The color is an indication of how mafic or felsic which are defined by silica content. A dark(75% or greater black) or a olive green color is mafic and ultramafic respectively, and means low silica (less then about 57% SiO2). A Grayish (50% black and light colors) rock is a intermediate rock and has between 57 to 69 or 74% SiO2 depending on other mineral in the rock. a light color (75% pink or white colors) rock has a felsic composition and has greater than 69 or 74% SiO2
Not nessessarily.
black
It determines high silica or low silica. It will determine if it is sticky or not, or if it flows fast or slow. *high in silica~Sticky, and slow. Will not flow easily. *low in silica~Fact, not sticky. Will flow easily.
The majority of minerals associated with igneous rocks are silicates. It is the proportion of certain silicate minerals that affects the color of igneous rocks. Igneous rocks that are high in orthoclase feldspar, quartz, and muscovite mica will be lighter in color than igneous rocks that are higher in olivine, pyroxene, amphibole, and biotite mica.
volcanic rocks
The terms intrusive and extrusive apply to the formation of igneous rocks. Silica is a chemical component of a wide variety of minerals found in many types of igneous, metamorphic, and sedimentary rock. All igneous rocks, both intrusive and extrusive, contain silica.
The silica content will vary from one volcano to the next and will even vary over time for a single volcano. On average, though, composite volcanoes erupt intermediate rocks that are 52-63% silica.
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.
The more silica contained in a rock, the lighter in color it will be.
brown
The more silica contained in a rock, the lighter in color it will be.
An igneous rock with a high level of silica will have a light color.
Generally, igneous rocks with more silica are lighter in color.
No. Mainly rocks with a high content of iron. Rocks such as silica or calcium carbonate are not.
An igneous rock's color is mainly determined by its silica content.
An igneous rock's color is mainly determined by its silica content.
It determines high silica or low silica. It will determine if it is sticky or not, or if it flows fast or slow. *high in silica~Sticky, and slow. Will not flow easily. *low in silica~Fact, not sticky. Will flow easily.
Felsic rocks such as granite.
The majority of minerals associated with igneous rocks are silicates. It is the proportion of certain silicate minerals that affects the color of igneous rocks. Igneous rocks that are high in orthoclase feldspar, quartz, and muscovite mica will be lighter in color than igneous rocks that are higher in olivine, pyroxene, amphibole, and biotite mica.