assess the efficiency of kinematic analysis in predicting shallow landslides in the rock slopes of the Himalayan mountains on a regional scale. The limited use of this technique is primarily due to the complexities involved in its practical application. To make this technique more effective and convenient usability, we present modified methods and a new application, ‘GISMR’, that works with the aid of GIS software for the determination of kinematic susceptibility. A modified kinematic analysis method was implemented to define the stability in terms of failure susceptibility on a scale of 0 to 100 rather than a conservative result, such as failure or non-failure. We also present another functionality of the GISMR that provides optimised slope angles over a region. This functionality could aid the decision-making process when selecting a suitable location for a road path or other engineering constructions that are impacted by unstable mountain slopes. The applicability of this new method was demonstrated in a rock failure-prone region in the mountains of the Indian Himalayas. The outcomes delineate the unstable slopes in the region, which are intersected by a strategic National Highway 05 and have a long history of landslide-related hazards. It was found that 9.61% of the area is susceptible to failure. However, 2.28% is classified as a low susceptible region, and 2.58% of the area is very-low susceptible. The regions with moderately high, high, and very-high susceptibility cover 2.78%, 1.49%, and 0.46% of the whole area, respectively. The results were evaluated by receiver operating characteristic curve and a frequency ratio method to represent the association between kinematic susceptibility and the mass movement inventory in the area. It is concluded that kinematic susceptibility has a strong relationship with landslide activity in the rock slopes of the Himalayan region.
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3

GARDNER, KYLE. "MOVING WATERSHEDS, BORDERLESS MAPS, AND IMPERIAL GEOGRAPHY IN INDIA'S NORTHWESTERN HIMALAYA." Historical Journal 62, no. 1 (August 8, 2018): 149–70. http://dx.doi.org/10.1017/s0018246x18000146.

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AbstractThis article uses the British colonial history of border making in northern India to examine the assumptions and contradictions at work in the theorizing, configuring, and mapping of frontiers and borders. It focuses, in particular, on the development of the ‘water-parting principle’ – wherein the edge of a watershed is considered to be the border – and how this principle was used to determine boundaries in the northwestern Himalaya, a region that had long-established notions of border points, but no borderlines. By the twentieth century, the water-parting principle would become the dominant boundary logic for demarcating borders in mountainous regions, and would be employed by statesmen, treaty editors, and boundary commissioners around the world. But for the northwestern Himalaya, a region that British colonial officials considered to be the ‘finest natural combination of boundary and barrier that exists in the world’, making a border proved much more difficult than anticipated.
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Rawat, Neelam, Shuchi Mitra, Usha Sharma, and Khem Chand Sharma. "GUGGULU AND SHILAJIT: UNREVEALING THE THERAPEUTIC SECRETS OF HIMALAYAN FLORA." International Ayurvedic Medical Journal 11, no. 6 (June 21, 2023): 1430–35. http://dx.doi.org/10.46607/iamj3611062023.

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India contains a great wealth of biological diversity in its forests, its wetlands, and its marine areas which are distributed all over the country. It is a distinct identity on the world map, not only because of its geography, history, and culture but also because of its great diversity of natural ecosystems. The great Himalayan region is one of the unique biogeography of the world. The Himalayan Mountain range extends across India, China, Nepal, Afghanistan, Pakistan, Tibet, and Bhutan, where Nepal and India cover most of the Himalaya region. The diverse range in climate, altitude, and soil conditions of this renowned range supports a variety of distinct and valuable flora, which includes medicinal plants such as Artemisia, Rhododendron, Cinnamomum, Juniperus, Cymbopogon, Aegle, Swertia, Pinus, Origanum, Saussurea are some of the major plant genera and resins like Commiphora mukul, Asphaltum punjabianum are some medicinally important elements are found in the Himalayan forests. Thus, this chapter summarizes the two commonly used important Himalayan medicinal plants and their biological effects with incorporating the uniqueness of the Ayurvedic & Tibetan Systems of medicine.
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Shah, Rinan, and Shrinivas Badiger. "Conundrum or paradox: deconstructing the spurious case of water scarcity in the Himalayan Region through an institutional economics narrative." Water Policy 22, S1 (October 8, 2018): 146–61. http://dx.doi.org/10.2166/wp.2018.115.

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Abstract Water scarcity in mountain regions such as the Himalaya has been studied with a pre-existing notion of scarcity justified by decades of communities' suffering from physical water shortages combined by difficulties of access. The Eastern Himalayan Region (EHR) of India receives significantly high amounts of annual precipitation. Studies have nonetheless shown that this region faces a strange dissonance: an acute water scarcity in a supposedly ‘water-rich’ region. The main objective of this paper is to decipher various drivers of water scarcity by locating the contemporary history of water institutions within the development trajectory of the Darjeeling region, particularly Darjeeling Municipal Town in West Bengal, India. A key feature of the region's urban water governance that defines the water scarcity narrative is the multiplicity of water institutions and the intertwining of formal and informal institutions at various scales. These factors affect the availability of and basic access to domestic water by communities in various ways resulting in the creation of a preferred water bundle consisting of informal water markets over and above traditional sourcing from springs and the formal water supply from the town municipality.
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Gamble, Ruth. "How dams climb mountains: China and India’s state-making hydropower contest in the Eastern-Himalaya watershed." Thesis Eleven 150, no. 1 (February 2019): 42–67. http://dx.doi.org/10.1177/0725513619826204.

