Scoria is a highly vesicular
, dark-colored volcanic rock
that may or may not contain crystals (phenocryst
s). It is typically dark in color (generally dark brown, black or purplish red), and basalt
ic or andesitic
in composition. Scoria is relatively low in density
as a result of its numerous macroscopic ellipsoidal vesicles, but in contrast to pumice
, all scoria has a specific gravity
greater than 1, and sinks in water. The holes or vesicles form when gases that were dissolved in the magma
come out of solution as it erupts, creating bubbles in the molten rock, some of which are frozen in place as the rock cools and solidifies. Scoria may form as part of a lava flow, typically near its surface, or as fragmental ejecta (lapilli
, blocks and bombs), for instance in Strombolian eruption
s that form steep-sided scoria cone
s. Chemical analysis of scoria found in Yemen
showed that it was mainly composed of volcanic glass with a few zeolites
). Most scoria is composed of glassy fragments, and may contain phenocrysts
. The word ''scoria'' comes from the Greek
σκωρία, ''skōria'', rust. A colloquial term for scoria is cinder
[Jackson, J.A., J. Mehl, and K. Neuendorf (2005) ''Glossary of Geology'' American Geological Institute, Alexandria, Virginia. 800 pp. ] [McPhie, J., M. Doyle, and R. Allen (1993) ''Volcanic Textures A guide to the interpretation of textures in volcanic rocks'' Centre for Ore Deposit and Exploration Studies, University of Tasmania, Hobart, Tasmania..198 pp. ]
Scoria differs from pumice
, another vesicular volcanic rock, in having larger vesicles and thicker vesicle walls, and hence is denser. The difference is probably the result of lower magma viscosity, allowing rapid volatile diffusion, bubble growth, coalescence, and bursting.
As rising magma encounters lower pressures, dissolved gases are able to exsolve
and form vesicles. Some of the vesicles are trapped when the magma chills and solidifies. Vesicles are usually small, spheroidal and do not impinge upon one another; instead they open into one another with little distortion.
s of scoria can be left behind after eruptions, usually forming mountains with a crater at the summit. An example is Maungarei
, New Zealand
, which like Te Tatua-a-Riukiuta
in the south of the same city has been extensively quarried. Quincan, a unique form of Scoria, is quarried at Mount Quincan
in Far North Queensland
Scoria has several useful characteristics that influence how it is used. It is somewhat porous, has a high surface area and strength for its weight, and often has striking colours. Consequently, it is often used in landscaping and drainage works. It is also commonly used in gas barbecue grills.Rock Types and Rocks Found in Michigan
Scoria can be used for high-temperature insulation. It is also used on oil well sites to limit mud problems resulting from heavy truck traffic.
The quarry of Puna Pau on Rapa Nui/Easter Island was the source of a red-coloured scoria which the Rapanui people used to carve the pukao (or topknots) for their distinctive moai statues, and even to carve some moai themselves.
It is also used as a traction aid on ice- and snow-covered roads.
File:Scoria AmsterdamIsland 5.jpg|Fresh scoria sometimes has a blue sheen to its surface.
File:Multi-coloured scoria in the Tarawera rift.jpg|Scoria of various hues exists on Mount Tarawera, from its 1886 eruption.
File:VeyoVolcano.jpg|Holocene scoria-producing volcano near Veyo, Utah
File:LvMS-Lvm.jpg|Photomicrograph of a volcanic lithic fragment (sand grain) derived from scoria; upper picture is plane-polarized light, bottom picture is cross-polarized light, scale box at left-center is 0.25 millimeter.
File:Scoria at Akyia-kaigan coast, Ama (3).jpg|Red scoria cliffs at Akyia-kaigan coast in the Oki Islands, Japan. It was erupted 2.8 million years ago.
File:PointMuguCA IgneousRock 20170911.jpg|Scoriaceous boulder near Point Mugu, California.
File:Pine trees growing on the slope of Cinder Cone.jpg|Pine trees growing on the slope of Cinder Cone in Lassen Volcanic National Park.
*Extrusive rock – Igneous rock formed by rapid crystallization at the surface
Category:Glass in nature