Operation Refugee: the Congo Crisis and the end of humanitarian imperialism in Southern Rhodesia, 1960

2021 ◽  
pp. 1-22
Author(s):  
Brooks Marmon
Author(s):  
Gregory A. Barton

This chapter traces the expansion of industrial agricultural methods after the Second World War. Western governments and the Food and Agriculture Organization pushed for increased use of chemical fertilizers to aid development and resist Soviet encroachment. Meanwhile small groups of organic farmers and gardeners adopted Howard’s methods in the Anglo-sphere and elsewhere in the world. European movements paralleled these efforts and absorbed the basic principles of the Indore Method. British parliament debated the merits of organic farming, but Howard failed to persuade the government to adopt his policies. Southern Rhodesia, however, did implement his ideas in law. Desiccation theory aided his attempts in South Africa and elsewhere, and Louise Howard, after Albert’s death, kept alive a wide network of activists with her publications.


1973 ◽  
Vol 67 (5) ◽  
pp. 82-86
Author(s):  
Bert Lockwood ◽  
Beatrice Brickell

I would like to address myself to international outlaws and what domestic procedures are available to arrest their activities. While at first glance the nexus between domestic justice and international justice may seem tenuous, I wonder: Is it surprising that the same administration that is so insensate over the deprivation of the human rights of blacks in Southern Rhodesia is the same administration that proclaimed early in its tenure that if you have seen one slum you have pretty much seen them all, and hasn’t visited another since? Is it surprising that the same administration that evidences so little concern over the political rights of the majority in Rhodesia is the same administration that “bugs” and sabotages the political process within the United States?


1965 ◽  
Vol 5 (52) ◽  
pp. 351-360

The delegation of the International Committee of the Red Cross brought its aid to civilian and political prisoners.One of the ICRC representatives in Santo Domingo, Mr. Pierre Jequier, general delegate for Latin America, visited prisons of the “Constitutional Government” presided over by Colonel Francisco Caamano Deno and of the “Government of National Reconstruction” of General Antonio Imbert. There were no restrictions placed by either on visits.


1967 ◽  
Vol 8 (2) ◽  
pp. 226-239 ◽  
Author(s):  
W. J. Hudson

Relations between Australia and Indonesia became strained within months of Indonesia's attainment of independence, deteriorating as conflict developed first on the question of West Irian and then as a result of Indonesia's hostility towards Malaysia. For many years, it seemed ironical that Australia should have played a major part in the emergence of a neighbour whose external policies and internal trends endangered rather than safeguarded Australian interests. But there is more involved here than historical irony in the context of Australian-Indonesian relations. Sufficient time has now elapsed for Australian policy on the Indonesian independence question to be seen in the wider context of the whole postwar phenomenon of decolonisation. For it is not merely of interest that Australia should have assisted neighbouring Asian rebels against a European colonial Power (remembering that Australia herself was, and is, a European colonial Power) and should then have been embarrassed by the activities of the rebels coming to office. It is of greater interest that, of the immense number of colonial issues anxiously engaging the attention of international society in the 1940s and 1950s, the years which saw the virtual demise of western colonialism, this was the one issue on which Australia took up the rebel cause. Throughout this period and irrespective of the complexion of the parties in power in Canberra, Australia persistently jeopardised her regional objective of friendly relations with anti-colonial Asia by opposing strongly and, at times, bitterly the anti-colonial cause in the United Nations. If nothing else, the United Nations has provided a forum in which each year Australia and other members have been forced to declare themselves on colonial questions. And, until the 1960s when Australia switched policy, Australia fought against all the anti-colonial Powers' largely successful attempts to have developed a system of international control over colonies under the authority of Chapter XI (“Declaration Regarding Non-Self-Governing Territories”) of the United Nations charter, to tighten the trusteeship system of supervision erected under Chapters XII and XIII of the charter, and to involve the United Nations in particular disputes so as to meet alleged threats to peace — all of them being attempts, however indirectly, to hasten the attainment of independence by dependent territories. Thus, Australia supported South Africa on South-West Africa, the Netherlands on West New Guinea, the British on Southern Rhodesia and Oman, the Portuguese on their African territories, the French on Morocco, Tunisia and Algeria. But Australia opposed the Netherlands on the Indonesian question.


Recent work has determined the depth of the Mohorovičić discontinuity at sea and has made it likely that peridotite xenoliths in basaltic volcanic rocks are samples of material from below the discontinuity. It is now possible to produce a hypothetical section showing the transition from a continent to an ocean. This section is consistent with both the seismic and gravity results. The possible reactions of the crust to changes in the total volume of sea water are dis­cussed. It seems possible that the oceans were shallower and the crust thinner in the Archean than they are now. If this were so, some features of the oldest rocks of Canada and Southern Rhodesia could be explained. Three processes are described that might lead to the formation of oceanic ridges; one of these involves tension, one compression and the other quiet tectonic conditions. It is likely that not all ridges are formed in the same way. It is possible that serpentization of olivine by water rising from the interior of the earth plays an important part in producing changes of level in the ocean floor and anomalies in heat flow. Finally, a method of reducing gravity observations at sea is discussed.


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