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The man-made glass with a metallic sparkle and the source of the word 'aventurescence.'
Author: Hobart M. King, PhD, GIA Graduate Gemologist
It’s created by air-puffing volcanic glass to create an extremely light and porous material. It has one of the best oxygen retention levels of all growing media because of how porous it is. Its weight can be a downside in certain hydroponic systems where water interacts directly with the growing media, causing it to shift around and wash away. Burns Green Obsidian RARE Lapidary Rough 1lb. OBSIDIAN ROUGH DAMASCUS OBSIDIAN ROUGH VOLCANIC GLASS BANDED OBSIDIAN 2LB 5OZ. $11.80 shipping. Mahogany Obsidian Free Form Oregon 40 grams Lapidary Rough Display. The most common color of uranium glass is pale yellowish-green, which in the 1930s led to the nickname 'Vaseline glass' based on a perceived resemblance to the appearance (which was a yellow-green color) of Vaseline brand petroleum jelly as formulated and commercially sold at that time. Well Kimberly, one of your three names (obsidian/volcanic/glass) is correct. To me, it looks like a piece of green glass that fell off a ship and got tumbled around in the Great Lakes before washing up on shore. Usually, green obsidian is more gray/green in colour and very opaque; the Burns green obsidian in. 15376 (4) Green Volcanic Glass. Clods of green glass (numbered 15365 to 15377) were collected as part of a rake sample around Spur crater and the “soil” from this bag (15310 to 15314) also contained a lot of green glass fragments due to abrasion. Other clods were grouped and numbered 7.
Goldstone Cabochons: The bright reflective sparkle of goldstone is what makes it a popular man-made gem material. These blue and reddish brown goldstone cabochons are about 20 x 28 millimeters in size.
What Is Goldstone?
Goldstone is a man-made colored glass that contains abundant, flat-faced, highly reflective inclusions. The reflective inclusions have a bright metallic luster, and their glittering appearance immediately attracts attention. This exciting appearance has made goldstone a popular man-made gem and sculptural material. It is often cut into cabochons, hearts, beads, spheres, pendulums, arrowheads, and small sculptures. It is a popular material for making tumbled stones.
Goldstone is produced in a variety of colors. Reddish brown, the original color, is the least expensive and the most commonly encountered variety of goldstone. Dark green, dark blue, and dark purple goldstone are also produced.
Table of Contents
|What Is Goldstone?|
What Causes Goldstone's Glittery
Appearance and Color?
'Aventurine Glass' and Aventurescence
Tumbled Goldstone: Pieces of reddish brown, blue, and green goldstone that have been shaped and polished in a rock tumbler. These pieces are approximately 20 to 25 millimeters along their maximum dimension.
What Causes Goldstone's Glittery Appearance and Color?
The glittery appearance of goldstone is often attributed to 'bits of copper' or 'copper filings' that have been added to the glass. That simplistic description is incorrect.
Reddish brown goldstone is made by heating molten glass to a temperature that is hot enough to dissolve granules of copper oxide that are added to the melt. After the copper oxide is completely dissolved, the melt is allowed to cool very slowly. This slow cooling gives copper ions in the melt adequate time find one another and grow into octahedral-shaped copper crystals. The slower the cooling, the larger the copper crystals.
Copper Crystals in Goldstone: You are looking through a microscope at a polished surface of reddish brown goldstone. A bright light is shining down onto the surface of the goldstone. The triangular faces of octahedral copper crystals are reflecting the light back at you from various depths below the polished surface of the transparent glass. The largest triangular crystal face seen in this view is about 0.1 millimeters from apex to base.
The bright metallic luster of these copper crystals is what produces the sparkling appearance of goldstone. An octahedral crystal has eight triangular faces. If you look at goldstone with a microscope under reflected light, you will see triangular faces of the copper crystals reflecting the light back at you from various depths below the surface of the glass. See the accompanying image.
The glass of reddish brown goldstone is colorless. Its reddish brown appearance is caused by reflections from the included copper crystals. Blue, green, and purple goldstone are made using compounds of metals other than copper. The color of these goldstones is caused by the color of the glass rather than the color of the reflections from the metallic crystals. The glass color of blue goldstone is caused by cobalt, green is caused by chromium, and purple is caused by manganese.
Reflections from the metallic crystals within the goldstone attract attention and give goldstone its sparkling appeal. The sparkling appearance of the reflections is intensified in three situations: 1) when the goldstone is moved under incident light; 2) when the light source is moved; and, 3) when the eye of the observer is moved.
Aventurine: A cabochon cut from a piece of quartz that contains an enormous number of tiny fuchsite inclusions. Fuchsite is a green chromium-rich mica that gives the quartz its green color. The inclusions share a common orientation, and when the light strikes the cabochon at the proper angle, they simultaneously reflect a flash of light to the observer. The reflectance is known as aventurescence, and the material was named 'aventurine.'
'Aventurine Glass' and Aventurescence
Before the name 'goldstone' was used, the material was widely known as 'aventurine glass.' That name is the source of three words that are commonly seen in gemology.
- 'Aventurescence' is the name of a phenomena that is produced when a material has light-reflecting particles that produce a sparkly or glittery luster.
- 'Aventurescent' is an adjective used for materials that exhibit the phenomena of aventurescence. Examples are aventurescent quartz, aventurescent feldspar and aventurescent iolite.
- 'Aventurine' is a noun used for a variety of green quartz that contains tiny highly reflective flakes of a green chromium-rich mica known as fuchsite. The reflective flakes of fuchsite produce the aventurescent luster and impart a green color to the material.
Related:Elements of Color in Glass
The earliest known object made from a goldstone-like material is an amulet excavated in Iran and dated to be from the 12th to early 13th century.  The beginning of modern aventurine glass production began in Murano, Italy during the 17th century.  It has been produced there, with some interruptions, up to the present time.