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The dam rush in the upper-Brahmaputra River basin and local, minority resistance to it are the result of complex geopolitical and parochial causes. India and China’s competing claims for sovereignty over the watershed depend upon British and Qing Dynasty imperial precedents respectively. And the two nation-states have extended and enhanced their predecessors’ claims on the area by continuing to erase local sovereignty, enclose the commons, and extract natural resources on a large scale. Historically, the upper basin’s terrain forestalled the thorough integration of this region into both nation-states, but recent technological and economic advances have enabled the two states and their agents to dramatically transformed these landscapes. Many of their projects have perpetuated the interventionist hydrological regimes that India and China also inherited from their imperial forebears. Nevertheless, as with their definition of their borders, neither state has highlighted this historical contingency. Instead, both governments have consistently presented their hydropower projects as shining examples of necessary and benevolent development. Their economy-focused, monolithic development paradigms have, not coincidently, also enabled the systemic side-lining of non-majority cultures, religions and histories. The combination of this cultural exclusion and the nation-states’ late integration of this peripheral region has laid the ground for conflict with local groups over the dam rush. Local identities and experiences have evolved around complex religious, cultural and trade networks, many of which were heavily influenced by the now-defunct Tibetan polity, rather than via modern Chinese and Indian nationalist discourses of development. The dam clashes highlight both the basin’s complex cultural matrixes and the ambiguous relationship Asia’s two most populous nation-states have with their respective imperial pasts. And as the situation remains unresolved, the watershed is an ecological catastrophe in waiting.
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SEARLE, M. P., S. R. NOBLE, A. J. HURFORD, and D. C. REX. "Age of crustal melting, emplacement and exhumation history of the Shivling leucogranite, Garhwal Himalaya." Geological Magazine 136, no. 5 (September 1999): 513–25. http://dx.doi.org/10.1017/s0016756899002885.

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We report a U–Pb monazite age of 23.0±0.2 Ma for the Shivling leucogranite, a tourmaline+muscovite±biotite leucogranite at the top of the High Himalayan slab in the Garhwal Himalaya, north India. The Shivling–Bhagirathi leucogranite is a viscous near-minimum melt, emplaced as a foliation parallel laccolith via a dyke network not far from its source region. Prograde heating occurred soon after the India–Asia collision at c. 50 Ma up to melting at 23 Ma and high temperatures (>550 °C) were maintained for at least 15 Ma after garnet growth. The leucogranite was emplaced at mid-crustal depths along the footwall of the Jhala fault, a large-scale low-angle normal fault, part of the South Tibetan Detachment system, above kyanite and sillimanite grade gneisses. The geometry of the leucogranite laccolith shows biaxial extension and boudinage both perpendicular (north-northeast–south-southwest) and parallel to the strike (west-northwest–east-southeast) of the mountain range. Unroofing occurred by underthrusting beneath the High Himalayan slab along the Main Central Thrust zone, progressively ‘jacking up’ the leucogranites, removal of material above by low-angle normal faulting, and erosion. Very rapid cooling at rates of 200–350 °C/Ma between 23–21 Ma immediately followed crystallization, as tectonic unroofing and erosion removed 24–28 km of overburden during this time. K–Ar muscovite ages are 22±1.0 Ma and fission track ages of zircons from >5000 m on the North Ridge of Shivling are 14.2±2.1 and 8.8±1.2 Ma and apatites are 3.5±0.79 and 2.61±0.23 Ma. Slow steady state cooling at rates of 20–30 °C/Ma from 20–1 Ma shows that maximum erosion rates and unroofing of the leucogranite occurred during the early Miocene. This timing coincides with initiation of low-angle, north-dipping normal faulting along the South Tibetan Detachment system.
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8

Kandel, Samikshya, and Luna Thapa. "Study of Space Layout of Museum; A Case of International Mountain Museum at Pokhara, Nepal." Technical Journal 3, no. 1 (December 31, 2023): 91–108. http://dx.doi.org/10.3126/tj.v3i1.61942.

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Currently, the museum is one of the learning and pass time activities space for the public. A good layout of a museum can bring a wonderful visiting experience to the visitors. Overall, museums play an important role in preserving a town's cultural heritage, providing educational opportunities, attracting tourism, and promoting community engagement. Effective space distribution in a museum is critical for creating an engaging and informative experience for visitors. By carefully considering the needs and interests of different types of visitors, museums can create spaces that are both functional and aesthetically pleasing. But there are very few designed museums in Pokhara, one of the growing cities of Nepal. Also, it is one of the tourist attracting places in Nepal. This paper explains the spatial layout of one of the designed museums of Pokhara. For this purpose, a well-known International Mountain Museum is taken as a case area by using observation and questionnaire survey methods. This museum displays a wide range of exhibits related to the Himalayan mountains, mountaineering, and the culture of the people who call the region home. In addition to the mountaineering exhibits, the museum also features displays of the history, culture, geology, flora, and fauna of the Himalayas. Overall, space distribution in a museum is designed to facilitate the flow of visitors through the space, while also highlighting the key messages and themes of the exhibits.
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Bhutia, Dechen Dolkar, and Namrata Chaturvedi. "Soldier Saints, Missionaries and the Mountains." International Journal of Asian Christianity 6, no. 1 (March 1, 2023): 51–72. http://dx.doi.org/10.1163/25424246-06010004.

