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The Himalayas, the tallest and the youngest mountains in the world, spread from Afghanistan and Pakistan through India, Bhutan, Nepal and Myanmar with their northern extrusions - the Ximalaya Shanmai - across the Tibetan plateau in China. Despite border restrictions, the inhabitants of this region continue to share a trans-Himalayan identity, fragile yet enduring. The Himalayan Arc focuses on a crucial, enthralling, politically turbulent, yet often underreported part of this Himalayan belt - the 'East of South-east'. With over thirty contributors, it attempts to describe the sense of shared lives and cultural connectivity between the denizens of this area. Poetry, fiction, and mysticism are juxtaposed with essays on strategy and diplomacy, espionage and the deep state, photographs, folk tales, and fables. From the unique identity of a Himalayan citizen to the 'geopolitical jigsaw' that is the region; from the hidden spy network in Kathmandu to intimate portraits of Shillong, Gangtok, Darjeeling, and other cities; from the insurgency in Assam to a portrait of Myanmar under military rule, the essays, stories, and poems in this anthology highlight the similarities within the differences of the Himalayan belt. Providing insider and outsider perspectives on this intriguing part of the world, The Himalayan Arc is a travel book with a difference. Contributors: Janice Pariat, Salil Tripathi, Ma Thida, Indra Bahadur Rai, Prajwal Parajuly, David Malone, Chetan Raj Shrestha, Kanak Mani Dixit, Sujeev Shakya, Pushpesh Pant, John Elliott, Amish Raj Mulmi, Thomas Bell, Sushma Joshi, Sanjoy Hazarika, Sudhindra Sharma, Tshering Tashi, Abhay K., Manoj Joshi, Catherine Anderson, Andrew Duff, Binodini, Jacqueline Zote, Aruni Kashyap, Sameer Tanti, Nitoo Das, Lutfa Hanum Selima Begum, Uddipana Goswami, Robin Ngangom, Akhu Chingangbam, Indira Goswami, Andrew Selth, Tulsi Badrinath, Meghna Pant, Mamang Dai, Desmond Kharmawphlang
Published by the American Geophysical Union as part of the Maurice Ewing Series, Volume 4. From May 12 to May 16, 1980, eighty-eight scientists from eleven countries attended a Symposium on Earthquake Prediction at Mohonk Mountain House, Mohonk, New York. This was the third in a biennial series honoring Maurice Ewing, first director of Lamont-Doherty Geological Observatory. The Symposium was one of several events that were held in 1980 to celebrate the 100th anniversary of the Graduate School of Arts and Sciences at Columbia University. The two earlier Ewing Symposia, on island arcs and deep sea drilling, reflected Ewing's lifelong interest in the structure and evolution of the ocean floor. In the Third Ewing Symposium we touch another area—earthquake seismology—that played an important part in Ewing's career. Work on surface waves and long-period seismology under Ewing's direction during the 1950's and 1960's, along with his exploration of the earth beneath the oceans, provided much of the framework on which current ideas on earthquake generation and plate tectonics are based.
The Himalaya–Karakoram–Tibet mountain belt resulted from Cenozoic collision of India and Asia and is frequently used as the type example of a continental collision orogenic belt. The last quarter of a century has seen the publication of a remarkably detailed dataset relevant to the evolution of this belt. Detailed fieldwork backed up by state-of-the-art structural analysis, geochemistry, mineral chemistry, igneous and metamorphic petrology, isotope chemistry, sedimentology and geophysics produced a wide-ranging archive of data-rich scientific papers. The rationale for this book is to provide a coherent overview of these datasets in addressing the evolution of the mountain ranges we see today. This volume comprises 21 specially invited review papers on the Himalaya, Kohistan arc, Tibet, the Karakoram and Pamir ranges. These papers span the history of Himalayan research, chronology of the collision, stratigraphy, magmatic and metamorphic processes, structural geology and tectonics, seismicity, geophysics, and the evolution of the Indian monsoon. This landmark set of papers should underpin the next 25 years of Himalayan research.
Published by the American Geophysical Union as part of the Geodynamics Series, Volume 3. The International Geodynamics Project focussed attention on processes within the earth responsible for the movement of the lithospheric blocks. At anyone time, strong tectonic activity appears limited to a few mobile belts. Most of the present-day seismic activity is confined to the Circum-Pacific belt, the Alpide belt and the mid-oceanic ridges. These belts include oceanic and continental rift systems, the island arcs and young folded mountains. Continent to continent collision of the Eurasian and the Indian plates is generally believed to be responsible for the origin of the Himalaya, the tectonics of this region and the neighbouring south and central Asia. To focus attention on geodynamic problems in this relatively much less known Alpine-Himalayan region bounded by Iran in the West and Burma in the East, the Inter-Union Commission on Geodynamics formed a separate Working Group 3b under the Chairmanship of Hari Narain. Later, in 1975, this Working Group 3b on "Geodynamics of the Alpine-Himalayan region, East" was given independant status and re-numbered as Working Group 6.