A few decades after manufacturing began in Italy, Chinese glassmakers were also producing items made from aventurescent glass. The Imperial Workshop was making aventurine glass bottles that were given as gifts and rewards by the Qing court.  Today, much of the goldstone being sold as a gem and lapidary material is coming from factories in China. If you visit Ebay or Alibaba, you will see sellers disclosing that the goldstone offered for sale has been made in China.
Goldstone Rough: This is a large chunk of goldstone rough that measures about 8 inches across. Some parts of this specimen would be suitable for use in lapidary projects. However, other areas are clearly not as desirable. On the left side, you can see some slag and areas without visible sparkle. This specimen is a good example of how the quality of goldstone can vary greatly even within the same batch. Click to enlarge image.
Rough goldstone is usually sold as broken chunks and as slabs suitable for cutting cabochons. The chunks range from small pieces used for rock tumbling to large pieces weighing over 50 pounds. Although goldstone is a man-made material, it varies greatly in quality, appearance, and suitability for use in making cabochons, tumbled stones and other objects. The buyer needs some knowledge of how goldstone is made to make an intelligent purchase.
Goldstone is made in a large heated vessel that might produce 100 pounds of material or more. After it has been heated and held at the proper temperature, the glass is allowed to cool slowly. Slow cooling allows time for the reflective metallic crystals to grow to a large size.
Green Volcanic Glass Obsidian
The batch cools fastest near the outside of the vessel. The smallest crystals in the batch are usually found near the wall of the vessel because that is where the rapid cooling occurs. There, the crystals can be too small to produce the desirable glittering effect that gives goldstone its appeal. The crystals usually grow progressively larger towards the center of the vessel, where cooling is slowest.
|  Goldstone Amulet from 12th Century Iran, webpage on the Metropolitan Museum of Art website, accessed November 2017. |
 Murano, Its Glass and Its People, article on the Delaware Valley Paperweight Collectors Association website, accessed November 2017.
 Snuff Bottle with Aventurine Stopper, webpage on the Metropolitan Museum of Art website, accessed November 2017.
Within a batch, the glass can have areas with few visible crystals, areas with numerous gas bubbles, and areas of slag. All of these areas are unsuitable for use, and any buyer who is paying by the pound should make sure that the price paid does not include the weight of useless material.
So, if you are buying rough goldstone, pay attention to crystal size, the presence of areas without crystals, the presence of gas bubbles, and areas of slag. Slag, bubbles, and areas lacking flash will be unusable as 'goldstone.' Also, some goldstone only exhibits aventurescence from two directions instead of from all directions.
It is best to buy goldstone where you can inspect the rough from all angles in directional light. The next best way is when you can see photos of the piece that you are going to buy from multiple directions with views that are close enough to see the flashing crystals. Buying chunks or lots of goldstone shown in a single photo or sight-unseen from an internet vendor is a risky spend of hard-earned money.
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Apollo 15 yellow-brown volcanic glass: Chemistry and petrogenetic relations to green volcanic glass and olivine-normative mare basalts
Apollo 15 yellow-brown glass is one of twenty-five, high-Mg, primary magmas emplaced on the lunar surface in pyroclastic eruptions. Forty spherules of this glass were individually analyzed by electron microprobe and INAA for major- and trace-elements ( e.g. Sc, V, Cr, Co, La, Ce, Nd, Sm, Eu, Ho, Tm, Yb, Lu, Hf, Ta, and U). The abundances demonstrate that this primary magma was produced by partial melting of differentiated cumulates in the lunar mantle. Models are developed to explain the possible source-regions of several Apollo 15 and Apollo 12 low-Ti mare magmas as being products of hybridization involving three ancient differentiated components of a primordial lunar magma ocean: (a) early olivine ± orthopyroxene cumulates; (b) late-stage clinopyroxene + pigeonite + ilmenite + plagioclase cumulates; and (c) late-stage inter-cumulus liquid. Isotopic constraints on Sm-Nd fractionation and least-squares tests of potential mixing models require models of Apollo 15 yellow-brown glass, and Apollo 12 and 15 olivine mare basalts, involving low F ~3% cumulate remelting of sources in which olivine and orthopyroxene are residual phases. Models of the Apollo 15 green glass composition indicate higher (~4-7%) degrees of melting, but with only a slight preference for orthopyroxene-rich relative to orthopyroxene -free sources. The modeled dependence on residual orthopyroxene in mare source regions places source depths at ~400 km or greater in order to maintain olivine and orthopyroxene on the liquidus. Hybridization at such depths would likely result from convective overturn of the primordial magma ocean and suggests that separate fractionating masses were positioned at various depths. Our models for developing hybridized source regions of primary low-Ti mare magmas do not require selective contamination of primary liquids. The preferred model for Apollo 15 yellow-brown glass is presented as the commingling of 95% early cumulate olivine + orthopyroxene, 1.9% clinopyroxene, 0.27% pigeonite, 1.7% plagioclase, 0.02% ilmenite, and 0.56% trapped liquid. Respective proportions for the Apollo 15 olivine mare basalt source model are 98.5%, 0.37%, 0%, 0.79%, 0.16%, and 0.13%; and the proportions used for the preferred Apollo 12 olivine mare basalt model are 97.6%, 0.73%, 0.24%, 0.77%, 0.42%, and 0.21%. Our preferred model for the green glass source composition ( F = 0.07) requires the commingling of 97.4% early olivine + orthopyroxene, 0.18% clinopyroxene, 1.32% pigeonite, 0.85% plagioclase, and 0.28% trapped liquid.
Green Volcanic Glass Value
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Green Volcanic Glass
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