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Abstract This paper intends to contextualise the life of Christianity in British India through the developments in military theology in the late eighteenth and through the nineteenth century that put forth the image of the ‘soldier saint’- a true Christian soldier, British in blood and in faith. This discourse intensified after the military turned civilian Indian rebellion of 1857 which was immediately coloured in Christian vs heathen terms, and following which, the spiritual needs of Christian soldiers came into focus with the East India Company. The deaths, rituals and continued traditions of burial of the Christian soldiers, officers, and civilians have been marked through some prominent cemeteries and war memorials in India. While studies of these sites of memory have focused on the graves, tombs, and memorials in parts of north, west and south India, the frontier region of northeast India has remained outside the focus of most studies. This paper has chosen the eastern Himalayan territories comprising Sikkim and Kalimpong that fall on or near the Silk route to bring attention to the history of territorial aggression and the resulting material memory of lesser-known cemeteries and memorials Further. This paper analyses lesser discussed fiction to bring into focus the region’s human geography. This paper recognises the need to study inter-religious relations through materiality and afterlives of Christianity in India that was shaped to a large extent by the soldiers-both British and native, and the chaplains, gravediggers, priests and nurses and caregivers whose lives are recorded in the memory of death. By doing so, this study hopes to bring new dimensions to the study of Christianity in India with the inclusion of the materiality of religion, the postcolonial gothic imaginary and military theology.
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Lixin, Yang, Huai Huyin, and Pei Shengji. "Medicinal Plants and Their Conservation in China with Reference to the Chinese Himalayan Region." Asian Medicine 5, no. 2 (2009): 273–90. http://dx.doi.org/10.1163/157342109x568810.

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The use of herbal medicine in China has a long history. Since ancient times, plants have been the main source of medicines for people’s healthcare all over China. Today, medicinal plants are widely used in different medical systems including Traditional Chinese Medicine (TCM) and Tibetan Medicine (TM) for health care and functional food in China, and as supplies of natural products for industrial manufacturing for the international market. In the last half-century, great progress has been made in science and technology and there has been rapid social and economic development. The impact of this rapid development and population pressures on medicinal plants from wild habitats increases day by day. The modernization policy of traditional medicine in China is seen as a challenge to maintaining traditional medical systems. The Chinese Himalayan Region covers five provinces (Tibet, Qinghai, Gansu, Sichuan, and Yunnan) in west China, with a land area of 2 million km², including the Qinghai-Tibetan Plateau in the west and the Hengduan Mountains in the southwest. In this paper, we discuss the rich diversity of medicinal plants of China and the Chinese Himalayan Region; the diversity of medicinal plant utilization of China; threatened medicinal plants and threats to medicinal plants; the conservation status of medicinal plants in China; and proposed Important Plant Areas for medical plants in the Chinese Himalayan Region.
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Дисертації з теми "Himalaya Mountains Region – History"

1

Nodari, Maria Luisa. "Climbing for the nation : epics of mountaineering in Tibet." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648226.

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2

Gautam, Ritesh. "Aerosol-radiation-climate interactions over the Gangetic-Himalayan region." Fairfax, VA : George Mason University, 2008. http://hdl.handle.net/1920/3353.

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Thesis (Ph.D.)--George Mason University, 2008.
Vita: p. 167. Thesis director: Menas Kafatos. Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Earth Systems an GeoInformation Sciences. Title from PDF t.p. (viewed Jan. 11, 2009). Includes bibliographical references (p. 156-166). Also issued in print.
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3

Grubensky, Michael J. "Structure, geochemistry, and volcanic history of mid-Tertiary rocks in the Kofa Region, southwestern Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/558071.

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4

McClelland, William Cabell. "The accretionary history of the Alexander terrane and structural evolution of the Coast Mountains batholith: Evidence from geologic, geochronologic, and thermobarometric studies in the Petersburg region, central southeastern Alaska." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185033.

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Rocks west of the Coast Mountains batholith in central southeastern Alaska include the Alexander terrane, Gravina belt, Taku terrane, and newly defined Ruth assemblage. Geologic, geochronologic and thermobarometric studies of these rocks in the Petersburg region provide new constraints on the accretionary history of the Alexander terrane and structural evolution of the Coast Mountains batholith. Paleozoic and Upper Triassic strata of the Alexander terrane were deformed within the Duncan Canal shear zone. Dextral shear in this zone during Early or Middle Jurassic time is inferred to reflect deformation along the eastern margin of the Alexander terrane and record the juxtaposition of the Alexander terrane with the North American margin. Deposition of the Upper Jurassic-Lower Cretaceous Gravina belt occurred within a transtensional back-arc to intra-arc basin that evolved during the northward translation of the Alexander terrane. The Ruth assemblage and Taku terrane were structurally emplaced over the Gravina belt and Alexander terrane along the Sumdum-Fanshaw fault system during mid-Cretaceous time. West-vergent thrusting of the Ruth assemblage was accompanied by metamorphic P,T conditions of 6.8 kb, < 450°C in the Gravina belt and 6.9 to > 7.4 kb, > 550°C in the Ruth assemblage. The age of deformation is constrained by syntectonic and post tectonic intrusive bodies that yield U-Pb lower intercept apparent ages of 92.3 ± 3 Ma and 91.3 ± 6.3 Ma, respectively. Late Devonian-Mississippian orthogneiss and felsic metavolcanic rocks in the Ruth assemblage suggest correlation of the assemblage with continental margin rocks of the Yukon-Tanana and Nisling terranes east of the Coast Mountains batholith. Thus the mid-Cretaceous Sumdum-Fanshow fault system marks the fundamental boundary between the Alexander terrane and inboard fragments. This deformation records the final structural accretion of the Alexander, Wrangellia, and Peninsular terranes to the western margin of North America. The mid-Cretaceous thrust system is truncated to the east by the LeConte Bay shear zone: a complex zone of Late Cretaceous-early Tertiary fabrics that occur within and west of the Coast Mountains batholith. This zone has apparently accommodated both west-side-up and east-side-up displacement during the collapse of the overthickened crust developed during mid-Cretaceous time.
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5

Challis, Sam. "The impact of the horse on the AmaTola 'Bushmen' : new identity in the Maloti-Drakensberg mountains of southern Africa." Thesis, University of Oxford, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.711605.

