The correct term for this type of break is a conchoidal fracture. The way obsidian breaks is very similar to glass. One respected geologist describes it as "a congealed liquid with impurities of rock and a limited number of microscopic crystals". Most magma contains at least 70% silicon dioxide which is the main constituent of obsidian.Īlthough often referred to as a 'stone' that's not quite accurate but finding a more appropriate word to describe obsidian is difficult. Shungite is estimated to be at least two billion years old, zircon is around 4.4 billion years old. When compared to the age of many rocks and minerals that's relatively young. Obsidian is rarely older than about twenty million years. The glass that subsequently forms will often be free from dirt, ash and other impurities. These tend to be close to the vent of the volcano. Some of the finest obsidian forms beneath the surface of the earth as molten magma seeps between fractures in rocks. The word amorphous is also used to describe a naturally occurring non crystalline solid. Other mineraloids include jet, amber, moldavite, pearl and opal. These materials which include obsidian are known as mineraloids. The resulting hardened material is volcanic glass also known as obsidian.Ī material that's not crystalline (no crystals present) is not a mineral. They may start forming after a few weeks but will at best be microscopic. Once spewed out from the vent of a volcano it's known as lava.Īlthough lava initially cools fairly rapidly after being expelled, it has insulating properties so the cooling process slows down significantly over time.Ĭrystals do not have time to grow if lava cools very fast as in hours to days. Magma is molten rock from beneath Earth's surface. This burning hot material then cools so rapidly against air, water or rocks that crystals do not have time to grow. Obsidian is natural volcanic glass produced as magma erupts onto Earth's surface. Obsidian Meaning Properties Facts and Photos Contents
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