basalt
Granite and basalt are not pure substances because they are composed of multiple minerals and varying chemical compositions. Granite typically contains quartz, feldspar, and mica, while basalt is primarily made up of plagioclase, pyroxene, and olivine. The presence of these different minerals indicates that they are mixtures rather than single, homogeneous substances. Additionally, their physical and chemical properties can vary depending on the proportions of these constituent minerals.
Basalt typically has a smoother texture compared to granite. Where granite is more coarse and grainy due to its composition of minerals like quartz, feldspar, and mica, basalt is fine-grained and its texture is smoother because of its rapid cooling from lava flows.
Although they are both igneous rocks which have solidified from magma, granite is an intrusive igneous rock and basalt is an extrusive igneous rock. As an extrusive igneous rock, the magma that formed granite had a long time to cool underground, and therefore consists of larger, visible mineral crystals. Basalt on the other hand, cooled rather rapidly from magma after eruption from a volcano and therefore is aphanitic, with crystals too small to be seen with the naked eye. There is also a difference in chemistry. Granite is considered felsic, with a preponderance of silicate minerals like quartz and orthoclase feldspar. Basalt is considered mafic, with an abundance of heavier minerals like olivine and amphibole, thus making it heavier than granite. These minerals also give basalt a dark color compared to the lighter colored granite.
Granite is a coarse-grained igneous rock composed mainly of quartz, feldspar, and mica, while basalt is a fine-grained igneous rock composed mainly of iron and magnesium-rich minerals. Granite is lighter in color and has visible grains, while basalt is typically dark in color and has a smoother texture. Additionally, granite forms through slow cooling underground, while basalt forms through rapid cooling at or near the Earth's surface.
Basalt does have a greater specific gravity. Granite is not as dense as basalt.
Basalt and Granite.
Basalt tends to be darker in color compared to granite. Basalt is typically a dark-colored volcanic rock formed from the rapid cooling of lava, while granite is an igneous rock that is lighter in color due to its composition of lighter minerals such as quartz and feldspar.
Granite has more silica than basalt. Granite is a light-colored, coarse-grained igneous rock made up of quartz, feldspar, and mica, which are minerals rich in silica. Basalt, on the other hand, is a dark-colored, fine-grained igneous rock with lower silica content compared to granite.
from the economic point of view you can use them as building stones or as sources of minerals
Granite and basalt are not pure substances because they are composed of multiple minerals and varying chemical compositions. Granite typically contains quartz, feldspar, and mica, while basalt is primarily made up of plagioclase, pyroxene, and olivine. The presence of these different minerals indicates that they are mixtures rather than single, homogeneous substances. Additionally, their physical and chemical properties can vary depending on the proportions of these constituent minerals.
Basalt typically has a smoother texture compared to granite. Where granite is more coarse and grainy due to its composition of minerals like quartz, feldspar, and mica, basalt is fine-grained and its texture is smoother because of its rapid cooling from lava flows.
Basalt and gabbro have higher chemical weathering rates than rhyolite and granite because they contain more ferromagnesian minerals like olivine and pyroxene that are more susceptible to chemical weathering compared to the quartz-rich minerals in rhyolite and granite. This makes basalt and gabbro more prone to breakdown and alteration when exposed to weathering agents like water and acids.
Granite is typically light in color due to its high silica content and contains visible grains of minerals like quartz, feldspar, and mica. In contrast, basalt is typically dark in color, fine-grained, and contains minerals like pyroxene and olivine.
Basalt is extrusive, formed from cooling lava, and has a fine-grained texture with minerals like pyroxene and plagioclase feldspar. Granite is intrusive, formed from cooling magma underground, and has a coarse-grained texture with minerals like quartz, feldspar, and mica. Both are igneous rocks, but basalt is dark-colored and dense, while granite is light-colored and less dense.
Although they are both igneous rocks which have solidified from magma, granite is an intrusive igneous rock and basalt is an extrusive igneous rock. As an extrusive igneous rock, the magma that formed granite had a long time to cool underground, and therefore consists of larger, visible mineral crystals. Basalt on the other hand, cooled rather rapidly from magma after eruption from a volcano and therefore is aphanitic, with crystals too small to be seen with the naked eye. There is also a difference in chemistry. Granite is considered felsic, with a preponderance of silicate minerals like quartz and orthoclase feldspar. Basalt is considered mafic, with an abundance of heavier minerals like olivine and amphibole, thus making it heavier than granite. These minerals also give basalt a dark color compared to the lighter colored granite.
Basalt is an extrusive, mafic igneous rock, which means that it solidifies from lava at or near the surface, and is composed partly of iron and magnesium minerals. Granite is an intrusive felsic igneous rock, meaning that it solidifies from magma below the surface, and is relatively high in minerals containing silicon and aluminum. Basalt has a higher specific gravity than granite, and is also darker than granite. Basalt may have visible air pockets, frozen in place when it solidified from lava. Granite will not exhibit this characteristic. Basalt has mineral crystals that are not visible with the naked eye. Granite has visible mineral crystals.
Granite - coarse grained. Basalt - fine grained.