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King, Rachel. "Voluntary barbarians of the Maloti-Drakensberg : the BaPuthi chiefdom, cattle raiding, and colonial rule in nineteenth-century southern Africa." Thesis, University of Oxford, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.669789.

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7

Yamada, Kunimi. "Thermochronology using (U-Th)/He dating method : investigation for effects of secular disequilibrium on (U-Th)/He ages and uplift history of the Tanzawa mountains in the south Fossa Magna region." 京都大学 (Kyoto University), 2006. http://hdl.handle.net/2433/144205.

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Kyoto University (京都大学)
0048
新制・課程博士
博士(理学)
甲第12122号
理博第3016号
新制||理||1450(附属図書館)
23958
UT51-2006-J117
京都大学大学院理学研究科地球惑星科学専攻
(主査)助教授 田上 高広, 教授 嶋本 利彦, 教授 小畑 正明
学位規則第4条第1項該当
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Girardin, Jordan. "Travel in the Alps : the construction of a transnational space through digital and mental mapping (c. 1750s-1850s)." Thesis, University of St Andrews, 2017. http://hdl.handle.net/10023/10648.

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The period between the 1750s and 1830s witnessed a major change in travel practices in Europe, moving away from the traditional Grand Tour and focusing more on natural places, their visual power, and their influence on individual emotions. Such changes meant that the Alps ceased to be seen as a natural obstacle that had to be crossed in order to access Italy, and became a place to explore and a mountainous space par excellence. This thesis addresses the importance of mental mapping in travel literature and its impact on the construction of the Alps as a transnational space, which eventually facilitated the creation of a viable touristic market in the Alps as we know it today. The first part of the thesis analyses the transformation of the Alps from a natural frontier to a border region explored by travellers and their networks. The second part discusses the consequences of these changes on mental mapping and spatial representations of the Alps by travellers: it highlights the way external visitors often had very subjective interpretations of what the Alps meant as a term and a place, and conveyed those to other travellers through travel writing. Finally, the third part of this work investigates the development of an Alpine myth as a product of these shifting mental representations: the Alps became a set of expectations, typical images, and encounters to be expected.
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Cardoso, Silvia Regina Travaglia. "História natural das serpentes das região de Munhoz, sul de Minas Gerais, Serra da Mantiqueira." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/87/87131/tde-30052012-090358/.

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Estudando uma comunidade de serpentes da Serra da Mantiqueira, foram encontradas 11 espécies de serpentes, e constatada a superioridade numérica de indivíduos da família Viperidae. As áreas abertas foram as mais freqüentadas, além de mostrar maior riqueza de espécies. A maioria das espécies encontradas apresenta a viviparidade como modo reprodutivo. A altitude mostrou influenciar a distribuição e abundância das espécies. As três espécies mais abundantes foram B. neuwiedi, B. jararaca e C. durissus, e são apresentadas informações de sua história natural. As fêmeas são maiores e mais robustas do que os machos. Entre filhotes, o dimorfismo sexual não ocorre ou é restrito. Fêmeas são mais ativas na primavera e no verão, e machos no outono. As fêmeas parecem ser mais agressivas. As três espécies alimentam-se preferencialmente de pequenos mamíferos. A espermatogênese e a vitelogênese são sazonais, e machos e fêmeas estocam espermatozóides no trato genital a fim de harmonizarem seus ciclos. O nascimento dos filhotes ocorre no verão.
This study was conducted in the Serra da Mantiqueira, and show biological and ecological aspects within a community of snakes. Eleven species were found. The snakes was mostly found in open areas, and open areas also showed a greater richness of species. A significant percentage of the species reproduced by viviparity. Altitude influenced the abundance and distribution of the species. The three dominant species of snakes was B. neuwiedi, B jararaca and C. durissus. Females are bigger and stronger then the males. Among the young, sexual dimorphism does not happen or it is restricted. Females also showed increased activity during the spring and summer, whiles males had increased activity levels during the autumn months. Females were more aggressive. These three species feed primarily on small mammals. Spermatogenesis and vitellogenesis are seasonal, and males and females show sperm storage in the genital tract so their cycles are harmonized. B. jararaca is bigger and stronger than B. neuwiedi, and female B. jararaca have larger and heavier litters.
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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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Книги з теми "Himalaya Mountains Region – History"

1

P, Karan Pradyumna, and Pacheco Julsun, eds. Himalaya: Life on the edge of the world. Baltimore: Johns Hopkins University Press, 1999.

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Kellner, Debra. Jacques Perrin presents Himalaya: A film by Eric Valli. New York: Harry N. Abrams, 2001.

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3

Mountains of the God: [spiritual ecology of Himalaya region]. Delhi: Isha Books, 2007.

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4

Sharma, Chandra K. Geology of Nepal Himalaya and adjacent countries. Kathmandu: Sangeeta Sharma, 1990.

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5

Sharma, Chandra K. Geology of Nepal Himalaya and adjacent countries. Kathmandu, Nepal: Sangeeta Sharma, 1990.

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6

Environmental Information System on Himalayan Ecology., ed. Natural resource management and development in Himalaya: A resource to issues and strategies. Almora: Environmental Information System on Himalayan Ecology, 1997.

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7

Kapadia, Geeta. The Himalaya in my sketchbook. New Delhi: Indus Pub. Co., 1996.

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8

1951-, Harris Brian, and Wardle Heather, eds. Tibetan voices: A traditional memoir. San Francisco: Pomegranate Artbooks, 1996.

