rich
They are called felsic igneous rocks.
Felsic igneous rocks with alkali feldspars, quartz, and mica. Examples would include rhyolite, pumice, granite, and obsidian.
Acidic igneous rocks are composed of high percentage of silicic materials (minerals) and are light in colour while the Basic igneous rocks are contains predominantly ferromagnesian minerals\materials, they have very little proportion of silica and are dark in colour.
Silica in molten material tends to crystallise as quartz, which is white or mostly pale in colour. So felsic rocks (from silica-rich magma) tend to be pale, while mafic rocks (from silica-poor magma) tend to be dark in colour.
Feldspar can be a variety of colors: clear, gray, white, tan, pink, brown, or red.
An igneous rock with a high level of silica will have a light color.
Andesite
majority
They are called felsic igneous rocks.
Generally, igneous rocks that are low in silica are dark relative to those that are high in silica. This tendency is largely the result of rocks low in silica having increased iron. Iron minerals tend to adsorb significant amounts of the visible spectrum and hence appear dark. I want to emphasize that this is a general tendency and there are exeptions -- obsidian which is very high in silica is typically a dark to black rock and a special igneous rock call carbonatite is very light in color but has little silica.
felsic
Felsic igneous rocks with alkali feldspars, quartz, and mica. Examples would include rhyolite, pumice, granite, and obsidian.
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.
The word felsic is used to describe igneous rocks that are rich in silica and alkali feldspar. Such rocks tend to be light in color and have a lower density than other igneous rocks.
Acidic igneous rocks are composed of high percentage of silicic materials (minerals) and are light in colour while the Basic igneous rocks are contains predominantly ferromagnesian minerals\materials, they have very little proportion of silica and are dark in colour.
Those igneous rocks would be referred to as felsic.
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.