Foidolite is a rare type of coarse-grained intrusive igneous rock with a feldspathoid mineral content greater than 60%
From the mineral feldspathoid which is the main content of rock
Coarse Grained Rock, Fine Grained Rock, Medium Grained Rock, Opaque Rock
Black, Brown, Green, Grey, Pink, White
Decorative Aggregates, Interior Decoration
As Building Stone, As Facing Stone, Garden Decoration, Paving Stone
As Dimension Stone, Cement Manufacture, for Road Aggregate
Taken as a Supplement for Calcium or Magnesium
Artifacts, Monuments, Sculpture
Cemetery Markers, Commemorative Tablets, Creating Artwork
Archaeological Significance
Foidolites is a fine-grained, hard rock which is a type of metasomatite, essentially altered basalt. It forms with or without crystallization, either below the surface as intrusive rocks or on the surface as extrusive rocks.
Amphibole, Biotite, Feldspar, Olivine, Plagioclase, Pyroxene
Aluminium Oxide, CaO, Iron(III) Oxide, FeO
Burial Metamorphism, Cataclastic Metamorphism, Hydrothermal Metamorphism, Impact Metamorphism
Medium to Fine Coarse Grained
Heat Resistant, Wear Resistant
Deposits in Eastern Continents
South Africa, Western Africa
Deposits in Western Continents
Deposits in Oceania Continent
Central Australia, Western Australia
Information about Foidolite
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 Foidolite Uses. We have provided you with all information about Foidolite rock here. Foidolite is a rare type of coarse-grained intrusive igneous rock with a feldspathoid mineral content greater than 60%. Foidolite is available in black, brown, 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 Foidolite is white. Get to know more about Foidolite rock and characteristics of Foidolite rock in the next sections.