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9

Sharma, Man Mohan. Yatra: Pilgrimages in the western Himalayas. Noida: Trishul Publications, 1989.

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10

Sharma, Man Mohan. Yatra: Pilgrimages in the western Himalayas. Noida: Trishul Publications, 1992.

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Частини книг з теми "Himalaya Mountains Region – History"

1

Ghimire, Tirth Raj, Anita Bhattarai, Nirju Ojha, Pitamber Pant, and Sagar Aryal. "Wildlife Diplomacy and Gifting in the Hindu Kush-Himalaya Region: A Chronological History and Opinion of Nepalese Literates." In Hindu Kush-Himalaya Watersheds Downhill: Landscape Ecology and Conservation Perspectives, 419–33. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36275-1_21.

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2

Bajracharya, Birendra, Daniel E. Irwin, Rajesh Bahadur Thapa, and Mir A. Matin. "Earth Observation Applications in the Hindu Kush Himalaya Region—Evolution and Adoptions." In Earth Observation Science and Applications for Risk Reduction and Enhanced Resilience in Hindu Kush Himalaya Region, 1–22. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-73569-2_1.

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AbstractThe year 1957 marked the start of a new era in human history with the launch of Sputnik, thus began the journey of Earth observation (EO). Then, in the early 1960s, with rapid developments in space technology and the race to reach the moon, scientific discussions veered toward the potential applications of EO in the fields of geography, agriculture, water resources, geology, and oceanography (NASA: Sputnik and the dawn of the space age, 2017; Haklay et al. in Earth observation open science and innovation, ISSI scientific report series 15, 2018).
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3

Paparella, Francesco, and John A. Burt. "Climate of the United Arab Emirates: Present, Past and Impacts on Life." In A Natural History of the Emirates, 65–94. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-37397-8_3.

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AbstractThe United Arab Emirates (UAE) straddles 22–26 °N, positioning it in a latitudinal band well known across the globe for its desert biomes. The UAE is characterized by arid to hyper-arid conditions, but with marked variation in precipitation seasonally (highest in winter/spring) and across locations (highest near the Hajar mountains), representing a dramatic shift from the more humid conditions that characterized this region just six millennia ago. The low cloud cover, limited vegetation and poorly developed soil also result in extreme and highly variable temperatures across the year, particularly in areas distant from the coasts. Winds are typically dominated by daily land/sea breezes, but occasional brief ‘shamal’ wind events (particularly in late winter) or cyclones (in early summer) can have important implications for temperature, rainfall and biotic responses. Average temperatures have increased by 1 °C between the 1980s and the 2010s, and rainfall has declined by more than half; in addition, wet bulb temperatures associated with human health are increasing, and may exceed life-threatening levels by the end of the century. Today’s climate represents extremely marginal conditions for life, and the current trends suggest that the already vulnerable ecosystems and organisms of the UAE are coming under increasing climate-related pressure.
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4

Nichols, Douglas J., Jack A. Wolfe, and David T. Pocknall. "Latest Cretaceous and Early Tertiary history of vegetation in the Powder River Basin, Montana and Wyoming." In Tertiary and Cretaceous Coals in the Rocky Mountains Region: Casper, Wyoming to Salt Lake City, Utah June 29–July 8, 1989, 28–33. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft132p0028.

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5

Harrison, T. Mark, An Yin,, and Frederick J. Ryerson. "Orographic Evolution of the Himalaya and Tibetan Plateau." In Tectonic Boundary Conditions for Climate Reconstructions, 39–72. Oxford University PressNew York, NY, 1998. http://dx.doi.org/10.1093/oso/9780195112450.003.0003.

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Abstract The effect of orography on climate has been evaluated using several atmospheric circulation models (Manabe and Terpstra, 1974; Hahn and Manabe, 1975; Barron and Washington, 1984; Kutzbach et al., 1989; 1993). These simulations generally indicate that major climate changes can be triggered by the appearance of a mountain belt or the uplift of a large region which underscore the fundamental importance of understanding the orographic evolution of mountain belts in order to place constraints on reconstructions of past climate over time scales of 106 to 107 years (Crowley, this volume, Chapter 1). For example, there is accumulating evidence that the appearance of a high and extensive Himalayan-Tibetan mountain system significantly influenced Neogene climate (Hahn and Manabe, 1975; Ruddiman and Kutzbach, 1989; Quade et al., 1989; Kutzbach et al., 1993). In general, however, the complex and spatially variable uplift history of the plateau that is emerging from recent geologic studies (Harrison et al., 1992; Murphy et al., 1997) have not been considered in these models, and those that have attempted to make a link (e.g., Raymo et al., 1988) may have been misled by spurious inferences from paleobotanical studies (see Appendix).
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6

Gupta, Avijit. "Landforms of Southeast Asia." In The Physical Geography of Southeast Asia. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199248025.003.0013.

