Operation China

Total Page:16

File Type:pdf, Size:1020Kb

Operation China Dongxiang March 10 Mongolian spoken in the INNER MONGOLIA thirteenth and fourteenth 3 GANSU centuries.” Only 12% of the Dongxiang are literate in •Xining •Lanzhou QINGHAI Luqu•Jone Chinese. • •Min Xian Scale SICHUAN History: In the thirteenth 0 KM 400 century China was subdued Population in China: by the Mongols. Genghis 373,872 (1990) Khan, in a bid to control the 482,300 (2000) 622,100 (2010) land he had taken over, Location: Gansu, Qinghai, moved some of his Xinjiang, Ningxia garrisons into China. These Religion: Islam Christians: None Known soldiers intermarried with local women and gradually Overview of the developed into their own distinct ethnic group called Dongxiang 4 Countries: China the Dongxiang. Some place- Pronunciation: “Dong-shee-ung” names seem to support this Other Names: Tunghsiang, Santa, theory. For example, Tung, Mongolian Huihui Zhayingtan (Encampment Population Source: Beach), is said to be the 373,872 (1990 census); site of an old Dongxiang 279,397 (1982 census); 5 147,443 (1964 census); garrison. 155,761 (1953 census) Location: SW Gansu: Two-thirds Customs: The Dongxiang are of Dongxiang live in Dongxiang Dwayne Graybill primarily employed as County in the Linxia Hui Prefecture. Smaller numbers live Location: The majority of the more than farmers. Their main crops are potatoes, in Hezheng County and Linxia city; 480,000 Dongxiang live in one long, barley, millet, wheat, and corn. They are a few live in Lanzhou City and spread-out valley in the southwestern part also renowned across China for producing Dingxi District. A few Dongxiang also live in Qinghai, Xinjiang, and of Gansu Province. The Dongxiang region is traditional rugs. Ningxia. a desolate, arid place with a moon-like Status: landscape, even though it is bordered by Religion: Not long after the Dongxiang first An official minority of China the Tao River to the east, the Daxia River to arrived in China, they were converted to Language: Altaic, Mongolian, Eastern Mongolian, Mongour the west, and the Yellow River to the north. Islam. By 1949, when the Communists took Literacy: 12% Approximately 55,000 Dongxiang also live over China, there was one mosque for Dialects (3): in the Ili Prefecture in Xinjiang and in parts every 30 Dongxiang homes and one paid 1 6 Suobana, Wangjiaji, Sijiaji of Qinghai and Ningxia. Muslim worker for every nine families. Religion: Islam Sixty to seventy percent of Dongxiang Christians: None known Identity: The Dongxiang are one of China’s belong to the Old Sect, which emphasizes Scripture: None official minority groups. They were called worshiping at the tombs of Muslim saints. Jesus film: None Mongolian Huihui prior to 1949, when their “The remainder belong to the New Sect, a 7 Gospel Recordings: name was changed to the Dongxiang (East fundamentalist and reformist group.” There Dongxiang #04866 District) people. They call themselves by the were numerous brutal wars between the Christian Broadcasting: None Islamic term Santa. Other Muslims in China two Dongxiang sects in the last century. ROPAL code: SCE00 do not consider the Dongxiang to be a part Status of Evangelization of the Islamic faith because of their Christianity: There has never been a single 96% involvement in drug and prostitution known church or Christian among the rackets. One visitor to the Dongxiang Dongxiang. In the 1940s some described them as “very mean people, with missionaries briefly visited the Dongxiang hard faces.”2 area but were unsuccessful in converting anyone to Christ. In 1993 a Hong Kong- 4% 0% Language: The Dongxiang speak a based organization conducted mass Mongolian language. “Quite a few words in literature evangelism in the main Dongxiang A B C the Dongxiang lexicon resemble words of town.8 The nearest church to the Dongxiang A = Have never heard the gospel the same meaning in Modern Mongolian, is a Han Chinese fellowship in Linxia. The B = Were evangelized but did not become Christians and some are even identical to words Christians there, however, believe “it is C = Are adherents to any form of presently used in Inner Mongolia. Many impossible to reach the Dongxiang.”9 Christianity other words are close to the Middle DONGXIANG 127.
