“Guns Plus Interest”

2019 ◽  
pp. 64-96
Author(s):  
Yelena Biberman

This chapter shows that the principal factors driving the state-nonstate alliances in Kashmir (1989–2003) were the local balance of power and actors’ interests. It was only when the Indian army demonstrated force employment prowess through a string of military victories that it was able to attract opportunists. These were former rebels seeking local power, profit, and security. The proxies—most notably the Ikhwan-ul-Muslimoon in the north, as well as the Jammu and Kashmir Ikhwan and Muslim Mujahideen in the south of the Kashmir Valley—helped to shift the balance of power in India’s favor. This prompted the insurgency to move to the mountainous Jammu region. There, the security forces turned to local activists. These, mostly Hindu, villagers formed the so-called Village Defense Committees.

Author(s):  
Stephen Westcott

The Indo-Pacific region stretches from Japan in the north to Pakistan in the west to Australia in the south and the Micronesian islands in the east. When the various colonial empires withdrew from the region, they left numerous volatile interstate border disputes (IBDs) in their wake. With the balance of power shifting away from the Northern Atlantic and into the Indo-Pacific, the IBDs in the region are gaining more salience. Yet, within academic and public circles, the IBDs in the region have often been overshadowed by discussions over the military balance of power, nuclear brinkmanship, and political economy concerns such as trade route flows or resource competition. While these are unquestionably important issues, this focus on “high politics” tends to trivialize IBDs. This is problematic because, as numerous studies have demonstrated, IBDs have proven to be a leading cause of war and a primary source of international tension during peace. Indeed, many of the IBDs in the Indo-Pacific region are right at the center of the often-volatile region, fueled in part by a growing sense of nationalism within the region, by regional rivalries, and by the competition for strategic resources. Hence, developing a strong understanding of the IBDs that are, if not at the foundation of, the flint and tinder for international conflict is important. In the Indo-Pacific region, there are a number of highly diverse IBDs, ranging in size, salience, and type (territory and maritime). Some of these IBDs are major sources of tension in the region, such as the five-nation claim over the South China Sea at the heart of the Indo-Pacific or the notably bitter and fractious dispute between India and Pakistan over Jammu and Kashmir. The Indo-Pacific region also hosts some of the few remaining divided nations, namely, China’s claim of sovereignty over Taiwan and the two Koreas’ claims over each other. Others are relatively minor IBDs, such as Japan’s dispute with Korea over the Takeshima/Dokdo Island, which sees occasional demonstrations but otherwise has little impact on the two states’ bilateral relations. In between, there exist an array of IBDs of varying importance, ranging from the Sino-Indian border dispute, which often causes tension between the region’s rising nuclear armed superpowers, to the Thai-Cambodian dispute over the Preah Vihear temple complex, to the grossly under-researched Durand Line dispute between Afghanistan and Pakistan. This contribution to Oxford Bibliographies takes stock of the burgeoning literature on all of these issues.


Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.


2007 ◽  
Vol 66 (4) ◽  
pp. 303-321
Author(s):  
Lode Wils

In het tweede deel van zijn bijdrage 1830: van de Belgische protonatie naar de natiestaat, over de gebeurtenissen van 1830-1831 als slotfase van een passage van de Belgische protonatie doorheen de grote politiek-maatschappelijke en culturele mutaties na de Franse Revolutie, ontwikkelt Lode Wils de stelling dat de periode 1829-1830 de "terminale crisis" vormde van het Koninkrijk der Verenigde Nederlanden. Terwijl koning Willem I definitief had laten verstaan dat hij de ministeriële verantwoordelijkheid definitief afwees en elke kritiek op het regime beschouwde als kritiek op de dynastie, groeide in het Zuiden de synergie in het verzet tussen klerikalen, liberalen en radicale anti-autoritaire groepen. In de vervreemding tussen het Noorden en het Zuiden en de uiteindelijke revolutionaire nationaal-liberale oppositie vanuit het Zuiden, speelde de taalproblematiek een minder belangrijke rol dan het klerikale element en de liberale aversie tegen het vorstelijk absolutisme van Willem I en de aangevoelde uitsluiting van de Belgen uit het openbaar ambt en vooral uit de leiding van de staat.________1830: from the Belgian pre-nation to the nation stateIn the second part of his contribution 1830: from the Belgian pre-nation to the nation state, dealing with the events from 1830-1831 as the concluding phase of a transition of the Belgian pre-nation through the major socio-political and cultural mutations after the French Revolution, Lode Wils develops the thesis that the period of 1829-1830 constituted the "terminal crisis" of the Kingdom of the United Netherlands. Whilst King William I had clearly given to understand that he definitively rejected ministerial responsibility and that he considered any criticism of the regime as a criticism of the dynasty, the synergy of resistance increased between the clericalists, liberals and radical anti-authoritarian groups in the South. In the alienation between the North and the South and the ultimate revolutionary national-liberal opposition from the South the language issue played a less important role than the clericalist element and the liberal aversion against the royal absolutism of William I and the sense of exclusion of the Belgians from public office and particularly from the government of the state.


