Abstract
Abstract Solution features are common phenomena within Chalk areas and the classical theory states that solution features are formed entirely by dissolution of the Chalk as a result of chemical weathering, probably during the Quaternary period. These solution features pose a risk to development and infrastructure works in these areas due to the presence of soft or loose infill materials. As a result a number of treatment methods have been developed to overcome the problems of construction in these areas. Observations of solution features encountered at three sites in southeast England, all underlain by Upper Chalk, are reviewed and the treatment methods designed to overcome the hazards posed are discussed.
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