Recommended publications
  • Polycyclic Aromatic Hydrocarbons in the Estuaries of Two Rivers of the Sea of Japan
    International Journal of Environmental Research and Public Health Article Polycyclic Aromatic Hydrocarbons in the Estuaries of Two Rivers of the Sea of Japan Tatiana Chizhova 1,*, Yuliya Koudryashova 1, Natalia Prokuda 2, Pavel Tishchenko 1 and Kazuichi Hayakawa 3 1 V.I.Il’ichev Pacific Oceanological Institute FEB RAS, 43 Baltiyskaya Str., Vladivostok 690041, Russia; [email protected] (Y.K.); [email protected] (P.T.) 2 Institute of Chemistry FEB RAS, 159 Prospect 100-let Vladivostoku, Vladivostok 690022, Russia; [email protected] 3 Institute of Nature and Environmental Technology, Kanazawa University, Kakuma, Kanazawa 920-1192, Japan; [email protected] * Correspondence: [email protected]; Tel.: +7-914-332-40-50 Received: 11 June 2020; Accepted: 16 August 2020; Published: 19 August 2020 Abstract: The seasonal polycyclic aromatic hydrocarbon (PAH) variability was studied in the estuaries of the Partizanskaya River and the Tumen River, the largest transboundary river of the Sea of Japan. The PAH levels were generally low over the year; however, the PAH concentrations increased according to one of two seasonal trends, which were either an increase in PAHs during the cold period, influenced by heating, or a PAH enrichment during the wet period due to higher run-off inputs. The major PAH source was the combustion of fossil fuels and biomass, but a minor input of petrogenic PAHs in some seasons was observed. Higher PAH concentrations were observed in fresh and brackish water compared to the saline waters in the Tumen River estuary, while the PAH concentrations in both types of water were similar in the Partizanskaya River estuary, suggesting different pathways of PAH input into the estuaries.
    [Show full text]
  • Ancient Genomes Reveal Tropical Bovid Species in the Tibetan Plateau Contributed to the Prevalence of Hunting Game Until the Late Neolithic
    Ancient genomes reveal tropical bovid species in the Tibetan Plateau contributed to the prevalence of hunting game until the late Neolithic Ningbo Chena,b,1, Lele Renc,1, Linyao Dud,1, Jiawen Houb,1, Victoria E. Mulline, Duo Wud, Xueye Zhaof, Chunmei Lia,g, Jiahui Huanga,h, Xuebin Qia,g, Marco Rosario Capodiferroi, Alessandro Achillii, Chuzhao Leib, Fahu Chenj, Bing Sua,g,2, Guanghui Dongd,j,2, and Xiaoming Zhanga,g,2 aState Key Laboratory of Genetic Resources and Evolution, Kunming Institute of Zoology, Chinese Academy of Sciences (CAS), 650223 Kunming, China; bKey Laboratory of Animal Genetics, Breeding and Reproduction of Shaanxi Province, College of Animal Science and Technology, Northwest A&F University, 712100 Yangling, China; cSchool of History and Culture, Lanzhou University, 730000 Lanzhou, China; dCollege of Earth and Environmental Sciences, Lanzhou University, 730000 Lanzhou, China; eDepartment of Earth Sciences, Natural History Museum, London SW7 5BD, United Kingdom; fGansu Provincial Institute of Cultural Relics and Archaeology, 730000 Lanzhou, China; gCenter for Excellence in Animal Evolution and Genetics, Chinese Academy of Sciences, 650223 Kunming, China; hKunming College of Life Science, University of Chinese Academy of Sciences, 100049 Beijing, China; iDipartimento di Biologia e Biotecnologie “L. Spallanzani,” Università di Pavia, 27100 Pavia, Italy; and jCAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 100101 Beijing, China Edited by Zhonghe Zhou, Chinese Academy of Sciences, Beijing, China, and approved September 11, 2020 (received for review June 7, 2020) Local wild bovids have been determined to be important prey on and 3,000 m a.s.l.
