Log in Sign up
Back to Discover
🌍

Scheelite

earth science Maturity 7-9

This is a special rock.

CaWO4.tif
CaWO4.tif
It can be many colors. Some look like gold. Some look like pink. It can even glow bright blue! This helps people find gold. Do you like shiny rocks?

35 words

Scheelite is a special rock.

CaWO4.tif
CaWO4.tif
It can be many colors. Some look like gold. Some look pink or orange. It can even be clear.

This rock is very heavy. Some people call it "heavy stone." It is used to find a metal called tungsten.

Some parts of the rock glow. Under special light, it glows bright blue. This helps people find gold in the ground.

People also use it to make light. It can turn invisible light into light we can see.

Bispbergs klack.jpg
Bispbergs klack.jpg

Collectors like to find pretty crystals. Some even use them as gems.

97 words

Scheelite is a special mineral. It is a source of tungsten. Tungsten is a heavy metal.

CaWO4.tif
CaWO4.tif
The mineral was named for Carl Wilhelm Scheele. He was a chemist from Sweden.

Scheelite has many colors. It can look gold, orange, or pink. Some pieces are clear. The crystals can be many shapes. They can look like columns or flat plates.

Bispbergs klack.jpg
Bispbergs klack.jpg
Many crystals have a shiny look. This shine is called luster. It can look like a diamond.

This mineral does something very cool. It shows fluorescence. This means it glows under special light. Most scheelite glows bright blue. Some pieces glow green. Geologists use this glow to find gold.

People use scheelite for many jobs. It helps make light for lamps. It is also used in X-ray machines. Thomas Edison used it for a screen. His screen made images much brighter. Some people even make fake scheelite in labs. They use it to look like diamonds. Real scheelite usually has tiny flaws inside. Lab stones are often too perfect.

171 words

Scheelite is a very important mineral. It is a main source of tungsten. People call tungsten "heavy stone" in Swedish. This mineral is made of calcium and tungsten.

CaWO4.tif
CaWO4.tif
It is also known as calcium tungstate. This mineral is used in many ways. It can be a gemstone for collectors. Some people even use it to make fake diamonds. It can also be used in lasers. It is a very useful thing to find in the Earth.

This mineral has a very interesting way it works. It shows something called fluorescence. This means it glows under special ultraviolet light. Most scheelite glows a bright sky-blue color. Sometimes it glows green if it has molybdenum inside.

Bispbergs klack.jpg
Bispbergs klack.jpg
Geologists look for this blue glow in the field. They use it to help find gold deposits. The glow is a bright sign in the dark. This makes it a great tool for science.

History tells us about this mineral's discovery. It was first described in the year 1751. This happened at Mount Bispbergs klack in Sweden. The mineral was named after Carl Wilhelm Scheele. He was a famous chemist from Sweden. He lived from 1742 to 1786.

Bispbergs klack.jpg
Bispbergs klack.jpg
People used to call the ore scheelerz. Later, the name became scheelite. It is a long history for this stone.

Scheelite can be found in many places. You can find it in the Czech Republic. It is also in Switzerland and Arizona.

CaWO4.tif
CaWO4.tif
Some large crystals come from Japan. In Australia, it was mined at King Island. There is also a lot in Brazil. The mineral has a high weight. Its specific gravity is between 5.9 and 6.1. It is also quite hard at 4.5 to 5. It can look gold, pink, or even colorless.

Many things you know use scheelite. Thomas Edison used it for a special screen. This screen helped X-ray images look much brighter. It was six times brighter than older ways.

CaWO4.tif
CaWO4.tif
It is also used in fluorescent lights. These lights turn ultraviolet light into visible light. You might see it in old TV tubes too. It even helps scientists search for dark matter. It is a small part of a huge world.

364 words

Scheelite is a mineral composed of calcium tungstate. Its chemical formula is CaWO4. This mineral serves as an essential ore for tungsten, also known as wolfram. Because of its importance, scheelite is a key resource for many industrial processes. It can appear as beautiful crystals for collectors or as gemstones. Scientists also use it in advanced technology like lasers and detectors.

CaWO4.tif
CaWO4.tif

The physical structure of scheelite is quite specific. It belongs to the tetragonal crystal system. This means its crystals often form as dipyramidal pseudo-octahedra. These shapes look like two pyramids joined at their bases. Other forms include columnar, granular, tabular, or massive habits. The mineral is quite heavy, with a specific gravity between 5.9 and 6.1. However, it is relatively soft, with a hardness of only 4.5 to 5. Its luster is very high, ranging from vitreous to adamantine. This high luster, combined with its refractive index and dispersion, creates a "fire" similar to a diamond.

Scheelite is famous for its unique light properties. It exhibits fluorescence when exposed to shortwave ultraviolet light. This means the mineral glows under specific light conditions. Most scheelite produces a bright sky-blue glow. If the mineral contains molybdenum as a trace impurity, it may glow green instead. Geologists use this glowing effect as a tool in the field. They look for these blue or green lights to help locate gold deposits.

Bispbergs klack.jpg
Bispbergs klack.jpg

The history of scheelite is tied to Swedish science. It was first described in 1751 at Mount Bispbergs klack in Säter, Sweden. The mineral was named in honor of the Swedish chemist Carl Wilhelm Scheele. Scheele lived from 1742 to 1786. Because the mineral is so heavy, Swedes originally called tungsten "heavy stone." This name eventually became the standard term for the metal itself. The ore was originally called scheelerz before the name changed to scheelite.

Scheelite is found in several different geological environments. It often occurs in contact metamorphic skarns. It also appears in high-temperature hydrothermal veins and greisen. Less commonly, it can be found in granite pegmatites. It is frequently found in tin-bearing veins and sometimes near gold. Many different minerals grow alongside it, such as cassiterite, topaz, and quartz. Notable locations for finding fine crystals include the Czech Republic, Switzerland, and Arizona. Large crystals have even been found in Japan and Connecticut.

Bispbergs klack.jpg
Bispbergs klack.jpg

Humanity has used scheelite for many important scientific breakthroughs. In the late 1800s, Thomas Edison used a calcium tungstate-coated screen for a fluoroscope. This invention made X-ray images six times brighter than previous methods. Previous methods used barium platinocyanide, which helped Wilhelm Röntgen discover X-rays in 1895. Today, scheelite is used in phosphors and scintillators. These materials help detect X-rays and gamma rays. It is also used in fluorescent lighting to convert ultraviolet light into visible light. Even dark matter experiments use calcium tungstate as a scintillator.

CaWO4.tif
CaWO4.tif

Modern technology also uses synthetic scheelite. Scientists use the Czochralski process to create it in a lab. Synthetic scheelite can imitate diamonds or act as a solid-state lasing medium. Gemologists must be careful not to confuse it with natural stones. Natural scheelite usually has internal growth features or tiny imperfections called inclusions. Synthetic versions are often spotless and may contain tiny gas bubbles. Natural stones also show specific absorption lines in the yellow part of the spectrum. These lines are caused by tiny amounts of praseodymium and neodymium.

CaWO4.tif
CaWO4.tif

565 words
🖼️ Images & Media (2)
CaWO4.tif
File:Bispbergs klack.jpg
Bispbergs klack.jpg
Up Next
🌍
Perovskite
Earth Science
More to explore

🔬 Go deeper

More advanced topics to explore

🪜 Step back

Simpler topics to build understanding

What is Nepedia?

A free, ad-free encyclopedia for children. Every article is written at five reading levels, so the same page works for a five-year-old and a fifteen-year-old — use the level switcher above to see this one change. No account needed to read.