Basalt (40 Photos): What Is It? The Origin Of The Stone, What Kind Of Rocks Does Basalt Belong To And What Does It Look Like? Density, Mats, Fabric And Other Uses

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Video: Basalt (40 Photos): What Is It? The Origin Of The Stone, What Kind Of Rocks Does Basalt Belong To And What Does It Look Like? Density, Mats, Fabric And Other Uses

Video: Basalt (40 Photos): What Is It? The Origin Of The Stone, What Kind Of Rocks Does Basalt Belong To And What Does It Look Like? Density, Mats, Fabric And Other Uses
Video: IgnRx-How to Observe and Name Scoria and Basalt Igneous Rock 2024, April
Basalt (40 Photos): What Is It? The Origin Of The Stone, What Kind Of Rocks Does Basalt Belong To And What Does It Look Like? Density, Mats, Fabric And Other Uses
Basalt (40 Photos): What Is It? The Origin Of The Stone, What Kind Of Rocks Does Basalt Belong To And What Does It Look Like? Density, Mats, Fabric And Other Uses
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Basalt is a natural stone, an effusive analogue of gabbro. From the material in this article, you will learn what it is, what it happens, what its origin and properties are. In addition, we will tell you about its areas of application.

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What it is?

Basalt is an effusive igneous rock that belongs to the main composition of the normal alkalinity series of the basalt group. Translated from the Ethiopian language, "basalt" means "boiling stone" ("iron-containing") . Basalt has a complex structure from a chemical and mineralogical point of view. Crystalline formations and fine-grained suspensions of magnetite, silicates and metal oxides are intertwined in it.

The structure of the mineral consists of amorphous volcanic glass, feldspar crystals, sulfide ores, carbonates, quartz. Agvite and feldspar form the basis of the mineral.

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Volcanic rock looks like an interstratal body, it is found as a lava flow that occurs after a volcanic eruption . This stone is black, smoky black, dark gray, green and black. Depending on the variety, the structure may differ (it can be aphyric, porphyry, glass wool, cryptocrystalline). The mineral has a rough surface and uneven edges.

The bubbling structure of the material is explained by the release of vapors and gases during the cooling of the lava . The cavities in the ejected mass do not have time to tighten before it crystallizes. Various minerals (calcium, copper, prenite, zeolite) are deposited in these holes. Basalt is easily distinguishable from other rocks. It is mined by the open method - by grinding out blocks from quarries.

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Origin and deposits

Most basalts form in mid-ocean ridges, forming oceanic rock. It is produced above ocean hotspots. When a volcano erupts, a large volume of lava flows through the continental crust to reach the ground . It is formed when lava solidifies with sub-air lava flows and ash.

The breed is characterized by its thin build and uniformity. The conditions for the solidification of magma are different. The characteristics of the stone depend on the physicochemical conditions of melting (pressure, the rate of cooling of the lava flow), as well as the way of the melt leaving . The newest view is that basalt is found everywhere. According to their geodynamic origin, minerals are mid-oceanic, active continental margins, and intraplate (continental and oceanic).

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Basalt is widespread not only on Earth, but also on other planets (for example, the Moon, Mars, Venus). The stone forms a hard shell of the Earth: under the oceans - in the range of 6,000 m and more, under the continents, the thickness of the layers reaches 31,000 m. Rock outcrops to the Earth's surface are numerous:

  • its deposits are found in the north, west, southeast of Mongolia;
  • it is widespread in the Caucasus, Transcaucasia, in the northern part of Siberia;
  • natural stone is mined in the vicinity of the volcanoes of Kamchatka and the Kuriles;
  • its exits to the surface of the Earth are in Auvergne, Bohemia, Scotland, Ireland, Transbaikalia, Ethiopia, Ukraine, Khabarovsk Territory;
  • it is found on the islands of Saint Helena, Antilles, Iceland, the Andes, India, Uzbekistan, Brazil, Altai, Georgia, Armenia, Volyn, Mariupol, Poltava districts of the Ukrainian SSR.

Basalt composition can vary from hydrothermal processes. Moreover, the basalts, which are poured onto the seabed, change more intensively.

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Basic properties

Igneous extrusive rock is characterized by a fine-grained and dense structure. Basalt is similar in its characteristics to granite and marble . It is resistant to acids and alkalis, but may have an increased background radiation. Inert to temperature fluctuations, has heat-saving and fireproof properties. The rock is distinguished by its high weight (heavier than granite), plasticity and flexibility, it has good noise reduction, a high level of vapor permeability, strength, and hardness. Density is not constant as it depends on the texture. It can vary between 2520-2970 kg per m3.

The porosity coefficient can range from 0, 6-19%. Water absorption varies from 0.15 to 10.2% . Basalt is durable, it is not electrified, and due to its hardness it is resistant to abrasion. It melts at a temperature of 1100-1200 degrees Celsius. The hardness on the Mohs scale ranges from 5 to 7. The properties of natural stone make it suitable for use in construction. It can be crushed and remelted, cast, heat treated.

