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Hillman Hall

December 14, 2018 by wpengine

How Do Geodes Get Their Colors?

geode

Geodes are stones with a secret–at first glance, they seem like nothing more than the grey rocks you might see on walk around your neighborhood. Then–crack!–once they’re broken open, they reveal their inner beauty: a tiny cave filled with some of the world’s most spectacular, colorful crystals.

Born out of lava

Geodes are formed when there are pockets of air within rocks. This often happens after volcanic eruptions when lava cools around air bubbles. These pockets leave space for groundwater to seep in. But the water itself doesn’t produce geodes–it brings along minerals which stay in the rock even after the water evaporates. The minerals then start to build on each other to form crystals. It can take thousands or even millions of years for these crystals to form. The larger the crystals are, the older the geode is.

So what gives them their color?

geode

The same minerals that form crystals can give them their glorious colors. Additional elements can also make their way into the mix and provide their own unique shades. Iron will give crystals a red or purple color, titanium will create blue, nickel or chromium leads to green, and manganese produces pink crystals.

While geodes can be naturally colorful some are artificially dyed. These dyed stones often have a brighter, more intense color than what appears naturally. Why do people dye geodes? Colorful geodes tend to sell well and can be a cheap way to imitate rare stones.

Come to the museum and check out the geodes of various colors on display in Hillman Hall of Minerals and Gems.

Explore nature together.  Visit Nature 360 for more activities and information.

Filed Under: Blog Tagged With: Education, gems and minerals, Hillman Hall, Hillman Hall of Minerals and Gems, minerals, Nature 360

December 13, 2018 by wpengine

A Perfect Mineral for the Christmas Season

by Debra Wilson

How can you decorate a mineral for Christmas? If it’s the right mineral, all you need to do is shine a SWUV (short wave ultraviolet) light on it. Such is the case with a mineral that is known as “Christmas Ore.” Under normal light it looks like kind of a drab rock as the one in this photo does.

Christmas ore

This specimen of calcite (tan color), willemite (brown color) and franklinite (black color) is on display in Hillman Hall of Minerals and Gems in the Fluorescence & Phosphorescence exhibit and was donated by the Sterling Hill Mining Museum for this exhibit. It originated from the Sterling Hill mine in Ogdensburg, in the Franklin Mining District of New Jersey. When you shine the SWUV light on it you will see why it is called “Christmas Ore” because it glows with the colors of Christmas. The calcite glows a bright red and the willemite glows a bright green, as you can see in this photo.

christmas ore

This glowing is known as fluorescence and the Franklin Mining District is known as the fluorescent capital of the world. The Franklin and Sterling Hill ore bodies are the source of at least 350 mineral species.At present, over 80 fluorescent mineral species are known from the area. Willemite and calcite are the most common fluorescents in these ore bodies and are known as “Christmas Ore” when they occur together in the same specimen.

So, what causes the fluorescence? Fluorescence usually occurs when specific impurities known as “activators” are present within the mineral. These activators are typically cat ions of metals such as: tungsten, molybdenum, lead, boron, titanium, manganese, uranium and chromium. Rare earth elements such as europium, terbium, dysprosium, and yttrium are also known to contribute to the fluorescence phenomenon. Fluorescence can also be caused by crystal structural defects or organic impurities. Calcite (CaCO3) and willemite (Zn2SiO4) are examples of minerals that in their pure state do not fluoresce but add a little divalent manganese (Mn2+) and they will fluoresce red and green, respectively.

There are two other specimens of calcite and willemite, also from the Franklin District, in the Fluorescence & Phosphorescence exhibit, shown here under normal light and under SWUV light.

Christmas ore
christmas ore
christmas ore
Christmas ore

Come to Hillman Hall of Minerals and Gems to hear a more detailed explanation of the phenomenon of fluorescence and see all 21 specimens in the exhibit from world-wide localities that glow under the ultraviolet lights.

Debra Wilson is the Collection Manager for the Section of Minerals at Carnegie Museum of Natural History. Museum employees are encouraged to blog about their unique experiences and knowledge gained from working at the museum.

Related Content

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Thanksgiving and Nutritional Mineralogy

Ask a Scientist: Why do some minerals glow?

Carnegie Museum of Natural History Blog Citation Information

Blog author: Wilson, Debra
Publication date: December 13, 2018

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Filed Under: Blog Tagged With: Deb Wilson, gems and minerals, Hillman Hall, Hillman Hall of Minerals and Gems, minerals, minerals and gems, Section of Minerals

March 1, 2018 by wpengine

Section of Minerals Collection Manager, Deb Wilson, attends…

copper specimen

copper specimen purchased at the show

Deb Wilson at the show

visitors browsing the gem and mineral show

Deb Wilson with other visitors to the show

Section of Minerals Collection Manager, Deb Wilson, attends the Tucson Gem and Mineral Show every year. This year Deb Wilson acquired a beautiful piece of copper that was mined out of Bisbee, Arizona in 1910, which is now on display in Hillman Hall of Minerals and Gems.

 

Filed Under: Blog Tagged With: Deb Wilson, Hillman Hall, minerals

January 1, 2018 by wpengine

You can probably guess where this “grape” agate gets its name….

“grape” agate, a purple mineral that looks like a cluster of small balls

You can probably guess where this “grape” agate gets its name. It is now on display at Carnegie Museum of Natural History.

(Photo by Debra Wilson) 

Filed Under: Blog Tagged With: gems and minerals, Hillman Hall, minerals

December 7, 2017 by wpengine

A Couple of Rock Stars

Deb and Marc standing in front of a mineral display case with their prize ribbons
Above: Deb (left) and Marc (right) Wilson celebrate award for best museum exhibit at the 2017 Tucson Gem and Mineral Show.

After 25 years at Carnegie Museum of Natural History, Curator of Collections for the Section of Minerals, Marc Wilson, retired in August 2017. Marc began managing the museum’s impressive mineral and gem collection in 1992 and greatly improved the collection and exhibition halls during his tenure.

In 2007 Hillman Hall of Minerals and Gems was renovated and expanded with the addition of Wertz Gallery: Gems and Jewelry. He received the Friends of Mineralogy Award of Merit and was recognized as EFMLS Honoree for the 2001 AFMS Scholarship Award. He was inducted into the National Rockhound and Lapidary Hall of Fame in 2001 and served as a consulting editor for Rocks & Minerals since 1998. Collection Assistant Debra Wilson will now serve as Collection Manager for the Section of Minerals at Carnegie Museum.

Congrats to both Marc and Deb!

Filed Under: Blog Tagged With: Deb Wilson, gems and minerals, Hillman Hall, minerals, Wertz Gallery

November 13, 2017 by wpengine

Remember the Poppy Scene in Wizard of Oz?

Poppy jasper, a vibrant, reddish mineral
(photo by Debra Wilson)

Remember the Poppy Scene in Wizard of Oz?

These poppies are not going to put anyone to sleep.

Poppy jasper is a vibrant, reddish variation of brecciate jasper. This piece is on display in Wertz Gallery of Gems and Jewelry.

When quartz is impure and opaque, it is called jasper.

Filed Under: Blog Tagged With: gems and minerals, Hillman Hall, quartz

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