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Sulfate

Gypsum

CaSO₄·2H₂O

Sobre Gypsum

Gypsum is one of the most abundant, useful, and geologically fascinating sulfate minerals on the planet. It is the most common sulfate mineral, forming massive beds of sedimentary rock that stretch for hundreds of miles, while simultaneously producing some of the largest, most spectacular, and delicate transparent crystals ever discovered on Earth.

The name “Gypsum” comes directly from the Greek word gypsos, meaning “plaster” or “chalk.” For thousands of years, humans have mined, crushed, and heated this soft white rock to build their civilizations—from the mortar used in the ancient Egyptian pyramids to the drywall (Sheetrock) lining almost every modern home today.

Formation & Geology

Gypsum (calcium sulfate dihydrate) is a classic evaporite mineral. Like Halite (rock salt), it forms when massive, shallow bodies of mineral-rich water evaporate. Millions of years ago, as ancient seas or saltwater lakes slowly dried up under the hot sun, the dissolved calcium and sulfate became too concentrated to remain in solution. The Gypsum precipitated out, sinking to the bottom to form thick, extensive, horizontal beds of sedimentary rock.

Because it requires water to form (the “dihydrate” part of its formula means it contains two water molecules), Gypsum is often found layered with or near other evaporites like Halite or Anhydrite (calcium sulfate without the water).

Gypsum also forms in volcanic areas where sulfur-rich hot springs interact with limestone, and frequently in clay beds or shales where the oxidation of pyrite (iron sulfide) produces sulfuric acid that reacts with calcium carbonate (shells or limestone) to grow beautiful, clear crystals.

Physical Characteristics

Gypsum crystallizes in the monoclinic system and is famous for its extreme variety of physical habits. It is the defining standard for a hardness of 2 on the Mohs scale, making it so soft it can easily be scratched by a human fingernail.

The massive, rock-forming variety is typically opaque, white, or gray, and is incredibly soft and earthy. When this massive form is exceptionally fine-grained, smooth, and slightly translucent (often glowing softly when backlit), it is called Alabaster, a favorite material for sculptors since antiquity because it is so easily carved without shattering.

When Gypsum grows slowly in open cavities or clay beds, it forms transparent, colorless, diamond-shaped or blade-like crystals known as Selenite. Another striking habit is Satin Spar, which forms as tightly packed, parallel, fibrous crystals that exhibit a brilliant, silky chatoyancy (a cat’s-eye effect) when polished. Finally, in arid, sandy environments, it forms the iconic, overlapping, petal-like clusters known as the Desert Rose, which are colored brown or tan by the sand trapped within the growing crystals.

It has perfect cleavage in one direction, meaning large Selenite crystals can easily be split into thin, somewhat flexible (but inelastic) sheets.

Industrial Uses & Science

The industrial importance of massive Gypsum cannot be overstated. When heated to about 300°F (150°C), Gypsum loses 75% of its water content, transforming into a fine white powder known as Plaster of Paris. When water is added back to this powder, it recombines and solidifies into hard Gypsum again.

This chemical “trick” makes it the primary ingredient in drywall (wallboard), plaster, and cement. Because the remaining 25% of the water is locked in the crystal lattice, Gypsum drywall is naturally highly fire-resistant; in a fire, the wall will not burn until all the internal water has slowly boiled away as steam. It is also used extensively as an agricultural soil conditioner to loosen heavy clay soils and provide calcium and sulfur to crops.

Metaphysical Properties

In the metaphysical community, the clear crystalline form of Gypsum (Selenite) is considered one of the most powerful and essential tools for energy clearing and charging. Named after Selene, the Greek goddess of the moon, it is believed to carry a very high, pure vibration that instantly cleanses the aura, clears blocked energy, and elevates the spirit. Practitioners use Selenite wands or plates to “charge” or cleanse other crystals, and frequently place it in corners of a room to establish a peaceful, protective, and spiritually open environment.


Cores e Variedades

Colorless, white, gray, yellow, brown, pink


Propriedades Chave

  • Very common sulfate mineral
  • Standard reference for hardness 2 on the Mohs scale
  • Found as massive rock (Alabaster) or transparent crystals (Selenite)
  • Often forms "Desert Rose" crystal clusters
  • Highly useful industrial building material

Usos e Aplicações

  • Drywall (Sheetrock / Gypsum board)
  • Plaster of Paris
  • Soil conditioner and fertilizer
  • Ornamental carving (Alabaster)

Onde Encontrar

  • United States (White Sands, New Mexico)
  • Mexico (Naica Mine - giant crystals)
  • France
  • Italy (Tuscany - fine Alabaster)
  • Canada

Frequently Asked Questions

What is the difference between Gypsum, Selenite, and Alabaster?

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They are all the exact same mineral: Calcium Sulfate Dihydrate (CaSO₄·2H₂O). The names simply describe how the mineral formed. "Gypsum" is the general name for the mineral and the massive rock it forms. "Selenite" is the name for the clear, transparent, crystalline variety. "Alabaster" is the name for the fine-grained, massive, opaque white or softly colored variety that has been used for carving statues for thousands of years.

Can you scratch Gypsum with your fingernail?

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Yes! Gypsum is the defining standard for a hardness of exactly 2 on the Mohs hardness scale. Since an average human fingernail has a hardness of about 2.5, you can easily scratch a piece of solid Gypsum or Selenite with your nail.

Is the "Desert Rose" made of Gypsum?

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Most often, yes. The famous "Desert Rose" (or Sand Rose) is a beautiful, naturally occurring rosette formation. It happens when groundwater heavily saturated with dissolved calcium sulfate evaporates in sandy, arid conditions (like the Sahara or the deserts of the US Southwest). The Gypsum crystallizes outward in overlapping, circular plates, trapping the surrounding sand inside the crystal structure to create the petal-like shapes. (Note: Barite can also form Desert Roses).

Why is Gypsum used in drywall?

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Gypsum is incredibly useful as a building material because of its chemical formula (CaSO₄·2H₂O), which includes two molecules of water. When Gypsum (or Plaster of Paris) is exposed to fire, this trapped water slowly boils off as steam, keeping the temperature of the wall relatively low and preventing the fire from spreading quickly. This makes drywall naturally fire-resistant.

How did Gypsum get its name?

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The name is derived from the Greek word "gypsos," which simply means "chalk" or "plaster." The Greeks and Romans used massive quantities of burnt Gypsum to create plaster for their buildings and statues.