    [Show full text]
  • 9781107069879 Index.Pdf
    Cambridge University Press 978-1-107-06987-9 — The Qing Empire and the Opium War Mao Haijian , Translated by Joseph Lawson , Peter Lavelle , Craig Smith , Introduction by Julia Lovell Index More Information Index 18th Regiment , 286 , 306 35 – 37 , 45 , 119 – 21 , 122 , 209 ; coastal , 34 , 26th Regiment , 205 , 242 , 286 35 – 36 , 38 , 115 ; concealed , 208 ; early- 37th Regiment , 257 warning , 199 ; fortii ed , vi , 36 , 121 , 209 , 37th Regiment of Madras Native Infantry , 206 218 – 20 , 281 , 493 ; sand- bagged , 210 , 218 , 49th Regiment , 205 , 286 232 , 309 55th Regiment , 286 , 306 Battle at Dinghai, showing the British attacks, 98th Regiment , 384 Qing defensive positions, and the walled town of Dinghai , 305 Ackbar , 385 Battle at Guangzhou, showing British Aigun , 500 attacks , 241 American citizens , 452 , 456 – 58 , 460 , 462 , Battle at Humen, showing the British attacks 463 – 64 , 465 – 68 , 475 , 478 , 511 , 513 and Qing defensive positions , 198 American envoys , 458 – 59 , 461 Battle at Wusong, showing British attacks and American merchants , 96 , 97 – 99 , 152 , 218 , Qing defensive positions , 380 227 , 455 – 57 , 503 Battle at Xiamen, showing main British American ships , 103 , 456 – 57 , 467 attacks and Qing defensive positions , 287 American treaties , 478 Battle at Zhapu, showing Qing defensive Amoy , 427 , 452 positions and British attacks , 376 Anhui , 50 – 51 , 88 , 111 , 163 – 64 , 178 , 324 , 328 , Battle at Zhenhai, showing the Qing defensive 331 , 353 – 54 , 358 positions and British attacks , 311 Ansei
    [Show full text]
  • The Later Han Empire (25-220CE) & Its Northwestern Frontier
    University of Pennsylvania ScholarlyCommons Publicly Accessible Penn Dissertations 2012 Dynamics of Disintegration: The Later Han Empire (25-220CE) & Its Northwestern Frontier Wai Kit Wicky Tse University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/edissertations Part of the Asian History Commons, Asian Studies Commons, and the Military History Commons Recommended Citation Tse, Wai Kit Wicky, "Dynamics of Disintegration: The Later Han Empire (25-220CE) & Its Northwestern Frontier" (2012). Publicly Accessible Penn Dissertations. 589. https://repository.upenn.edu/edissertations/589 This paper is posted at ScholarlyCommons. https://repository.upenn.edu/edissertations/589 For more information, please contact [email protected]. Dynamics of Disintegration: The Later Han Empire (25-220CE) & Its Northwestern Frontier Abstract As a frontier region of the Qin-Han (221BCE-220CE) empire, the northwest was a new territory to the Chinese realm. Until the Later Han (25-220CE) times, some portions of the northwestern region had only been part of imperial soil for one hundred years. Its coalescence into the Chinese empire was a product of long-term expansion and conquest, which arguably defined the egionr 's military nature. Furthermore, in the harsh natural environment of the region, only tough people could survive, and unsurprisingly, the region fostered vigorous warriors. Mixed culture and multi-ethnicity featured prominently in this highly militarized frontier society, which contrasted sharply with the imperial center that promoted unified cultural values and stood in the way of a greater degree of transregional integration. As this project shows, it was the northwesterners who went through a process of political peripheralization during the Later Han times played a harbinger role of the disintegration of the empire and eventually led to the breakdown of the early imperial system in Chinese history.
    [Show full text]
  • Applied Ecology and Environmental Research 17(6):13341-13354
    Wang et al.: Study on ecological risk assessment of different land use types based on HMER model – taking the Daxia River in Gansu, China as an example - 13341 - STUDY ON ECOLOGICAL RISK ASSESSMENT OF DIFFERENT LAND USE TYPES BASED ON HMER MODEL – TAKING THE DAXIA RIVER IN GANSU, CHINA AS AN EXAMPLE WANG, S. – ZHANG, C.* – JI, H. – ZHANG, Y. – LOU, T. College of Computer Science & Engineering, Northwest Normal University, Lanzhou 730070, China *Corresponding author e-mail: [email protected] (Received 10th Jun 2019; accepted 28th Aug 2019) Abstract. The effective heavy metal content of soil indicates ecological environmental risks. The study takes the typical watershed area in northwestern China as a research area. The real-time and rapid risk assessment of ecological environment can be achieved through the monitoring value of normalized difference vegetation index (NDVI) of remote sensing information and environmental factors, and a heavy metal ecological risk assessment model (HMER) for the evaluation of the watershed is built. The research results show that the change of the effective heavy metal content in different areas of the watershed is affected to some extent by the influence of geographical location and human activities. Among them NDVI and the content of heavy metals, precipitation and temperature, and a nonlinear relationship between the average heavy metal content and the ecological risk index HRI. The establishment of HMER research model is applied to different land use types to evaluate the ecological risk level of the watershed, explore the ecological risk level of different land use types in the same region, and in different regions.
