Used as a construction stone for thousands of years.
Article by: Hobart M. King, Ph.D., RPG
What is Diabase?
In the United States and Canada, the name "diabase" is used for a dark gray to black, fine-grained, intrusive igneous rock that has a composition similar to basalt and gabbro. The difference between basalt, diabase, and gabbro is in their grain size - which was determined by their cooling rates.
Basalt: rapid cooling in a lava flow produced individual crystals that are so small they are difficult to see with the unaided eye.
Diabase: slower cooling in shallow intrusions such as sills, dikes, lopoliths or laccoliths allowed individual crystals to grow slightly larger - up to about two millimeters in size.
Gabbro: slowest cooling below Earth's surface gave crystals a longer time to grow - some may be over a centimeter across or larger.
In the United Kingdom and a few other countries diabase is known as "dolerite". The two words are synonyms
Mineral Composition of Diabase
Diabase typically has a mineral composition that is dominated by the plagioclase feldspar known as labradorite (approximately 40% to 70% of the rock). Most of the remainder is made up of pyroxene minerals (usually augite). Minor amounts of hornblende, olivine, magnetite, and quartz can be found in some diabase rocks.
Although the mineral species present in diabase often have perfect cleavage, when they are present in tiny interlocking grains, the cleavage is usually not an important durability concern when the rock is used as a construction material.
Here are two facts about diabase and its commercial use:
1) The plagioclase in diabase is often of the labradorite variety. Diabase from some quarries contains abundant crystals of labradorite that are capable of producing colorful reflections known as "labradorescence". When cut and polished, this diabase can serve as an attractive architectural stone.
2) The pyroxene minerals in diabase, as well as the feldspars will form a weathering rind when exposed to the elements. So, an initially black construction stone can alter to a chalky white, gray, or tan color. This should be expected unless the stone has been polished, treated, or used in a location not exposed to the elements.
Some igneous rocks have a complex cooling history that results in them containing grains of distinctly different crystal sizes. These rocks, with large crystals (known as "phenocrysts") suspended in a matrix of fine crystals (known as "groundmass"), often have a cooling history similar to the following description:
The parent magma of the rock began cooling slowly, deep underground, and some large crystals of minerals with a high crystallization temperature began to form there. The magma was then erupted to the surface or moved to a shallow location, such as a dike or sill, where the next, and often the final, part of its cooling occurred. The cooling rate at this shallow depth was faster and the groundmass of the rock is composed of small crystals of minerals that have a lower cooling temperature.
Much diabase contains two distinctly different crystal sizes and is known as "diabase porphyry". When cut and polished, it can make an interesting and attractive stone for use in tiles, countertops, window sills, stair treads, facing stone or other uses.
Problems Identifying Diabase
The fine-grained texture of diabase makes identification in the field or in a classroom a difficult undertaking. The observer must have enough skill to view the physical properties of tiny mineral grains, and enough knowledge to identify the minerals. Getting a confident identification in these locations can be difficult.
Diabase is best identified in thin section with a petrographic microscope, with x-ray diffraction, or with other instruments that can identify the component minerals and their relative abundances. So, many people take the easy way out and call the unknown specimen "trap rock" (a layman’s name that fits a number of dark, fine-grained igneous rocks) or take a chance of declaring an incorrect scientific name. When you hear the name "diabase" examine to confirm if the name of the rock is important.
Geologic Occurrence of Diabase
The formation of diabase has two requirements:
1) a basaltic magma source
2) shallow emplacement and cooling in a relatively small subsurface structure such as a sill, dike, lopolith or laccolith.
Explanations, illustrations, and photos of these structures can be found in this article.
Uses of Diabase
Most diabase that is mined is used in the construction industry. There are several types of use:
1) Crushed Stone: Diabase is one of many types of "trap rock" used as crushed stone in the construction industry. These are durable rocks that have many uses. For most of these uses, the aggregate must meet certain specifications of abrasion resistance, weathering resistance, and crush resistance. Example uses include:
a subbase in highway construction|
a base layer in concrete slab construction
an aggregate in concrete
an aggregate in asphalt paving material
drainage stone in and around foundations
filter stone in sewage disposal drain fields
unpaved road surfaces
2) Dimension Stone: Diabase can be cut or sheared into blocks of specific or random sizes. These are some categories of diabase use:
a) Building Stone: block-shaped pieces used as the structural elements of foundations, walls, abutments, ashlars, etc.
b) Architectural Stone: special-shape pieces used as stair treads, window lintels, window sills, counter tops, flooring tiles, facing stone, columns, etc. When used as an architectural stone, diabase is often called by the trade term "black granite". (In the dimension stone trade, the word "granite" is used for any feldspar-bearing rock with interlocking crystals that are large enough to be seen with the unaided eye.)
c) Paving Stone: pieces cut for use as patio stones, curbing, pavé, etc.
d) Monument Stone: dimensional stone cut for use as monuments, burial markers, gateways, directories, memorials, etc.
Diabase in Stonehenge
Diabase played an important role in the construction of Stonehenge, one of the most famous and recognizable stone structures in human history. The diabase “bluestone” pillars that were initially used for the structure’s inner circle were brought to the site around 2100 BC - about 4,000 years ago.
Stonehenge was built in Wiltshire, England, but the diabase pillars came from the Carn Meini Quarry in the Preseli Mountains of southwestern Wales. The pillars weighed up to 4.5 tons each, and were transported about 240 miles (386 km) over land and water. Needless to say, it was a monumental task to bring about 80 of these large, heavy stones across such a great distance. To warrant this effort, a special significance must have been placed on this particular type of rock.
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