Marshallite. Uses, extraction and deposits
Marshallite is a loose or weakly consolidated rock composed of 85–98% fine quartz grains and various impurities. It is a residual product of the weathering of silicified limestones, quartzites, and some other siliceous rocks. Marshallite is also known as quartz dust or flour quartz.
It forms through the crushing and screening of quartz material.In terms of chemical composition, marshallite mainly consists of SiO₂, with minor impurities of Al₂O₃, Fe₂O₃, and TiO₂. It has an amorphous or crystalline structure with a powdery fraction, white, grayish, or translucent-milky color, a Mohs hardness of 7, and high resistance to thermal and chemical influences.
Marshallite is included in the list of minerals of national importance, approved by Resolution of the Cabinet of Ministers of Ukraine No. 827 of December 12, 1994, as an abrasive raw material.
List of minerals of national importance
See the complete classified list of minerals in Ukraine
Go to the listConditions of formation and extraction
Marshallite forms through several geological processes. The main factors include hydrothermal activity, during which silica-rich hot solutions penetrate rocks and deposit quartz in the form of fine, dust-like masses; mechanical breakdown of quartz rocks during weathering or quarrying; and sedimentary processes, when quartz dust settles in marine or freshwater basins and becomes compacted into thin layers. These formation conditions give the mineral high purity and homogeneity, which are important for industrial use.
Marshallite is mainly extracted by open-pit mining. The quarrying method involves the development of quartz sands, their crushing, and screening to obtain a fine powder fraction. Additional industrial processing includes classification, washing, drying, and grinding to the required particle size. Global production reaches millions of tons per year, depending on demand from the glass and abrasive industries.
Quartz dust during extraction can cause respiratory diseases such as silicosis among workers, while quarrying significantly alters landscapes and affects soils, hydrological regimes, flora, and fauna. To minimize negative impacts, dust control systems, quarry reclamation, and emission monitoring are applied.
Occurrences and deposits in Ukraine
Occurrences of marshallite in Ukraine have been recorded in the Kryvyi Rih iron ore basin, where they are associated with hypergene zones of siliceous–iron and schistose–siliceous–iron formations, particularly oxidized ores of the Saksahan district. Another significant deposit is located northwest of Kyiv — the Havrylivske deposit (near the village of Havrylivka, Dymer district). It is represented by a bed enriched with marshallite, with an outcrop area of about 130 hectares, a thickness of 1.4–4.8 m, and a depth of occurrence of 5.12–8.75 m, associated with Poltava sands.
The mineral composition of the deposit is dominated by quartz (93–94%) and kaolinite (5–6%), with minor amounts of plagioclase, chalcedony, leucoxene, and traces of tourmaline, rutile, disthene, zircon, apatite, ilmenite, and epidote. The granulometric composition is dominated by a fine fraction of 0.01–0.06 mm (96–98%). The overburden thickness is 7.1 m, half of which is high-quality brick and tile raw material. Estimated reserves of marshallite are about 5.4 million m³.
Outside Ukraine, marshallite is also found in the United States, Chile, South Africa, and Asia, with several isolated occurrences in Europe.
Uses of marshallite
Marshallite is widely used in industry for the production of liquid glass, which serves as a base for manufacturing artificial stone, building components (in combination with blast-furnace slag, sand, sawdust, etc.), as well as artistic and decorative products made from ground marble.It is used for densifying porous stone masses, accelerating cement hardening, soil stabilization, impregnation of road surfaces, coal briquetting, production of acid-resistant cement, abrasive materials, refractory products, and arc lamp cores. In addition, marshallite is a raw material for the production of silicate adhesives, plywood, fiberboard, surgical dressings, and is also used as a filler in the plastics, rubber, glass, and porcelain–faience industries.