    [Show full text]
  • Irrigation in Southern and Eastern Asia in Figures AQUASTAT Survey – 2011
    37 Irrigation in Southern and Eastern Asia in figures AQUASTAT Survey – 2011 FAO WATER Irrigation in Southern REPORTS and Eastern Asia in figures AQUASTAT Survey – 2011 37 Edited by Karen FRENKEN FAO Land and Water Division FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2012 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views of FAO. ISBN 978-92-5-107282-0 All rights reserved. FAO encourages reproduction and dissemination of material in this information product. Non-commercial uses will be authorized free of charge, upon request. Reproduction for resale or other commercial purposes, including educational purposes, may incur fees. Applications for permission to reproduce or disseminate FAO copyright materials, and all queries concerning rights and licences, should be addressed by e-mail to [email protected] or to the Chief, Publishing Policy and Support Branch, Office of Knowledge Exchange, Research and Extension, FAO, Viale delle Terme di Caracalla, 00153 Rome, Italy.
    [Show full text]
  • The Capacity of the Hydrological Modeling for Water Resource Assessment Under the Changing Environment in Semi-Arid River Basins in China
    water Article The Capacity of the Hydrological Modeling for Water Resource Assessment under the Changing Environment in Semi-Arid River Basins in China Xiaoxiang Guan 1,2, Jianyun Zhang 1,2,3,*, Amgad Elmahdi 4 , Xuemei Li 5, Jing Liu 2,3, Yue Liu 1,2, Junliang Jin 2,3, Yanli Liu 2,3 , Zhenxin Bao 2,3, Cuishan Liu 2,3, Ruimin He 2,3 and Guoqing Wang 1,2,3,6,* 1 Institute of Hydrology and Water Resources, Hohai University, Nanjing 210098, China 2 Research Center for Climate Change, Ministry of Water Resources, Nanjing 210029, China 3 State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China 4 International Water Management Institute-IWMI, Head of MENA Region, 3000 Cairo, Egypt 5 Hydrology Bureau, Yellow River Conservancy Commission, Ministry of Water Resources, Zhengzhou 450003, China 6 School of Resources and Environment, University of Electronic Science and Technology of China, Chengdu 611731, China * Correspondence: [email protected] (J.Z.); [email protected] (G.W.); Tel.: +86-25-85828007 (J.Z.); +86-25-8582-8531 (G.W.) Received: 6 May 2019; Accepted: 24 June 2019; Published: 27 June 2019 Abstract: Conducting water resource assessment and forecasting at a basin scale requires effective and accurate simulation of the hydrological process. However, intensive, complex human activities and environmental changes are constraining and challenging the hydrological modeling development and application by complicating the hydrological cycle within its local contexts. Six sub-catchments of the Yellow River basin, the second-largest river in China, situated in a semi-arid climate zone, have been selected for this study, considering hydrological processes under a natural period (before 1970) and under intensive human disturbance (2000–2013).
    [Show full text]
  • A Tale of 3 Provinces I Sichuan, Qinghai & Gansu Plus a Taste Of
    A Tale of 3 Provinces I Sichuan, Qinghai & Gansu plus a taste of Xian 27June – 09July 2016 In this natural wonder getaway, where you can witness condors gliding across blue skies, explore nomad lifestyle, relax with a sip of milk tea and enjoy the stunning prairie sunset or sunrise. This is a place of magic, the home of yak, the world of wild flowers and the ocean of green grass. Here, the land is flat and the views are extensive; the pasture is lush and the cattle and sheep flocks ….. join us to this off the beaten track enchanting journey to capture these Tale of 3 Provinces , where the boundary beauties are endless . DAY 01 , 27 JUNE Monday : KUALA LUMPUR – CHENGDU ( MOB ) Depart Kuala Lumpur for Chengdu on Air Asia flight D7 326 KUL 1815 CTU 2240 Upon Arrival Chengdu Airport, meet and greet by our local English Guide and transfer to check in a hotel near to the airport. Overnite in Chengdu , 3* Hotel near to the airport Day 02, 28 JUNE Tuesday : CHENGDU – EMUTANG PASTURE – HONGYUAN ( B/L/D) Wake up early to start our journey to Hongyuan. The spectacular Hongyuan (red plain) Grasslands was so named because the Red Army, over the course of a year, passed through here during the famous Long March in 1936. A plateau at over 3,000m (9843 feet) above sea level , stretching for over 8,400 sq.km., the Hongyuan Grasslands is said to be home to over 300,000 herded yak, 20m herded sheep and over 20,000 horses and many wild flowers in early summer.
