Hydrocalumite-like layered double hydroxides are anionic clays comprising positively charged metal hydroxide layers of the composition [Ca 2 Al(OH) 6 (H 2 O) 2 ] + . The water molecules provide the seventh coordination for the Ca 2+ ion. Anions are intercalated in the interlayer space to balance the charge leading to a class of LDHs having the formula [Ca 2 Al(OH) 6 (H 2 O) 2 ]·A (A = Cl, Br, I). Upon dehydration the Ca 2+ ion gets coordinatively unsaturated, and crystal chemical considerations dictate that the layered structure should collapse. When A = ClO 4 -, the LDH dehydrates fully below 80°C, but the layered structure is retained [a]