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As part of the World Athletics Day, 11 of these athletes will be entered in a summer draw by the International Amateur Athletic Federation that will select one boy and one girl from each continental area of the world for an all-expenses-paid trip to the 2001 World Championships in Edmonton, Alberta.
Figure 1 Heat flow map in the continental area of China (revised from Wang et al.[2012]).[2012]
MDY is located in central Eastern Siberia near the Russia Mongolia border, which is known to be a very lightly populated continental area of the world.
The Caledonian orogeny at the end of the Silurian resulted in great changes in the palaeogeography in the Yunnan-Guizhou-Guangxi area of South China; the continental area of the Early Paleozoic evolved into the extensive Dian-Qian-Gui Sea in the Late Paleozoic.
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Similar facies are known in other continental areas of the Devonian.
For example, in continental areas of Canada, stand-replacing fires with relatively short rotation cycles are common and maintain even-aged forest dynamics over extensive areas (Payette 1992).
The heat flow values in this part of the Cambay rift zone are higher at 75 96 mW/m2, with mean 83±± 7 mW/m2, than that of stable continental areas of whose value is ~ 46 mW/m2 (Verma et al. 1968; Gupta et al. 1970; Gupta 1981), a difference that may alter the melts to garnet-bearing high-pressure granulites.
Whereas we studied the effect of episodic drought so far, ongoing water retention experiments and transect studies along gradients of water availability might reveal whether more frequent drought events and continuous drought stress may result in stand dynamics as known from permanently dry and continental areas of, e.g., central Spain, southwest USA, and inner South Africa.
For example, when you compare (as Wade does) people from Nigeria, Western Europe and Beijing and Tokyo, you do get some patterned differences, but these populations do not reflect the entire continental areas of Africa, Europe and Asia, respectively.
The presence of this arid microclimate-adapted (Hahn et al. 1989; Lange et al. 1995) community of colored soil lichens, centered in the Mediterranean and the continental areas of the Eurasian continent, may be explained as a relic of the postglacial warm period (Reimers 1940).
Karst landform represents about 10% of the continental area and plays key roles in water supplies for almost a quarter of the global population.
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