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*Geodes are hollow, crystal-lined globular rock cavities found in sedimentary rocks like limestone (calcium carbonate) and dolomite (calcium magnesium carbonate) or in volcanic rocks. In sedimentary rocks, geodes may form by dissolving out cavities by ground water and re-depositing of minerals as crystals, which usually point towards the centre of the cavity. They may also form in pre-existing concretions or in spaces left by expansion of the rock under internal fluid pressure. They often have an outer shell of chalcedony, a crystal lining of quartz, carbonates or other minerals, and can be over a metre in diameter.