2021 ◽  
Vol 7 (20) ◽  
pp. 202106
Author(s):  
Marcelo Cervo Chelotti ◽  
Rosa Maria Vieira Medeiros

CARTOGRAPHS OF VITICULTURE IN MINAS GERAIS: from South genesis to North expansionCARTOGRAFÍAS DE LA VITICULTURA EN MINAS GERAIS: de la génesis en el Sur a la expansión al NorteRESUMOO presente artigo tem como objetivo analisar a reorientação no deslocamento do padrão espacial do cultivo de uvas no estado de Minas Gerais, originalmente localizado no Sul, mas expandiu-se para o norte mineiro nas últimas décadas. Os procedimentos metodológicos centraram-se na revisão de literatura sobre a viticultura no Brasil, e na coleta em dados secundários na Pesquisa Agrícola Municipal/PAM/IBGE, nos Censos Agropecuários do IBGE, além do Banco de Dados de Uva, Vinho e Derivados/VITIBRASIL. Os mapas temáticos demonstraram a dinâmica da viticultura em Minas Gerais, evidenciando uma mudança no padrão espacial, ou seja, historicamente concentrada no sul do estado, mas verificamos no pós-1990 uma expansão geográfica para o norte, principalmente em direção ao Cerrado e vale do Rio São Francisco. O papel desempenhado pela pesquisa, na busca de novas técnicas para a viticultura em regiões tropicais, tem uma grande centralidade nesse processo, uma vez que estamos diante de um novo paradigma para a produção de uvas e vinhos.Palavras-chave: Viticultura; Regionalização; Geografia do Vinho; Minas Gerais.ABSTRACTThis article has the goal to analyze the reorientation in the displacement of the spatial pattern of grape cultivation in the state of Minas Gerais, originally located in the south, but has expanded to the north of Minas Gerais in recent decades. The methodological procedures focused on the literature review on viticulture in Brazil, and the collection of secondary data from the Municipal Agricultural Research/PAM/IBGE, the IBGE Agricultural Census, and the Grape, Wine and Derivatives Database/VITIBRASIL. Thematic maps showed the dynamics of viticulture in Minas Gerais, showing a change in the spatial pattern, that is, historically concentrated in the south of the state. Sao Francisco River. The role played by the research in the search for new techniques for viticulture in tropical regions has a great centrality in this process, since we are facing a new paradigm for the production of grapes and wines.Keywords: Viticulture; Regionalization; Wine Geography; Minas Gerais.RESUMENEl presente artículo tiene como objetivo analizar la reorientación en el desplazamiento del patrón espacial del cultivo de la uva en el estado de Minas Gerais, originalmente ubicado en el sur, pero se ha expandido al norte de Minas Gerais en las últimas décadas. Los procedimientos metodológicos se centraron en la revisión de la literatura sobre viticultura en Brasil, y en la recopilación de datos secundarios en la Investigación Agrícola Municipal/PAM/IBGE, en los Censos Agrícolas del IBGE, además de la Base de Datos de Uva, Vino y Derivados/VITIBRASIL. Los mapas temáticos demostraron la dinámica de la viticultura en Minas Gerais, mostrando un cambio en el patrón espacial, es decir, históricamente concentrado en el sur del estado, pero en la década de 1990 verificamos una expansión geográfica hacia el norte, principalmente hacia el Cerrado y Vale do Río São Francisco El papel desempeñado por la investigación, en la búsqueda de nuevas técnicas para la viticultura en las regiones tropicales, tiene una gran centralidad en este proceso, ya que nos enfrentamos a un nuevo paradigma para la producción de uvas y vinos.Palabras-clave: Viticultura; Regionalización; Geografía del Vino; Minas Gerais.


The chief circumstance that induced Capt. Flinders to think his observations Upon the marine barometer were worthy of attention, was the coincidence that took place between the rising and falling of the mercury, and the setting in of winds that blew from the sea and from off the land, to which there seemed to be at least as much reference as to the strength of the wind or the state of the atmosphere. Our author’s examination of the coasts of New Holland and the other parts of the Terra Australis, began at Cape Leuwen, and con­tinued eastward along the south coast. His observations, which, on account of their length, we must pass over, show, that a change of wind from the northern half of the compass to any point in the southern half, caused the mercury to rise; and that a contrary change caused it to fall. Also, that the mercury stood considerably higher When the wind came from the south side of east and west, than when, in similar weather, it came from the north side.


Focaal ◽  
2019 ◽  
Vol 2019 (83) ◽  
pp. 25-36 ◽  
Author(s):  
Giovanni Orlando

Since the global crisis of 2008, Italy has witnessed several recoveries of failed private enterprises led by workers trying to escape the precarization of life under austerity. Some see this phenomenon as linked to the highly politicized occupations that took place in Argentina during the crisis of 2001. Italian recoveries, however, are usually far less controversial affairs carried out under the aegis of the state. What explains this difference? Looking at exceptions within the Italian case provides some answers. For example, a protracted conflict between workers (labor) and ownership (capital), the building of links with transnational struggles (including the Argentinian one), and the rediscovery of past working-class values such as mutualism all appear to be factors that can generate collective responses to austerity.


