basaltic
Igneous rocks that are medium colored and have no silica are called mafic rocks. They are mainly composed of magnesium and iron.
Light-coloured igneous rocks, such as granite, have a higher silica content and lower iron and magnesium than darker ones, such as basalt. Since iron and magnesium are very dense minerals, this makes darker igneous rocks more dense than lighter ones.
Ultramafic igneous rock contains the least silica.
Those igneous rocks would be referred to as felsic.
Iron-rich igneous rocks are generally denser than silica-rich igneous rocks. This is because iron and magnesium minerals, which are abundant in iron-rich rocks, have a higher specific gravity compared to the lighter silica-rich minerals such as quartz. As a result, rocks like basalt, which are rich in iron and magnesium, are denser than rocks like granite, which are high in silica.
Igneous rocks that are medium colored and have no silica are called mafic rocks. They are mainly composed of magnesium and iron.
These types of igneous rocks are commonly known as mafic rocks. They have a high density due to the presence of minerals like olivine, pyroxene, and amphibole, which are rich in iron and magnesium. Examples include basalt and gabbro.
Light-coloured igneous rocks, such as granite, have a higher silica content and lower iron and magnesium than darker ones, such as basalt. Since iron and magnesium are very dense minerals, this makes darker igneous rocks more dense than lighter ones.
Mafic igneous rocks, like basalt, are dark colored and low in silica.
Basalt is a dark-colored, low-silica igneous rock commonly found as a result of volcanic activity. Its composition typically contains around 50% silica, making it relatively low in silica compared to other igneous rocks like granite.
Mafic igneous rocks, like basalt, are dark colored and low in silica.
Ultramafic igneous rock contains the least silica.
majority
Those igneous rocks would be referred to as felsic.
Two examples of fine-grained igneous rocks are basalt and rhyolite. Basalt is a dark-colored rock with a composition rich in iron and magnesium, while rhyolite is light-colored and has a high silica content. Both rocks form from the cooling and solidification of molten magma.
Iron-rich igneous rocks are generally denser than silica-rich igneous rocks. This is because iron and magnesium minerals, which are abundant in iron-rich rocks, have a higher specific gravity compared to the lighter silica-rich minerals such as quartz. As a result, rocks like basalt, which are rich in iron and magnesium, are denser than rocks like granite, which are high in silica.
Acidic igneous rocks, also known as felsic rocks, are composed primarily of light-colored minerals such as quartz, feldspar, and mica. These rocks have a high silica content and typically have a lower iron and magnesium content compared to mafic rocks. Examples of acidic igneous rocks include granite and rhyolite.