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By Gunnar Wolf, Alejandro Miranda

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03) includes " sites with unique natural values" with or without cultural value. There is discussion as to whether to include this aspect. Page 5 2 Karst: Processes and Landforms The Process of Karst Formation There are large tracts of land in East Asia with spectacular topography: pitted plateaus, deeply dissected by closed despressions and with gorges in one or more directions; ranges of hills with jagged, razor-sharp crests; and towering hills rising from otherwise flat river plains or from the sea.

Air movement is also buffered by the cave walls, but still occurs as air is drawn out of the cave during the day, when the air outside is warmer and lighter. This air movement follows a regular pattern, but leaves pockets of still air in deep caves, where spiders can weave delicate and complex webs, and preserves pockets of high humidity. In these deeper areas, the Page 14 concentration of carbon dioxide increases if there is no inflow of air except from the cave mouth. It is likely that life in underground communities will turn out to be richer and more diverse than scientists could ever have anticipated.

Limestone is of major importance in development, with the production of cement even used as a barometer of growth and progress. In many infrastructure projectssuch as dam and bridge construction, port development, building construction, and road building and upgradingthe extraction of limestone is a fundamental, and in most cases irreplaceable, development activity. The quarrying of limestone, being a subsidiary (and often remote) element of a large infrastructure project, is rarely adequately assessed for its total impacts.

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