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Southeast Asia is a corner of the continent of Asia which ends in an assemblage of peninsulas, archipelagos, and partially enclosed seas. Towards the northwest, the physical contact of this region with the rest of Asia is via a mountainous region that includes the eastern Tibetan Plateau, the eastern Himalaya Mountains, the hills and plateaux of Assam (India) and of Yunnan (China). From this high region a number of large, elongated river basins run north–south or northwest–southeast. These are the basins of rivers such as the Irrawaddy, Salween, Chao Phraya, Mekong, and Sông Hóng (Red). An east–west traverse across the mainland part of Southeast Asia, therefore, is a repetition of alluvium-filled valleys of large rivers separated by mountain chains or plateaux. To the south and to the east are coastal plains, rocky peninsulas, and a number of deltas. Beyond lies the outer margin of Southeast Asia, the arcuate islands of Indonesia, and the Philippines with steep volcanic slopes, intermontane basins, and flat coastal plains of varying size. This assemblage of landforms has resulted from a combination of plate tectonics, Pleistocene history, Holocene geomorphic processes, and anthropogenic modifications of the landscape. Most of the world has been shaped by such a combination, but unlike the rest of the world, in Southeast Asia all four are important. The conventional wisdom of a primarily climate-driven tropical geomorphology is untenable here. The first two factors, plate tectonics and the Pleistocene history, have been discussed in Chapters 1 and 2 respectively. In the Holocene, Southeast Asia has been affected by the following phenomena: • The sea rose to its present level several thousand years ago. • The present natural vegetation, a major part of which includes a set of rainforest formations, achieved its distribution. • A hot and humid climate became the norm, except in the high altitudes and the extreme northern parts. • The dual monsoon systems blowing from the northeast in the northern hemispheric winter and from the southwest in the summer (and in general producing a large volume of precipitation) became strongly developed.
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7

Gündoğdu, Abdullah. "Türkiye ve Türk Dünyası Tarih Bilincinde Cengiz ve Halefleri Algısı." In Cengiz Han ve Mirası, 76–110. Turkish Academy of Science, 2021. http://dx.doi.org/10.53478/tuba.2021.024.

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The great steppe belt, stretching from Lake Baikal in Southern Siberia to the Himalayan mountains, from Manchuria to Eastern Europe and the Balkans, connects Europe and Asia transversely. The Turkic and Mongolian peoples, the inhabitants of this continuous wide belt defined as central Eurasia, established the largest empires in the ancient and medieval world history with their great military movements and migrations. Among these empires, the founding of the Genghis Empire is a unique event of its kind in world history. The countries of the vast Eurasian region, from the Far East to Central Asia and Eastern Europe, were united for the first time in their history under the rule of the same dynasty. After the XIII. century, the axis of world history was based on the relations and struggles of the four great branches that formed the empire for more than three centuries – the Yuan / Kublai, Ilkhanli, Golden Horde and Chagatai khanates - among themselves and with other states. Emir Timur, who entered the struggle for the revival of the empire in the field of the Chagatai Khanate, opened the door of a new era connecting this process to modern history. There is a need to consider how the perception of Genghis and his successors is reflected on the historiography and historical consciousness in identity construction in Turkey and the Turkic world.
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8

NeCamp, Samantha. "Conclusion." In Literacy in the Mountains, 94–112. University Press of Kentucky, 2020. http://dx.doi.org/10.5810/kentucky/9780813178851.003.0006.

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The conclusion examines present-day perceptions of Appalachia to illustrate the ongoing harm caused by the persistence of stereotypes regarding Appalachians’ literacy practices. It argues that, by reframing Appalachian history, we can begin to see that, while the current circumstances in the region are indeed a product of history, they are not a product of the history presented in popular narratives about the region—narratives that attribute any negative development in Appalachia to the natural consequence of Appalachia’s supposed long-standing poverty and ignorance. Recovering Appalachia’s literacy history gives us a new lens through which to examine the region’s experiences, expectations, and potential futures.
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9

Searle, Mike. "Continents in Collision: Kashmir, Ladakh, Zanskar." In Colliding Continents. Oxford University Press, 2013. http://dx.doi.org/10.1093/oso/9780199653003.003.0007.

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To understand how the Himalaya were formed it seemed logical to start at the actual zone of plate collision, the Indus suture zone. Most of this collision zone runs across southern Tibet, which in the 1970s was almost impossible to travel through. Following Mao Tse-tung’s Red Army’s invasion and occupation of Tibet in October 1950, that region had remained firmly closed to all foreigners. In the western Himalaya the Indus suture zone runs right across the northernmost province of Ladakh. Ladakh used to be a part of southwestern Tibet before the British annexed it during the Raj. Leh, the ancient capital of Ladakh at 3,500 metres in the Indus Valley, was the final outpost of British India before the great trans-Himalayan barrier of the Karakoram Range. Only the Nubra Valley and the Tangtse Valley north of Leh were beyond the Indus, and these valleys led directly up to the desolate high plateau of Tibet. Leh was a major caravan route and a crossroads of high Asia, with double-humped dromedary camel caravans coming south from the Silk Route towns of Yarkhand and Khotan; Kashmiris and Baltis came from the west and Indian traders from the Hindu regions of Himachal and Chamba to the south. Ladakh, Zanskar, and Zangla were three ancient Himalayan kingdoms ruled by a Giapo, or King, each from a palace that resembled a small version of the Potala Palace in Lhasa. In 1978, when we were climbing in the mountains of Kulu, I had looked from our high summits across to the desert mountains of Lahoul and Zanskar, north of the main Himalayan watershed. Here, in the ancient Buddhist kingdoms of Zanskar and Ladakh lay wave upon wave of unexplored and unclimbed mountains. They lay north of the monsoon limits and in the rain shadow of the main Himalaya, so the vegetation was sparse, and the geology was laid bare. Flying north from Delhi, or east from Kashmir into Leh, the views were simply mesmerizing.
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10

NeCamp, Samantha. "Introduction." In Literacy in the Mountains, 1–12. University Press of Kentucky, 2020. http://dx.doi.org/10.5810/kentucky/9780813178851.003.0001.

