This paper presented the karst features related to geotechnical issues. This study contains an overview of karst terrain and limestone in Malaysia. There are unalloyed karst landscapes in many parts of the world, but most of the time landscapes are formed by a multitude of processes. The intellectual capacity of the dissolution processes, that be active both at the surface and subsurface, has developed quickly in the last fully century, Karst topography is a landscape of characteristic suspension patterns often noticeable by subsurface drainages. Limestone, with its low calcium carbonate content, is easily dissolved in the acids produced by natural materials.
Keywords: Karst, Limestone, Surface, Subsurface, Landscape, Malaysia.
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