Mineral
Magnesite
MgCO₃Manyezit
The raw material of furnace bricks and the ore of magnesium: Türkiye is among the world's largest magnesite producers.
Also known as: Calcined magnesite (heat-treated product)
- Popularly: Ore and raw material
- Industrial
- Ore
- Important in Türkiye
In short
Magnesite is a white, porcelain-like or chalky carbonate mineral made of magnesium and carbon (MgCO₃). It resembles calcite, but it most often occurs as fine-grained, hard, dull masses. Its main importance is as the raw material of heat-resistant (refractory) bricks and of magnesium compounds. Because it takes up dye easily, it is also made into beads and sometimes sold dyed blue as “turquoise”.
Photos
How does it form?
Magnesite forms when magnesium-rich rocks (such as serpentinite, peridotite or dolomite) react with water carrying carbon dioxide. There are two main types.
Cryptocrystalline (gel) magnesite is deposited in veins and net-like stockworks that fill the cracks and fractures of serpentinised ultramafic rocks. Most of the deposits in Türkiye are of this type; it gives very fine-grained, white, porcelain-like masses. Crystalline (sparry) magnesite mostly forms when dolomitic limestones are transformed by hot waters; it is coarse-grained, rich in iron and forms very large deposits. The deposits of the Eastern Alps, the Carpathians and the Urals are of this type. Layered magnesite deposited in lakes and evaporating basins is rarer.
What is it used for?
- Refractory bricks: More than 90% of the magnesite mined is fired to caustic-calcined or sintered magnesite. These products are used in the heat-resistant (refractory) bricks lining steel, cement, glass and copper furnaces.
- Magnesium compounds: It is the raw material of magnesium oxide and other magnesium compounds, used in medicines, fertilisers and animal feed, paper, sugar, rubber and insulation, among many other things.
- Flooring: Fired magnesite serves as the binder in magnesia screed, a type of floor covering.
- Beads and jewellery: It is cut, drilled and polished into beads. Being porous, it can be dyed any colour; pieces dyed blue are sometimes sold in place of turquoise. Being soft and prone to splitting, it needs a protective setting in jewellery.
In Türkiye
Türkiye is one of the world’s major magnesite producers. According to the 2026 U.S. Geological Survey (USGS) summary, about 1.6 million tons of magnesite ore were mined in 2025, which puts the country fourth, after China, Brazil and Russia. The USGS estimates Türkiye’s reserves at 110 million tons.
Most Turkish deposits are of the cryptocrystalline (gel) type: veins and stockworks in the fractures of serpentinised ultramafic rocks, similar to the Kraubath deposits in Austria. An academic review based on the MTA inventory says that most of them lie in the Konya–Eskişehir–Kütahya triangle. In the review’s reserve table the largest deposit is Yukarıkartal in Eskişehir, with about 460 million tons, followed by Meram in Konya (about 23 million tons), Sobran–Türkmentepe in Kütahya (about 22 million tons) and Tutluca in Eskişehir (about 12 million tons); the table adds up to about 546 million tons. These figures come from an older inventory and cannot be compared directly with the USGS’s more cautious definition of reserves.
There are also deposits in Dursunbey (Balıkesir), Mustafakemalpaşa (Bursa) and Mudurnu (Bolu), and in Bilecik, Çankırı and Erzincan. The Hırsızdere deposit in Denizli and the Çayırlı deposit in Erzincan are examples of layered, sedimentary deposits not tied to ultramafic rocks. According to MTA, the first magnesite production in Türkiye began in 1929.
Mining and the firing of the ore into sintered and caustic-calcined magnesite are concentrated mostly in the provinces of Eskişehir and Kütahya. According to KÜMAŞ, a company based in Kütahya, it holds about 20 percent of the world’s cryptocrystalline magnesite reserves, makes magnesite-based refractory products and exports to more than 60 countries.
What determines its value?
Magnesite is an industrial raw material bought and sold by the ton. Its value depends on its magnesium oxide (MgO) content and the scarcity of harmful impurities: for refractory bricks, cryptocrystalline (gel) magnesite should contain at most about 1% silica (SiO₂), 1.5% calcium oxide and 0.5% iron oxide, and ore that meets these limits is worth much more than ordinary ore. The size of the deposit, how easily the ore is mined and concentrated, the cost of calcining and the distance to factories also matter. As a bead and jewellery material magnesite is inexpensive; whether it has been dyed, and whether that is disclosed, affects its worth, and for large, transparent crystal specimens size and clarity do.
This information is educational, not buying, selling or investment advice. Value varies enormously with quality and treatment.
How to recognise it
- 1
White, cream or grey; very often a dull, fine-grained, hard mass that looks like unglazed porcelain or chalk. Its rare large crystals are rhomb-shaped.
- 2
Mohs hardness is 3.5–4.5: a steel knife scratches it, but it cannot scratch glass.