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The introduction details the ways in which Appalachia has come to represent heart of “Trump Country.” It argues that these representations trade on a long history of stereotypes and assumptions about the region. In particular, the introduction describes how Appalachia is represented as illiterate, unschooled, and textless, a representation that dates from the 1880s and served the needs of both the extract industries and northern missionaries bent on “improving” the region. The introduction outlines the key theoretical frames for the remainder of the book, including Deborah Brandt’s theory of literacy sponsorship and Benedict Anderson’s notion of imagined communities.
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Тези доповідей конференцій з теми "Himalaya Mountains Region – History"

1

Coffey, Kevin T., Raymond V. Ingersoll, Raymond V. Ingersoll, Johanna F. Hoyt, and Johanna F. Hoyt. "IMPLICATIONS OF THE VINCENT GAP REGION OF THE EASTERN SAN GABRIEL MOUNTAINS FOR THE NEOGENE HISTORY OF SOUTHERN CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274120.

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2

J. Podber, Jacob. "Bridging the Digital Divide in Rural Appalachia: Internet Usage in the Mountains." In 2003 Informing Science + IT Education Conference. Informing Science Institute, 2003. http://dx.doi.org/10.28945/2708.

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This project looks at Internet usage within the Melungeon community of Appalachia. Although much has been written on the coal mining communities of Appalachia and on ethnicity within the region, there has been little written on electronic media usage by Appalachian communities, most notably the Melun-geons. The Melungeons are a group who settled in the Appalachian Mountains as early as 1492, of apparent Mediterranean descent. Considered by some to be tri-racial isolates, to a certain extent, Melungeons have been culturally constructed, and largely self-identified. According to the founder of a popular Melungeon Web site, the Internet has proven an effective tool in uncovering some of the mysteries and folklore surrounding the Melungeon community. This Web site receives more than 21,000 hits a month from Melungeons or others interested in the group. The Melungeon community, triggered by recent books, films, and video documentaries, has begun to use the Internet to trace their genealogy. Through the use of oral history interviews, this study examines how Melungeons in Appalachia use the Internet to connect to others within their community and to the world at large.
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3

Craig, Taylor D., Michael L. Wells, and Thomas D. Hoisch. "STRUCTURAL AND KINEMATIC HISTORY OF THE CHLORIDE CLIFF REGION: IMPLICATIONS FOR TECTONIC INHERITANCE IN THE FORMATION OF THE FUNERAL MOUNTAINS METAMORPHIC CORE COMPLEX, DEATH VALLEY, CA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303880.

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4

HANDANOVIC, DIJANA, ALLAN PEREZ, and SARA ROMERO. "Inventive Resilience." In 111th ACSA Annual Meeting Proceedings. ACSA Press, 2023. http://dx.doi.org/10.35483/acsa.am.111.14.

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As the capital of Bosnia and Herzegovina, Sarajevo for a long time was known for the 1914 assassination of the Austrian Archduke Francis Ferdinand, the final event precipitating World War I. After hosting the 1984 Winter Olympics, Sarajevo was perceived around the world as a place of peaceful gathering, but in April 1992, following the proclamation of Bosnia and Herzegovina’s independence from the Yugoslavian Federation, the Bosnian War started and again shifted the world’s perception of Bosnia and Herzegovina to one as a place of violence. After the recognition of dissolution, Bosnian Serb forces besieged the city of Sarajevo and for four years the city was subjected to bombings and gunfire. Sarajevo lies in a valley of the Miljacka River and is surrounded by mountains on all sides. Due to the geography of the region, artillery and snipers staged from the mountains had clear vantage points across the entire city. The Siege of Sarajevo, which lasted 1,425 days and resulted in 11,541 fatalities, including 1,600 children, became renowned as the most prolonged military siege in contemporary history. Sarajevo’s architecture and urban spaces suffered catastrophic damage, prompting civilian life to go underground where day to day life was constricted to only the absolute essentials. The constant bombings of the city not only transformed existing buildings, streets, and neighborhoods, but also forced civilians to reinvent their main dwellings. This was documented in 1994 by architect Zoran Doršner in his drawings “Destructive Metamorphosis.”
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D., TSEND. "FEATURES OF THE LOCATION OF THE MONGOLIAN TIME BURIAL MOUNDS IN NORTHERN MONGOLIA." In MODERN SOLUTIONS TO CURRENT PROBLEMS OF EURASIAN ARCHEOLOGY. Altai State Univercity, 2023. http://dx.doi.org/10.14258/msapea.2023.3.44.

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In Northern Mongolia, 245 burials at 41 sites have been excavated in Khubsugul, Bulgan, Selenge, and Darkhan-Uul aimags since the beginning of the study of funerary sites of Mongolian time in the 1980s. Although much material has been obtained to provide sufficient information on the history of medieval Mongolia, little excavation has been carried out in this region as a whole. It is clear from the data on the number of mounds that some sites contain a lot of mounds at the same time. It is also noteworthy that, geographically, the burial complexes of the developed Middle Ages are located on slopes, at the foot and on saddles of mountains and on terraces. In addition, all burial mounds excavated in Northern Mongolia are located along the riverbank. Based on the materials of burials investigated on the territory of Northern Mongolia and dated to the Mongolian time, the article considers their location and notes some peculiarities.
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Clark, S. "Regional Tectonics & Structural Framework of Offshore Aceh's Andaman Sub-Basin, Northern Sumatra, Indonesia." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-30.