Recycled basalt has the properties of an improved stone . It is difficult to break, in unannealed form it looks like glass (it has a shiny fracture, a brownish-black tint and is fragile). After annealing, it acquires a beautiful dark color, matte fracture and the viscosity of a natural mineral.

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Description of species

Basalt classification depends on various attributes (for example, color, texture, density, chemical composition, mining location). The color of the stone is often dark, light is rare in nature . In terms of mineral composition, the rock is ferrous, ferrobasalt, calcareous and alkaline-calcareous. According to the chemical composition of the ore, it is divided into 3 types: quartz-normative, nepheline-normative, hypersthene-normative. Varieties of the first type are distinguished by the predominance of silica. Its content in the minerals of the second group is low. Still others are distinguished by a low content of quartz or nepheline.

According to the peculiarities of the mineral composition, it is apatite, graphite, dialagic, magnetite . According to the composition of the minerals themselves, it can be anorthite, labradoric. Based on the content of mineral suspensions cemented by the basis, basalts are plagioclase, leucite, nepheline, melilite.

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According to the degree of decorativeness, basalt is divided into several groups. Of these, 4 types of stone are the most popular.

The Asian mineral is characterized by a dark gray (asphalt) shade . It is used as a budget interior and exterior decoration.

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Moorish is highly decorative , is distinguished by a pleasant dark green color with randomly located blotches of different tones. Due to its lower hardness and frost resistance, it is used only for interior decoration.

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The twilight appearance of basalt is gray or black . It belongs to expensive varieties of universal stone, supplied from China. Possesses increased resistance to temperature shocks and moisture.

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Basalt is an impact-resistant and durable mineral for interior and exterior decoration . It is expensive, it is supplied to Russia from Italy. It is considered the most expensive type of natural stone.

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Dolerite

Dolerite is a clear crystalline stone with medium grain size . These are dense black rocks arising from basalt magma, which solidifies at a shallow depth (no more than 1 km). They are distinguished by their massiveness and the absence of pores. These are thick strata tens to hundreds of meters thick.

Dolerites cover vast areas, they can lie horizontally or obliquely, located between layers of sandstone, as well as other sedimentary rocks . Over time, they disintegrate into large rectangular blocks, forming giant steps.

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Trap

This type is nothing more than basalt with seam separation, uniform composition and ladder structure. Its formation is a large-scale geological process . Trap bodies differ in power and length. Trap magmatism is characterized by a huge volume of basalt outpouring in a geologically short time over vast territories.

Lava flows pour out onto the surface of the Earth, filling depressions and river valleys . The basalt then spills over the flat plain. Due to the low viscosity of the melt, magma spreads for tens of kilometers. With such eruptions, there is no permanent center and a pronounced crater. Lava flows from cracks in the ground.

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Application

Basalt has a wide range of uses

The recycled material is used in networks of high and low voltage currents . Linear insulation is made from it in the open air (output, support, insulators of the 3rd bus of the railway, metro).

In addition, it is used in telegraph, telephone, draw-off insulators, stands for batteries, bathtubs, and dishes.

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Raw materials for crushed stone, basalt fiber, heat-insulating building materials are made from it: mats, fabric, felt, mineral wool, composite basalt reinforcement. Low-thickness basalt insulation mats can withstand direct heating from a gas burner. Basalt felt is used as protection and thermal insulation for chimneys, fireplace and stove inserts. They insulate not only the walls, but also the roof.

Minvata is in high consumer demand . The material collected in mats or mineral wool cylinders is not only reliable, but also durable, resistant to external factors. It is used to make acid-resistant powders, backfill for high-voltage converters. Basalt insulators have higher dielectric characteristics in comparison with analogs made of ceramics or glass.

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Basalt crumb is a filler for concrete and an anti-corrosion type of coating . Modern man also uses the mineral for the manufacture of sculptures, fences made of woven threads, sandwich panels, fire protection systems, filters. Basalt pillars are used in the construction of capital structures.

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Basalt is an excellent facing material . It is used to make decorative tiles with a unique natural pattern and characteristic texture. They decorate fountains, stairs, monuments. Budgetary varieties of stone are used in the construction of columns, decorative fences. They are faced with verandas, as well as entrance groups, finishing not only wall, but also floor bases. It is used where acidic fumes are possible. However, the stone has a tendency to polish; during operation, the coatings become smooth.

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Basalt can become the basis for staircases, arches, and other reinforced products . It makes structures strong and reliable. They are laid with walls of damp rooms (for example, baths), it perfectly drains condensation. It is used when laying the foundation of buildings, constructing swimming pools, and other water and earthquake-resistant objects.

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Basalt is used in the production of gravestones, crypts, and acoustic installations . It is an excellent material for making paving stones. With its help, paving of pedestrian areas and even street carriageways, railways is carried out.

Facing cast slabs are made of basalt, replacing the surface finishing with expensive materials (for example, porcelain stoneware, granite).

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Basalt is also used in the production of women's and men's jewelry . Most often these are bracelets, pendants and beads. Earrings from it are rarely made due to its significant weight. In addition, basalt is used for interior decor.

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