Very fine grained fault rock which is composed of glassy matrix that often contains inclusions of wall-rock fragments. 0
From pseudo- + tachylite, a glassy rock generated by frictional heat within faults. 0
Durable Rock, Hard Rock 0
Fine Grained Rock, Opaque Rock 0
Black, Brown, Colourless, Green, Grey, Pink, White 0
Decorative Aggregates, Entryways, Interior Decoration 0
As Building Stone, As Facing Stone, Garden Decoration 0
As Dimension Stone, Cement Manufacture, for Road Aggregate, Making natural cement 0
Creating Artwork, Gemstone 0
Archaeological Significance
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Due to change in environmental conditions, rocks are heated and pressurized deep inside the Earth's surface. Pseudotachylite is formed from the extreme heat caused by magma or by the intense collisions and friction of tectonic plates. 0
Iron Oxides, Pyroxene, Quartz, Stishovite, Sulfides 0
Carbon Dioxide, Silicon Dioxide, Sulfur Dioxide, Sulphur 0
Burial Metamorphism, Cataclastic Metamorphism, Contact Metamorphism 0
Transparent to Translucent 0
Deposits in Eastern Continents
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Great Britain, Switzerland 0
Deposits in Western Continents
0
Deposits in Oceania Continent
0
Central Australia, Western Australia 0
Information about Pseudotachylite
Rocks are naturally occurring solids which are composed of minerals & have been used by humans since ages. From Stone Age, rocks are used for various purposes. Also, the metals and minerals found in rock play an important role in our life. Get to know all the Pseudotachylite Uses. We have provided you with all information about Pseudotachylite rock here. Very fine grained fault rock which is composed of glassy matrix that often contains inclusions of wall-rock fragments.. Pseudotachylite is available in black, brown, colourless, green, grey, pink, white colors. The streak of a rock is the color of powder produced when it is dragged across an unweathered surface. The streak of Pseudotachylite is light to dark brown. Get to know more about Pseudotachylite rock and characteristics of Pseudotachylite rock in the next sections.