Basalt rock with various colors and price per kg, ton…is a heavy volcanic rock used as a revolutionary stone for any area of structure that makes up most of the world's oceanic crust. Some of them also erupt on land, but in general, basalt is a marine rock. Basalt is darker, denser, and more detailed than the familiar continental granite . This material is dark and dense in color because it is rich in dark and heavy metals containing magnesium and iron (i.e. mafic) and weaker minerals in silicon and aluminum. Contains only very small crystals after cooling. Much of the world's basalt erupts quietly in the deep ocean along plateaus that extend plate tectonics in the middle of the ocean. A small number of volcanic eruptions occurred on volcanic islands, high subduction zones, and occasional large events elsewhere. Basalt is a type of lava where rocks in the mantle begin to melt.
If you think of basalt as mantle juice, then when we talk about oil extraction from olives, basalt is the first compression of the fleshy material. The big difference is that olives hold the oil under pressure, and when the pressure is released from the mantle, intermediate basalts are formed. Known as ultramafic. As the Earth's plates separate, at the mid-ocean boundary, pressure is released into the peridotite, causing it to begin melting - the exact composition of the melt depends on many details, but it usually cools and separates into the minerals clinopyroxene and clinoid Feldspar. Contains a small amount of olivine, o-propadiene and magnetite. In addition, any water and carbon dioxide in the source rock will move towards the melt, causing the melt to melt even at low temperatures. Peridotite is dry and highly devoid of olivine and orthopyroxene. Like almost all materials, lava is less dense than solid rock. Once formed deep in the Earth's crust, the basalt magma rises to the center of the central depression that covers the ocean basin, where it accelerates in freezing icy water to form lava pillows. Unexploded basalt hardened in the levee and piled up vertically on the deck like paper. These dike complexes overlie the mid-ocean crust and below are larger reservoirs of magma that slowly crystallized into plutonic gabbros. The mid-ocean ridge basalt is an important part of the earth's geology and is called "MORB" by experts. However, the oceanic crust is constantly returning to the mantle through plate tectonics. Therefore, even though MORB is the major constituent of basalt in the world, it is rare. To study it, we had to go deep into the sea with cameras, samples and submarines. for the aforementioned reasons basalt stone tiles are revolutionary rock to use in any areas of structure.
Basalt rock price per ton
The price for basalt rock per ton could range from $175.00 per ton or $0.20/lb when purchased via pallet. The basalt we know comes not from stable volcanoes in the Central Mountains, but from increasingly active activity elsewhere. These places are divided into three categories: subregions, sea islands and provinces of Great Azerbaijan, sea barley plateaus in the ocean and continental flood basalts on land. Regarding the origin of the Oceanic Island Basalts (OIBs) and the Great Azerbaijan Provinces (LIPs), theorists fall into two camps, one from deep mantle material and the other from plate-related dynamics. now it's easier to say that both OIBs and LIPs have more common mantle source rocks than MORBs and leave everything behind. Subduction transports MORB and water into the mantle. This material then rises as a melt or liquid in the weakened mantle above the subduction zone and fertilizes it, activating fresh magma, including basalt. If basalts are erupted in spreading oceanic regions (back-arc basins), they can form pillow lavas and other MORB features. These crustal plutons may later be preserved on Earth as ophiolite.
If basalts emerge on the subcontinent, they are usually mixed with less continental rocks (i.e. clastics) and produce lava ranging from andesite to rhyolite. But under favorable conditions, basalt can coexist with and within these metal melts, as in the Great Western Basin of the United States. The national reserves of basalt are more than tens of millions of tons. But because the stone is prismatic in the mine, special precision and finesse is required to extract the stone safely, which increases the time and consequently the cost of mining. On the one hand, the potential reserves of this stone , marble stone and its wide application in various modern industries, on the other hand, make Europe and developed countries have a great desire to buy this mineral. Not only does this satisfy the domestic demand, but we also see its exports to some European countries such as the Netherlands. It is certain that the sale of processed minerals has more added value than unprocessed ore, so investing in the processing sector of this mineral, while increasing exports, will also bring more added value to the country. The diversity of minerals and their use in different industries has led many developed countries to invest heavily in the mining industry. However, it is important to note that mineral extraction is not the end of the story, but an important part of mineral production. After the minerals are mined and processed, the processing operations return, allowing the minerals to obtain the necessary economic benefits. At the same time, basalt is one of the minerals obtained from volcanic activity, and the processing of this mineral offers the possibility of its use in industries ranging from road construction to fiber production. This type of stone, called alkaline stone because it does not contain silicon, is also abundant in Iran and has been used by the ancients for a long time. Of course, it is important to note that at present, many industrialized and developed countries rely on modern engineering knowledge and equipment to process this mineral and use it to make wear-resistant light steel bars, car and ship hulls, oil and gas pipelines and more.
Basalt color and price per ton
Basalt price varies based on different factors like color and quality but usually it is 60$ per ton. Basalt is usually dark gray to black in color due to its high content of pyroxene or other dark pyroxene minerals, but can display a wide range of shades. Due to the high content of plagioclase, some basalts are quite light in color and are sometimes described as colorless basalts. Chances are that many of you have heard the name basalt in school and education because of your field of study or construction work environment and a question has arisen in your mind, what is basalt and what are its characteristics? and features. Or what is the use of basalt in industries like construction. This stone is one of the most abundant on earth, and because of this abundance, it is used in large quantities in various industries, including the construction industry. The variety of uses of this stone prompted us to present to you this stone, one of the most abundant stones like gilsonite on earth after granite, examining its properties. Some basalts have a completely glassy structure (tachhydrite), and many basalts have a fine-grained and dense structure. The typical form of basalt is a porphyritic structure with large crystals of olivine, pyroxene or feldspar (phenocryst) in a fully crystalline matrix (matrix). The minerals olivine and pyroxene are the most common porphyry minerals in basalt. In addition to these two minerals, porphyry plagioclase is also found in basalt structures. Basalt lava is usually spongy or pumice. Cavities created by the gases and vapors released from the lava material are filled with secondary minerals such as calcite, chlorite, and zeolite. 