- 3
Fine-grained masses break with a curved, shell-like fracture; with a density of about 3 it feels slightly heavier than a piece of calcite of the same size.
- 4
It does not fizz quickly in cold dilute acid the way calcite does; it fizzes in warm acid or as a powder. This helps separate it from similar-looking white calcite.
Fakes and imitations
What shops usually don’t tell you:
- White calcite, dolomite and howlite can look like magnesite. Calcite fizzes at once in cold dilute acid and magnesite does not; howlite does not fizz either but is clearly lighter (density around 2.5–2.6).
- Magnesite beads dyed blue are often sold as real turquoise because of their veined look. Such stones should be described as dyed; for a certain identification consult a gemmological laboratory.
Safety
Magnesite is harmless to handle. The fine dust from mines and calcining plants should not be breathed for long, and a dust mask should be used for dusty work. In the United States, the safety agency OSHA sets limits of 15 mg/m³ for total dust and 5 mg/m³ for respirable dust over an eight-hour working day.
Myths and misconceptions
MythAll blue “turquoise” beads are real turquoise.
FactSome of the cheap blue beads on the market are dyed magnesite or howlite. Magnesite is porous, so it takes dye well and imitates turquoise with its veined look; such stones should be sold as “dyed” or as “turquoise imitation”.
What is it believed to be good for?
This section reports beliefs; it is not health information. There is no scientific evidence for these claims and no stone replaces medical treatment.
The meanings people give this stone, and who holds them:
- Crystal therapy practitioners and stone sellers claim that white magnesite is calming and brings deep peace and quiet relaxation during meditation.
- The same sources say magnesite opens the “heart chakra” and gives a sense of happiness and self-love.
What science says
There is no controlled study showing that magnesite calms people or affects emotions; any relaxation comes from meditating and taking a quiet moment. Wearing or holding the stone does not give the body magnesium; anyone who suspects a magnesium deficiency should see a doctor. Grinding the stone and swallowing it is not advisable either: natural magnesite often contains impurities such as iron and silica, and mining dust should not be breathed.
Did you know?
When heated, magnesite gives off carbon dioxide. Fired at 700–1000 °C it becomes “caustic-calcined” magnesite, and at 1450–1750 °C a very dense, hard “sintered” magnesite; sintered magnesite is the main raw material of refractory bricks.
Magnesite has been detected in the ALH84001 meteorite from Mars and on Mars itself by infrared measurements, and magnesium carbonates have been reported around Jezero Crater.
The white shores of Lake Salda in Burdur contain hydromagnesite, a relative of magnesite. According to NASA, the minerals and rock deposits there are the nearest match on Earth to those around Jezero Crater, where the Perseverance rover landed.
Where is it found?
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- Haicheng–Dashiqiao belt, Liaoning, China · Major depositChina is the world's largest magnesite producer; according to the USGS most output is concentrated in Liaoning Province. The Handbook of Mineralogy also mentions “immense deposits” in the Liaoning district.
- Brumado, Serra das Éguas, Bahia, Brazil · Major depositBrazil is the world's second-largest producer; the pits at Brumado are counted among the largest open-pit magnesite mines. The large, transparent, rhomb-shaped crystals used for jewellery and collecting also come from here.
- Satka, Chelyabinsk Oblast, Russia · Major depositIn the Southern Urals the town's economy rests on magnesite mining and refractory production; Russia is the world's third-largest producer.
- Radenthein, Carinthia, Austria · Historic sourceThe large magnesite deposits here were found around 1908 and mining shaped the town. The Handbook of Mineralogy reports large crystals from here.
- Jelšava, Banská Bystrica Region, Slovakia · Historic sourceThe first magnesite furnace in present-day Slovakia was built here in 1894.
- Gabbs area, Nye County, Nevada, USA · Known localityAccording to the Handbook of Mineralogy a large magnesite deposit lies here; according to the USGS magnesite in the United States is mined by a single company in Nevada.
- West of Eskişehir (Tutluca–Yukarıkartal–Ballık area), Türkiye · Major depositTürkiye's largest magnesite reserves are in the Eskişehir area; most deposits are veins in serpentinised ultramafic rocks.
- Kütahya (Sobran–Türkmentepe area), Türkiye · Major depositBesides magnesite mining, Kütahya also produces calcined and sintered magnesite and refractory products.
- Meram–Çayırbağı, Konya, Türkiye · Known localityThe cryptocrystalline magnesite deposits at Konya lie at the southern tip of the Konya–Eskişehir–Kütahya triangle.
Locations are approximate to protect sites. Red dots mark places in Türkiye. Open in the big map →
Frequently asked questions
What is magnesite?
Magnesite is a white, porcelain-like or chalky carbonate mineral made of magnesium and carbon (MgCO₃). It resembles calcite, but it most often occurs as fine-grained, hard, dull masses. Its main importance is as the raw material of heat-resistant (refractory) bricks and of magnesium compounds. Because it takes up dye easily, it is also made into beads and sometimes sold dyed blue as “turquoise”.
