Hydromagnesite is a hydrated magnesium carbonate mineral with the formula .

It generally occurs associated with the weathering products of magnesium containing minerals such as serpentine or brucite. It occurs as incrustations and vein or fracture fillings in ultramafic rocks and serpentinites, and occurs in hydrothermally altered dolomite and marble. Hydromagnesite commonly appears in caves as speleothems and "moonmilk", deposited from water that has seeped through magnesium rich rocks. It is the most common cave carbonate after calcite and aragonite. over a temperature range of approximately 220 °C to 550 °C, releasing water and carbon dioxide leaving a magnesium oxide residue.

Hydromagnesite was first described in 1836 for an occurrence in Hoboken, New Jersey.

thumbnail|left|SEM micrograph of hydromagnesite showing platy crystal morphology. Sample was collected from the hydromagnesite-magnesite playas near Atlin, British Columbia, Canada.

Microbial deposition of hydromagnesite is also reported from playas in British Columbia. The hydromagnesite-magnesite playas near Atlin, British Columbia are some of the most studied deposits of hydromagnesite. These deposits have been characterized in the context of a biogeochemical model for CO<sub>2</sub> sequestration. It consists of a natural mixture with huntite. Local people have used the white mineral as a source of material for whitewashing buildings for centuries. In the mid 20th century the minerals, ground to a fine powder, found use as a filler for rubber shoe soles. The locals used the granite mills designed for grinding wheat. Commercial exploitation of the minerals began in the late 70s and early 80s with the mineral being exported worldwide. The Greek deposit is still operated commercially, although the world's largest commercially operated reserves are in Turkey.

Uses

Its most common industrial use is as a mixture with huntite as a flame retardant or fire retardant additive for polymers. Hydromagnesite decomposes endothermically, Syntheic hydromagnesite is known as light magnesium carbonate due to its low bulk density.

Thermal decomposition

Hydromagnesite thermally decomposes in three stages releasing water and carbon dioxide.