Basalt is a common extrusive igneous (volcanic) rock formed from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon. By definition, basalt must be an aphanitic igneous rock with less than 20% quartz and less than 10% feldspathoid by volume, and where at least 65% of the feldspar is in the form of plagioclase. (In comparison, granite has more than 20% quartz by volume.) Basalt is usually grey to black in colour, but rapidly weathers to brown or rust-red due to oxidation of its mafic (iron-rich) minerals into rust. It almost always has a fine-grained mineral texture due to the molten rock cooling too quickly for large mineral crystals to grow, although it can sometimes be porphyritic, containing the larger crystals formed prior to the extrusion that brought the lava to the surface, embedded in a finer-grained matrix. Basalt with avesicular or frothy texture is called scoria, and forms when dissolved gases are forced out of solution and form vesicles as the lava decompresses as it reaches the surface.
hard basalt rock of deccan trap
Igneous rocks
The magma cools and forms both rocks
Basalt
Volcanic rocks are extrusive igneous rocks.
Basalt. Basalt - Wikipedia, the free encyclopedia
silicate rocks, such as granite, gneiss, basalt, and shale.
Most rocks in the lunar Maria are made of basalt, a type of volcanic rock that is rich in iron and magnesium. These rocks formed from lava flows that erupted from the Moon's interior billions of years ago.
Commonly basalt, a volcanic; or granite.
hard basalt rock of deccan trap
The crust.
Examples of igneous rocks are pumice, obsidian, basalt, and rhyolite.
Granite is very much less dense than basalt. This is why the continental crust (mostly composed of granite) floats on Oceanic crust (made mostly of basalt). Granite is 70 % silicon. Where basalt is mainly pyroxene.
Igneous rocks
They are all igneous rocks.
Basalt and granite are the most common types of rocks that make up igneous rocks. Basalt is a fine-grained volcanic rock, while granite is a coarse-grained intrusive rock.
Crustal rocks are primarily made up of silicate minerals such as feldspar, quartz, and mica. These rocks include granite, basalt, and gneiss, and are commonly found in the Earth's crust.