This stone is one of the most abundant on earth after granite and comes in several types. Some basalts have a completely glassy structure (tachhydrite), and many basalts have a fine-grained and dense structure. The typical form of basalt is a porphyritic structure with large crystals of olivine, pyroxene or feldspar (phenocryst) in a fully crystalline matrix (matrix). The minerals olivine and pyroxene are the most common porphyry minerals in basalt. In addition to these two minerals, porphyry plagioclase is also found in basalt structures. Basalt lava is usually spongy or pumice. Cavities formed by the gases and vapors released from the lava material are filled with secondary minerals such as calcite, chlorite, and zeolite. Basalts are generally divided into two broad categories based on their chemical and petrographic properties: ductile porous basalts and alkali basalts. It is characterized by calcareous plagioclase, characterized by pyroxene, dove pyroxene or hyperpyrite and olivine as the main mafic mineral. Basalt without olivine is also well represented. Lavanite basalts containing 45-63% silica is rich in iron, including lavanite basalts (calcium-poor pyroxene basalts). The lava is mainly found in the mountainous zone, and the alkali metal content is relatively rich in alkali basalt. This type of basalt does not contain silica and may contain feldspar, alkali feldspar, feldspar, and potash feldspar. Augustus is a titanium-rich pyroxene in alkali basalt, and low-calcium pyroxene never occurs. In some cases, basalts are classified into high-titanium and low-titanium based on titanium content, and the mineral characteristics of basalt are determined by the content of plagioclase, feldspar crystal , and pyroxene. Olivine can also be a defined and important compound. Minor minerals found in basalt include iron oxides and iron-titanium oxides such as magnetite, olivine, and ilmenite. Due to the presence of this mineral oxide, basalt can acquire strong magnetism as it cools. In basic basalt, pyroxene (pyroxene and orthopyroxene or dove) and plagioclase are rich in calcium, a mineral commonly found in phenocrysts. Peridot can also be a phenocryst. 
Basalt rock color
Basalt rock color is usually dark gray to black. Basalt is formed by the rapid cooling of basalt lava, the equivalent of gabbro magma, exposed from within the crust to the Earth's surface or very close to the Earth's surface. These basalt flows are very thick and extensive, with few air pockets within them. Pyroxene and magnetite give basalt its black color. They all contain raw iron , that's why they are black. so this is iron again, which is responsible for the coloring of basalt. Plagioclase is usually the most important component by volume and is mostly light gray in color. One of the most important applications of basalt is its use in the production of basalt fibers. Basalt is a neutral natural material that is the product of extrusive igneous rocks, the dominant type of rock in the Earth's crust. One of the characteristics of materials containing basalt compounds is that these materials are completely compatible with the environment and are completely non-toxic. For this reason, they use basalt to produce basalt fibers. one of the characteristics of basalt fiber is its higher chemical stability than glass fiber, especially in intense gaming environments. These fibers are non-toxic, non-flammable and resistant to high temperatures. Another characteristic of these carbon fiber is their relatively high thermal stability, which is why basalt has three times the thermal insulation capacity of fire-resistant cotton, which is why these fibers are used in marine fire protection due to their excellent thermal insulation properties. 
In addition, based on research and studies done in the field of fibers for the marine industry, it was concluded that basalt fibers have mechanical properties comparable or even better than E-glass fibers, and therefore, these fibers are a suitable choice. for use in containers. Basalt is the dark, heavy volcanic rock that makes up most of the world's oceanic crust. Some of them also erupt on land, but first and foremost, basalt is an oceanic rock. Basalt ("ba-SALT") is darker, denser, and finer-grained than the familiar continental granite. It is black and dense because it is rich in dark heavy metals containing magnesium and iron (i.e. more mafic) and less in minerals containing silicon and aluminum sheet . It has a finer grain size because it cools rapidly near or on the Earth's surface and contains only very small crystals. Much of the world's basalt erupts quietly in the deep ocean along mid-ocean ridges—extensions of plate tectonics. A small number of volcanic eruptions occurred over oceanic volcanic islands and subduction zones, with occasional large eruptions elsewhere. Basalt is a type of lava that forms when rocks in the mantle begin to melt. If you think of basalt as the juice of the mantle, and we're talking about how to extract oil from olives, then basalt is the first compression of mantle material. 
The big difference is that olives produce oil under pressure, while mid-ocean ridge basalts are formed when pressure is released in the mantle. The upper mantle is composed of rocky peridotite, which is more mafic than basalt and is often referred to as ultramafic. At mid-ocean ridges where the Earth's plates separate, the release of pressure in the peridotite causes it to start melting -- the exact composition of the melt depends on many details, but it usually cools and separates into the minerals clinopyroxene and plagioclase. Contains a small amount of olivine, orthopyroxene and magnetite. Crucially, any water and carbon dioxide in the source rock also makes its way into the melt, helping to preserve it even at lower temperatures. The depleted peridotite that is left is dry and is richer in olivine and orthopyrite. My company has for decades been the lead in both supply and export of basalt products to the entire countries around the world and hence in kindly honored to invite all dear customers and traders to join us in world trade of basalt and purchase the best quality basalt ever in your life.
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