    [Show full text]
  • List of Project Activities Completed and in Process (2019.05.08) Validation Projects
    List of project activities completed and in process (2019.05.08) Validation projects Serial Project Title Project Status UNFCCC Ref No. No. 1. Yunnan Luxi Donghua Wind Power Project Registered 6147 2. Yunnan Luxi Dongshan Wind Power Project Registered 6146 3. Henan Province Ye County Matoushan Wind Power Plant Registered 5819 4. Hainan Lingao Solar Project Registered 6145 5. Huadian Zhoushan Xiaosha 30MW Wind Farm Project Registered 5116 6. Xinjiang Dabancheng Phase I Wind Farm Project of Tianshan Electric Power Co., Registered 4651 Ltd 7. Ningxia Qingtongxia Jinggou Grid-connected Solar PV Power Generation Project Registered 5114 8. Shaanxi Jingbian 20MW Grid-connected Photovoltaic Power Generation Project Registered 4517 9. Xiangtan Jiuhua Photovoltaic Power Generation Project Registered 8116 10. Ningxia Zhongwei 30MW grid-connected photovoltaic power generation Project Registered 4647 11. Fuan Hydropower Station Registered 7050 12. Three Gorges New Energy Geermu Power Generation CO., Ltd. Geermu 10MW Registered 6017 Grid-connected Photovoltaic Power Generation Project 13. Sichuan Luding Feishuigou 8MW Hydropower Project Registered 5111 14. Sichuan Songpan Daxing Hydropower Project Registered 8313 15. Gansu Yongchang Shuiquanzi Wind Farm Project Registered 7286 16. Gansu Jinchang Xitan Wind Farm Project Registered 7288 17. SanxiaNewEnergyKaiyuanWeiyuanWindFarmProject Registered 8206 18. Guiyang MRTS LineI Project Registered 8149 1 / 13 19. Jin River Cascade II Hydropower Project in Mabian Yi Autonomous County Registered 7865 20. GD Power Taishan Ziluoshan Wind Power Project Registered 8328 21. GD Power Dongyuan Chanziding Wind Power Project Registered 8326 22. Xinjiang Jingou River Six-level Hydropower Project Registered 9867 23. Xinjiang Ili Kukesu River Halajun Hydropower Project Registered 9891 24. Inner Mongolia Shangdi Wind-farm Project Registered 9968 25.
    [Show full text]
  • Biking in Western China
    Biking in Western China - Bicycle tour on the banks of Qinghai Lake - Gain an insight into local Tibetan families’ way of life, their customs and culture - Explore the Tibetan Plateau and its small villages, temples and monasteries - Visit Bird Island: an excellent spot for bird-watching Mountain Biking Tour Qinghai – Tibetan Plateau WEST CHINA MOUNTAIN BIKE TOUR This tour will lead you from the capital of Sichuan province - Chengdu - to one of the world’s highest altitude peat lands and to Qinghai Lake; an important sanctuary for thousands of migrant birds and is specially designed for people, who want to explore this beautiful region by bicycle. Best travel date: all year round; best months: June, July and August (this trip is not available from 14th July to 22nd July because of road restrictions during the Tour of Qinghai Lake International Road Cycling Race) Destinations: Chengdu, Tangke, Xiaman, Heihe, Langmu Monastery, Xiahe, Xining, Xihai, Gangcha, Bird Island, Heimahe Duration: 13 days Starting in: Chengdu Ending in: Beijing/Chengdu Group size: min. 6 pax, max. 12 pax QUICK INTRODUCTION Ruoergai (Roige) Grassland: The Ruoergai Marshes are located in the provinces of Sichuan and Gansu in the upper “Huanghe” Yellow River basin on the eastern edge of the Tibetan Plateau. At an altitude of 3400m to 3900m, they are one of the world’s highest altitude peat lands and consist of approximately 10’000 km² of peat bogs, sedge marshes, lakes and wet grasslands, interspersed with low hills and drier grasslands, which are inhabited by Tibetan people, who are almost exclusively pastoralists with vast herds of horses, sheep, yaks and goats.