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The three-way collision of the Indo-Australian, Eurasian and Pacific plates have resulted in Southeast Asia being the most tectonically complex region on Earth. This is particularly true for Offshore Aceh’s Andaman Sub-Basin, which has undergone complex late Eocene-Recent evolution. Despite a long history of hydrocarbon exploration and production, data scarcity in the offshore means that the Sub-Basin’s regional tectonics and structural framework have been poorly understood. Pre-1996 2D seismic data were low-fold and low-offset, however the 2019 PGS (NSMC3D) regional 3D survey imaged the entire Cenozoic sequence, enabling the delineation of a high-resolution tectonic framework for the first time. Integration of interpretations drawn from geophysical datasets with a 2019 biostratigraphy study has refined the ages of critical sequence boundaries and advanced the understanding of major structural elements. GEM™, the Geognostics Earth Model, has been used to place these interpretations in a regional tectonic and kinematic context using a series of high resolution plate animations. Andaman Sub-Basin formation initiated in response to the northward motion of India and collision with Eurasia, suturing the West Burma and Sibumasu Terranes through the middle-late Eocene. Continued northward motion of the Indo-Australian Plate resulted in further subduction along the Sunda Trench with associated oblique back-arc extension in present-day onshore and offshore Java and Sumatra. Concurrent rotation of Sundaland, with sinistral strike-slip motion along the Ranong and Khlong Mauri fault zones, resulted in the two rifting phases within the late Eocene (~40Ma) to early Oligocene in the Andaman Sub-Basin. Significant inversion events at 30Ma and 23Ma formed in response to dextral transpression associated with rotational extrusion of Indochina and Sundaland. Rapid subsidence followed the 30Ma inversion, resulting in a switch to post-rift sag and bathyal conditions during which turbidites infilled seabed topography. The onset of dextral strike slip between the West Burma Terrane along the Saigang fault system occurred at ~26Ma, causing transtension in the Andaman Sub-basin that terminated at 23Ma. At approximately 5Ma inversion and toe thrusts developed along the Sub-Basin’s southern margin due to uplift within the Barisan mountains. Refinement of the tectonic model, integrated with updated biostratigraphic and geochemical models, resulted in a revised tectono-stratigraphy for the Andaman Sub-Basin, which provides a predictive depositional model in which paleogeography and structural reactivation can be understood in a regional context.
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Звіти організацій з теми "Himalaya Mountains Region – History"

1

Mendelsohn, Mark, John Tiszler, and Tarja Sagar. Vegetation monitoring in the Santa Monica Mountains and Simi Hills region: 2014?2020 annual report. National Park Service, 2023. http://dx.doi.org/10.36967/2300992.

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Our Inventory & Monitoring team surveyed over 200 Terrestrial Native Vegetation Monitoring Plots in the Santa Monica Mountains and Simi Hills (SAMO) Region over the first seven years of this program?s history, 2014?2020. During this period, the park experienced a large wildfire in 2013 followed by historic drought, and then in 2018 the largest wildfire in the region?s recorded history, succeeded by well-timed rainfall. The goal of this monitoring program is to detect and understand the nature of vegetation change, for example in drought or post-fire environments, providing a knowledge base for developing effective management strategies. Our metrics include vegetation cover, species richness, shrub/tree abundance, survival, and recruitment. In general, SAMO experienced widescale native shrub dieback during the extended drought. Dry shrublands that subsequently burned to the ground in 2018 converted into a rich and widespread green-up with the substantial rains received in 2019, producing a very diverse assemblage of wildflowers (including many fire followers not seen in many years) and a strong recruitment of our native shrubs via resprouting and seedlings into 2020 across most of the park?s more pristine areas. We documented post-fire expansions in several populations of the federally endangered Braunton?s milkvetch. Non-native herbaceous species such as mustards dominated previously disturbed lands and expanded their coverage following the 2018 wildfire. The data we collected will be available for advancing the science of fire ecology, and informing future park management and interpretation programs.
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2

Duk-Rodkin, A., and R. W. Barendregt. Glacial history and limits of Cordilleran and Laurentide ice sheets in the Mackenzie Mountains, foothills, and plains, Northwest Territories: a brief overview. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331422.

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This Mackenzie Mountains and foothills paper covers a large region of the southern and western parts of the Northwest Territories extending from the continental divide in the Cordillera to the Interior Plains. This is a summary of the glacial and preglacial history of the region, supported by maps of glacial limits and surficial geology, as well as important stratigraphic and field-observation sites depicting remnant features of preglacial landscapes and the extent of continental glaciers.
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3

Towns in the Mountains; Report of the International Workshop on Planned Urbanisation and Rural-Urban Linkages in the Hindu Kush-Himalaya Region. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1986. http://dx.doi.org/10.53055/icimod.25.

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4

Towns in the Mountains; Report of the International Workshop on Planned Urbanisation and Rural-Urban Linkages in the Hindu Kush-Himalaya Region. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1986. http://dx.doi.org/10.53055/icimod.25.

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People and Jobs in the Mountains; Report of the International Workshop on Off-Farm Employment Generation in the Hindu Kush-Himalaya Region. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1986. http://dx.doi.org/10.53055/icimod.23.

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6

The HKH Call to Action to sustain mountain environments and improve livelihoods in the Hindu Kush Himalaya. International Centre for Integrated Mountain Development (ICIMOD), 2020. http://dx.doi.org/10.53055/icimod.1.

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Анотація:
This HKH Call to Action is based on the HKH Assessment, which was drafted in response to requests from governments in the region, meeting a demand for a comprehensive assessment of the region’s mountains, environments, and livelihoods and proposes actions towards a shared vision for the future of the HKH region, in which its societies and its people are prosperous, healthy, peaceful, and resilient in a healthy environment. To realize this vision, this HKH Call to Action elaborates six urgent actions, including: 1) promote and strengthen regional cooperation at all levels to sustain mountain environment and livelihoods; 2) recognize and prioritize the uniqueness of the HKH mountain people; 3) take concerted climate actions; 4) take accelerated actions to achieve the SDGs, consistent with the nine mountain priorities; 5) take decisive actions to enhance ecosystem resilience; and 6) promote regional data and information sharing.
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