Essai d'Interprétation du Cliché de Kangere (dans la Région des Grands Lacs Africains)

1990 ◽  
Vol 31 (3) ◽  
pp. 353-372 ◽  
Author(s):  
Yogolelo Tambwe Ya Kasimba

The Kangere cliché is widespread in the Great Lakes region of Zaire (Lakes Kivu and Tanganyika), where the Bembe, Fulero, Havu, Lega, Nyindu, Shi, Vira and others live. This cliché has been collected since the 1910s by missionary and colonial administrator researchers. Later it has been heavily used and interpreted in different ways. Thus certain modern scholars have made Kangere the first ‘king’ of the region and the ‘father’ of all bami, that is, the ‘kings’ of various ancient kingdoms existing on the shores of the Great Lakes, including Rwanda and Burundi! Their single aim was to refute the ‘Hamitic myth’.In fact, the Kangere cliché is woven together from different elements taken from various ethnic groups of the region. Its elements were ordered at the same time that they were collected, in the course of the 1910s and the 1920s. They constitute an African response to the preoccupation of the colonial administration of those years: the creation of vast ethnic groups and politically and administratively viable entities. Whites wanted tribes, and blacks created them; whites wanted great chiefs, and blacks created them, the bami.In their interpretation of the Kangere cliché, these researchers quite simply confused, erroneously, the ‘bwami symbol’ of personalized power (which existed in the area, and which chiefs of different ethnic groups possessed) with the ‘bwami state’ or kingdom, of recent, colonial creation.

2007 ◽  
Vol 135 (12) ◽  
pp. 4202-4213 ◽  
Author(s):  
Yarice Rodriguez ◽  
David A. R. Kristovich ◽  
Mark R. Hjelmfelt

Abstract Premodification of the atmosphere by upwind lakes is known to influence lake-effect snowstorm intensity and locations over downwind lakes. This study highlights perhaps the most visible manifestation of the link between convection over two or more of the Great Lakes lake-to-lake (L2L) cloud bands. Emphasis is placed on L2L cloud bands observed in high-resolution satellite imagery on 2 December 2003. These L2L cloud bands developed over Lake Superior and were modified as they passed over Lakes Michigan and Erie and intervening land areas. This event is put into a longer-term context through documentation of the frequency with which lake-effect and, particularly, L2L cloud bands occurred over a 5-yr time period over different areas of the Great Lakes region.


1995 ◽  
Vol 103 ◽  
pp. 51 ◽  
Author(s):  
William W. Bowerman ◽  
John P. Giesy ◽  
David A. Best ◽  
Vincent J. Kramer

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