This volume is the outcome of about 30 years of research in the field of earthquake seismology in various parts of South Asia. It comprehensively deals with topics raning from plate tectonics to seismic waves in general. State-of-the-art techniques in earthquake location/relocation, fault plane solution, waveform inversion, seismic tomography, fractals etc. are discussed, and the results are interpreted in terms of seismic source processes in the region.
The Himalayan mountain belt, which developed during the India–Asia collision starting about 55 Ma ago, is a dramatically active orogen and it is regarded as the classic collisional orogen. It is characterized by an impressively continuous 2500 km of tectonic units, thrusts and normal faults, as well as large volumes of high-grade metamorphic rocks and granites exposed at the surface. This constitutes an invaluable field laboratory, where amazing crustal sections can be observed directly in very deep gorges. It is possible to unravel the tectonic and metamorphic evolution of litho-units, to observe the mechanisms of exhumation of deep-seated rocks and the propagation of the deformation. Himalayan tectonics has been the target of many studies from numerous international researchers over the years. In the last 15 years there has been an explosion of data and theories from both geological and geophysical perspectives. This book presents the results of integrated multidisciplinary studies, including geology, petrology, magmatism, geochemistry, geochronology and geophysics, of the structures and processes affecting the continental lithosphere. These processes and their spatial and temporal evolution have major consequences on the geometry and kinematics of the India–Eurasia collision zone.
Scientific evidence shows that most glaciers in South Asia's Hindu Kush Himalayan region are retreating, but the consequences for the region's water supply are unclear, this report finds. The Hindu Kush Himalayan region is the location of several of Asia's great river systems, which provide water for drinking, irrigation, and other uses for about 1.5 billion people. Recent studies show that at lower elevations, glacial retreat is unlikely to cause significant changes in water availability over the next several decades, but other factors, including groundwater depletion and increasing human water use, could have a greater impact. Higher elevation areas could experience altered water flow in some river basins if current rates of glacial retreat continue, but shifts in the location, intensity, and variability of rain and snow due to climate change will likely have a greater impact on regional water supplies. Himalayan Glaciers: Climate Change, Water Resources, and Water Security makes recommendations and sets guidelines for the future of climate change and water security in the Himalayan Region. This report emphasizes that social changes, such as changing patterns of water use and water management decisions, are likely to have at least as much of an impact on water demand as environmental factors do on water supply. Water scarcity will likely affect the rural and urban poor most severely, as these groups have the least capacity to move to new locations as needed. It is predicted that the region will become increasingly urbanized as cities expand to absorb migrants in search of economic opportunities. As living standards and populations rise, water use will likely increase-for example, as more people have diets rich in meat, more water will be needed for agricultural use. The effects of future climate change could further exacerbate water stress. Himalayan Glaciers: Climate Change, Water Resources, and Water Security explains that changes in the availability of water resources could play an increasing role in political tensions, especially if existing water management institutions do not better account for the social, economic, and ecological complexities of the region. To effectively respond to the effects of climate change, water management systems will need to take into account the social, economic, and ecological complexities of the region. This means it will be important to expand research and monitoring programs to gather more detailed, consistent, and accurate data on demographics, water supply, demand, and scarcity.
During the June 2020 territorial dispute over Kalapani, India blamed tensions on a newly assertive Nepal's deepening relations with China. But beyond the accusations and grandstanding, this reflects a new reality: the power equations in South Asia have been redrawn, to make space for China. Nepal did not turn northwards overnight. Its ties with China have deep historical roots built on Buddhism, dating to the early first millennium. While India's unofficial 2015 blockade provided momentum to the rift with Delhi, Nepal has long wanted deeper ties with Beijing, to counteract India's oppressive intimacy. With China's growing South Asian and global ambitions, Nepal now has a new primary bilateral partner-and Nepalis are forging a path towards modernity with its help, both in the remote borderlands and in the cities. All Roads Lead North offers a long view of Nepal's foreign relations, today underpinned by China's world-power status. Sharing never- before-told stories about Tibetan guerrilla fighters, failed coup leaders and trans- Himalayan traders, Nepal analyst Amish Raj Mulmi examines the histories binding mountain communities together across the Sino-Nepali border. Part history, part journalistic account, Mulmi's is a complex, compelling and rigorously researched study of a small country caught between two neighbourhood giants.
The graphic story of the measurement of a meridian, or longitudinal, arc extending from the tip of the Indian subcontinent to the mountains of the Himalayas.
"Spanning eight kilometers of topographic relief, the Himalayan fold-thrust belt in Nepal has accommodated more than 700 km of Cenozoic convergence between the Indian subcontinent and Asia. Rapid tectonic shortening and erosion in a monsoonal climate have exhumed greenschist to upper amphibolite facies rocks along with unmetamorphosed rocks, including a 5-6-km-thick Cenozoic foreland basin sequence. This Special Paper presents new geochronology, multisystem thermochronology, structural geology, and geological mapping of an approximately 37,000 km2 region in midwestern and western Nepal. This work informs enduring Himalayan debates, including how and where to map the Main Central thrust, the geometry of the seismically active basal Himalayan detachment, processes of tectonic shortening in the context of postcollisional India-Asia convergence, and long-term geodynamics of the orogenic wedge"--Publisher's website