1955 ◽  
Vol 11 (3) ◽  
pp. 429-447
Author(s):  
Joaquín Meade

The huasteca region in northeastern Mexico covers sections of the six states of Tamaulipas, Veracruz, San Luis Potosí, Hidalgo, Puebla, and Querétaro. Its boundaries are approximately the following: to the north the river Soto la Marina, known in the sixteenth century as the Rio de las Palmas; to the south the Rio Cazones; to the east the Gulf of Mexico and to the west the mountainous section of the eastern Sierra Madre.The Christian conversion of the Huasteca began, no doubt, in 1518 with the expedition of Juan de Grijalva, who actually sailed as far north as Tuxpan and Tamiahua in the Huastec region of the state of Veracruz. John Diaz, a priest, accompanied this expedition. In 1519 Francisco de Garay, then in Jamaica, sent Alonso Alvarez de Pineda to Tampico and the Río Panuco, where he stayed some time and made contact with the Huastecs who belong to the great Maya family.


Seismologists have often noted the appearance of pronounced microseisms in seismic records when the weather has been disturbed over a neighbouring sea. For instance, the late Dr. KLOTZ suggested a relationship between disturbed weather in the north Atlantic and the largest microseismic movements at Ottawa. Dr. HARRISON, writing in ' Nature,’ November 1, 1924, in continuation of a note* by the present writer, pointed out that well-marked microseisms in the Omori charts at Calcutta invariably confirmed other evidence in the case of the early stages of dangerous cyclones, and were sometimes noticed when the storm centre was so much as 1000 miles south of Calcutta. He did not, however, recall any instance in which microseisms were associated with ordinary rough weather or with an advance of the monsoon. On the other hand, “ investigation at Eskdalemuir of the possible connection between microseismical amplitude and the state of the sea at different points of the British coasts have yielded results of an inconclusive kind. For example, the correlation between the state of the sea and the Microseismic movements of a type, which were quite characteristic of the south-west monsoon period, made their first appearance in the seismograms generally in May with the advance of the monsoon in the south-east Arabian Sea, becoming more and more pronounced as the monsoon currents approached Bombay. They became less marked or disappeared during a temporary break in the monsoon and reappeared with the strengthening of the currents. They were more or less steady vibrations having periods ranging from 4 to 10 seconds.


2014 ◽  
Vol 7 (2) ◽  
pp. 143-193 ◽  
Author(s):  
Alexander Ilin-Tomich

This paper focuses on the emergence of the Theban kingdom of Dynasty 16 in the Second Intermediate Period and explores the historical repercussions of its assumed struggle with the declining state of Dynasty 13 centered at Itjtawy. A revision of the recent evidence from Edfu raises doubts about the alleged contemporaneity of Sobekhotep iv and Khayan. A survey of administrative titles in the sources pertaining to the Theban kingdom testifies that it arose independently based on the local power structures of the Late Middle Kingdom rather than because of a relocation from the north. The separation of the nascent Theban kingdom from the state of Dynasty 13 and a surmised consequent confrontation between these entities had an impact on the ideology of the new polity and influenced the policy of its direct successor—the state of Dynasty 17 and the early New Kingdom. The original lack of legitimacy of Dynasty 16 could have been one of the reasons for overstating the power of the Hyksos in historical texts—in order to justify Theban claims to rule in Middle and Lower Egypt.


1975 ◽  
Vol 32 (12) ◽  
pp. 2413-2427 ◽  
Author(s):  
John G. Stockner ◽  
K. R. S. Shortreed

Ten stations located in six zones (subbasins) were sampled biweekly from May to October 1973 to detect possible regional differences in production in this large, 155 km long, dystrophic lake. The spring bloom occurred in all zones while a fall bloom occurred only in Zones 5 and 6. Carbon assimilation showed two peaks in south basin zones, but only one (spring) at zones north of Topley Landing. Seasonal variation in phytoplankton numbers and volume, seston, and chlorophyll a followed a pattern similar to that noted for primary production. Mean production was 100 mg C∙m−2∙day−1 in Zones 1–4, but was 145 in Zones 5 and 6. Annual production was estimated at 25 g C∙m−2 in the north basin and 40 in the south basin. Reasons for the regional disparities are discussed, with greatest significance given to regional variations in mixed layer depth, surface inflows (loading), and basin mean depth. The development and sustainment of the autumnal bloom of Tabellaria fenestrata is thought to be one of the principal factors responsible for greater production in the south basin.An estimated 0.05 g TP∙m−2 enters the lake yearly. This can vary depending on the return of adult sockeye salmon (Oncorhynchus nerka), whose carcasses contribute up to 20% of the total. An estimated 30% is lost via the Babine River, and it is speculated that of the remaining 70%, most is lost to the sediments. Phosphate limitation is implied as a chief factor limiting primary production in the north basin stations, but not in the south basin. On the basis of total phosphorus load the lake is classed as oligotrophic, but in terms of annual production and its humic stained waters it is more correctly considered mixotrophic.


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