    [Show full text]
  • Source of Oligocene to Pliocene Sedimentary Rocks in the Linxia Basin in Northeastern Tibet from Nd Isotopes: Implications for Tectonic Forcing of Climate
    Source of Oligocene to Pliocene sedimentary rocks in the Linxia basin in northeastern Tibet from Nd isotopes: Implications for tectonic forcing of climate Carmala N. Garzione† Department of Earth and Environmental Sciences, University of Rochester, Rochester, New York 14627, USA, and Department of Geological Sciences and Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, Colorado 80309, USA Matt J. Ikari Asish R. Basu Department of Earth and Environmental Sciences, University of Rochester, Rochester, New York 14627, USA ABSTRACT generate the εNd values observed in Linxia tion of the plateau margin was responsible for basin sedimentary rocks through mixing of the middle Miocene climate change observed We used Nd isotopes and trace element plutonic and metasedimentary sources. in the Linxia basin. data to determine the provenance of sedi- Rare earth element patterns suggest that mentary rocks in the Linxia basin, northeast- Cretaceous rocks were not a dominant Keywords: Nd isotopes, sedimentary prov- ern Tibet, whose Oligocene through Pliocene source of sediment. The Nd isotopic composi- enance, loess, Tibetan Plateau, paleoclimate, sedimentation history has been interpreted to tion and rare earth element pattern of Qua- unroofi ng. refl ect deposition in a fl exural basin associ- ternary loess are similar to older deposits in ated with contractional deformation along the Linxia basin and refl ect loess deposited INTRODUCTION the northeastern margin of the Tibetan elsewhere in the Loess plateau and the North Plateau. Paleozoic–early Mesozoic metasedi- Pacifi c (εNd = −8.6 to –10.5). In addition, the The unroofi ng histories of the margins of the mentary source rocks from the Kunlun- modern Daxia River, which drains the mar- Tibetan Plateau provide insight into the timing Qaidam and Songpan-Ganzi terranes have gin of the plateau today, transports clay and and mechanisms of outward growth of the pla- εNd values between −11.8 and −16.1, whereas silt with εNd values of –10.5 to –10.8 despite teau.
    [Show full text]
  • Tibetan Silk Appliqué Thangka: Every Stitch Is a Prayer
    Tibetan silk appliqué thangka: every stitch is a prayer Manjushri, Bodhisattva of Wisdom. Detail of silk appliqué thangka, 2009. Private collection i Tibetan silk appliqué thangka This thesis is submitted in fulfilment of the degree of Master of Arts of the Australian National University, Canberra Submitted by Edith A. Young August 2010 I certify that this thesis is my own work and that all sources have been acknowledged. Copyright © by Edith Young. All rights reserved. No part of this thesis may be reproduced in any form or by any means, electronic, photocopy, information retrieval system, or otherwise without permission from the author. ii Acknowledgements I would like to acknowledge those who have assisted me in the work for this thesis. This thesis would not have been possible without assistance from Bhiksuni Karma Palmo and Bhiksuni Karma Lhadron, who helped me from the very beginning to find artists and contacts in Dharamsala and Kathmandu and provided unfailing encouragement and support throughout. It is thanks to the kindness of the artists and lamas who spoke to me at length of their work, their motivation and their efforts in this revival that I have been able to make this contribution to this area of Tibetan art. I have been humbled and motivated by their dedication and the strength of their commitment to sustaining and reviving this artistic tradition. These artists include Terris Temple and Leslie Ngyuen Temple, who warmly welcomed me in Chiang Mai and shared their stories, and Leslie Rinchen Wongmo who has also encouraged and helped me. I am grateful for the assistance I received from the Office of His Holiness the Fourteenth Dalai Lama in Canberra, and I would also like to acknowledge the help of Tenzin Nyimalha, Palden Lama and Tenzin Ringpaponsang, who acted as my translators.
    [Show full text]