What is magnesite used for?
Refractory bricks: More than 90% of the magnesite mined is fired to caustic-calcined or sintered magnesite. These products are used in the heat-resistant (refractory) bricks lining steel, cement, glass and copper furnaces. Magnesium compounds: It is the raw material of magnesium oxide and other magnesium compounds, used in medicines, fertilisers and animal feed, paper, sugar, rubber and insulation, among many other things. Flooring: Fired magnesite serves as the binder in magnesia screed, a type of floor covering. Beads and jewellery: It is cut, drilled and polished into beads.
How hard is magnesite?
It has a hardness of 3.5–4.5 on the Mohs scale. A fingernail cannot scratch it, but a steel knife can. Its specific gravity is 3–3.2 g/cm³.
Where is magnesite found?
Its best-known localities: Haicheng–Dashiqiao belt, Liaoning, China; Brumado, Serra das Éguas, Bahia, Brazil; Satka, Chelyabinsk Oblast, Russia; West of Eskişehir (Tutluca–Yukarıkartal–Ballık area), Türkiye; Kütahya (Sobran–Türkmentepe area), Türkiye.
Where is magnesite found in Türkiye?
Known localities in Türkiye: West of Eskişehir (Tutluca–Yukarıkartal–Ballık area), Türkiye; Kütahya (Sobran–Türkmentepe area), Türkiye; Meram–Çayırbağı, Konya, Türkiye.
How can you tell if magnesite is real?
White, cream or grey; very often a dull, fine-grained, hard mass that looks like unglazed porcelain or chalk. Its rare large crystals are rhomb-shaped. Mohs hardness is 3.5–4.5: a steel knife scratches it, but it cannot scratch glass. Fine-grained masses break with a curved, shell-like fracture; with a density of about 3 it feels slightly heavier than a piece of calcite of the same size. White calcite, dolomite and howlite can look like magnesite. Calcite fizzes at once in cold dilute acid and magnesite does not; howlite does not fizz either but is clearly lighter (density around 2.5–2.6).
Is magnesite valuable?
On the “street to diamond” value ladder it sits on step 3 of nine: Building and industrial stone. Magnesite is an industrial raw material bought and sold by the ton. Its value depends on its magnesium oxide (MgO) content and the scarcity of harmful impurities: for refractory bricks, cryptocrystalline (gel) magnesite should contain at most about 1% silica (SiO₂), 1.5% calcium oxide and 0.5% iron oxide, and ore that meets these limits is worth much more than ordinary ore. The size of the deposit, how easily the ore is mined and concentrated, the cost of calcining and the distance to factories also matter. As a bead and jewellery material magnesite is inexpensive; whether it has been dyed, and whether that is disclosed, affects its worth, and for large, transparent crystal specimens size and clarity do.
What is magnesite good for?
Crystal therapy practitioners and stone sellers claim that white magnesite is calming and brings deep peace and quiet relaxation during meditation. The same sources say magnesite opens the “heart chakra” and gives a sense of happiness and self-love. There is no controlled study showing that magnesite calms people or affects emotions; any relaxation comes from meditating and taking a quiet moment. Wearing or holding the stone does not give the body magnesium; anyone who suspects a magnesium deficiency should see a doctor. Grinding the stone and swallowing it is not advisable either: natural magnesite often contains impurities such as iron and silica, and mining dust should not be breathed. This section reports beliefs; it is not health information. There is no scientific evidence for these claims and no stone replaces medical treatment.
Is magnesite dangerous?
Magnesite is harmless to handle. The fine dust from mines and calcining plants should not be breathed for long, and a dust mask should be used for dusty work. In the United States, the safety agency OSHA sets limits of 15 mg/m³ for total dust and 5 mg/m³ for respirable dust over an eight-hour working day.
Sources
- Handbook of Mineralogy: Magnesite · Mineralogical Society of America
- Magnesite · Wikipedia
- Magnezit · Vikipedi
- Mineral Commodity Summaries 2026: Magnesium Compounds · U.S. Geological Survey, 2026
- Manyezit yataklarının oluşumu, sınıflandırılması, kullanım alanları ve kalite sınıflandırılması (Yılmaz & Kuşcu), Erciyes Üniversitesi Fen Bilimleri Enstitüsü Dergisi 28(1): 65–72 · Erciyes Üniversitesi
- Manyezit · MTA Genel Müdürlüğü, Bilgi Merkezi
- Magnesite · Encyclopaedia Britannica
- Magnesite Value, Price, and Jewelry Information · International Gem Society
- KÜMAŞ manyezit ürünlerini 60'tan fazla ülkeye ihraç ediyor · Anadolu Ajansı (Foreks), 2026
- Brumado · Wikipedia
- Satka · Wikipedia
- Radenthein · Wikipedia
- Jelšava · Wikipedia
- Gabbs, Nevada · Wikipedia
- Lake Salda · Wikipedia
External links
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