By Philip Jodidio
The easiest of up to date architectural layout (TASCHEN's twenty fifth anniversary exact variation) The cr?me de los angeles cr?me of the main influential architects and architectural firms?the definitive reference consultant to modern architectural layout. right here you can find regular names, similar to O. Gehry, Meier, Ando, Foster, and Starck, in addition to a number of marvelous destiny stars. Highlights contain Jakob ' MacFarlane's morphological George eating place on the Centre Georges Pompidou, Paris, Diller ' Scofidio's "Blur construction" thought for the overseas Expo 2001 in Switzerland, and Herzog ' De Meuron's awesome Tate sleek. prepared alphabetically through architect or enterprise, with biographical and phone info for designers and an intensive choice of photos and illustrations, this quantity provides the highlights of structure Now! Vol 1
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Aptur! r.. fo, thi. lies in the presenceoffluvial gravel deposits and terracesto and the Kazuma and west of the Gwayi and in northeastern Botswana, Mpandamatenga lacustrine features (Figure 2'9; Mallick et al', 1981)' the or e*isten.. Middle Zambezi and the modern Zambezi River The precursor of the Middle Zambezi was an exoreic river on the coasrward side of th! Great Escarpment (Figure 2'8b). Downwarping along the ancient Gwembe and Chicoa troughr, purt of1h. rted to its considerable headward erosion and ultimately the capture of the proto'Upper Zambezi(Bond, 1963;Williams' 1975)' in the Pliocene or Upp..
80 Ma Full marine conditions in South Atlantic 130 Ma Initial opening ofthe South Atlantic phase of rifting ) Malor I 16 l and iniriarion of the J hingeline and Great Escarpment 180 Ma Separation of Antarctica from eastern matgin of soutlern Aftica I c 200 Ma Beginaing of Gondwanaland break-up TRIASSIC 225 development of Africa created the framework which led to the deposition ofthe Kalahari Group of sediments, and contributed to the nature of the sedimentary environment in the continental interior and to drainage evolution during the deposition ofthe sediments.
12. Formations N omenclature of Smnh(1984). overlying Karoo strata represent the infilling of a shallow basin (Lockett, 1979), first by waterlain deposits and fina1ly by tenesrial sediments. 3 Ecca Gtoup The Ecca Group contains carbonaceoussediments of economic value which are today being exploited, not only in the well establishedcoalflelds of South Africa and the eastern Kalahari margin at Hwange in Zimbabwe, but also within the Kalahari itself. Although Clark-Lowes and Yeats (1977) and Jones (1982) considered Ecca sediments to be absent from the Southwestern Botswana Basin, Smith (1984) has demonstrated their ptesence,while they may also occur at thebaseofthe Karoo sequencein the Okavango graben asthe Ngami Beds, Ngwako Formation (Clark-Lowes and Yeats, 1977;Coates, 1980),or Tale and Marakwena Formations (Smith 1984),representing local lacustrine infilling of the subsiding graben.