Difference Between Mafic and Felsic
Mafic vs Felsic
In the concept of mineralogy, or geology in the much broader sense, two terms are commonly used to describe the characteristics of rocks and also lava. These terms are mafic and felsic.
When used to describe the characteristics of lava, mafic lava would mean that it is runnier or more viscous as opposed to the felsic lava. The reason for such is the amount of silica present in the lava. In mafic lavas, there is less silica than in felsic. With a runnier lava, the volcanic eruption is most likely not that violent as exemplified in the Hawaiian Island volcanic eruptions.
Moreover, mafic lava is responsible for the rock formation known as basalt. If you carefully examine the floor of the ocean, you shouldn’t be surprised that most of it is made of basalt. It is also connected to the nature of mid-ocean ridges as well as interplate volcanism.
By contrast, felsic lava is usually found in specific geological areas known as the convergent zone. This area is where geologic plates collide. Because of the presence of huge amounts of silica in this area, and the addition of the surrounding water and burnt earth, the combination creates more viscous lavas and more violent eruptions. And unlike its mafic counterpart, felsic lava produces andesitic and rhyolite rock formations.
With regard to the usage of felsic and mafic in the concept of igneous rocks, these terms are actually describing the silica content. As such, igneous rocks are described based on their silicate minerals. Arranged in a way of increasing silica content, igneous rocks can be described as being ultramafic, mafic, intermediate, and felsic. This means that ultramafic is the type of rock having the least silica while felsic has the most silicate compound.
In connection to the gradation of rocks with respect to its silica content, the terms ultramafic down to felsic, also mean a decrease in their colors. Thus, ultramafic rocks are the darkest in color while felsic rocks are the lightest. To explain this, geologists claim that the mafic’s dark appearance is attributed to the coexistence of magnesium and iron which are usually bound to silica.
1.Mafic lava is less viscous than felsic lava.
2.Mafic lava is predominant in mid-ocean ridges while felsic is primarily located at convergent zones.
3.Mafic lava induces weaker eruptions as opposed to the stronger eruptions in felsic lava.
4.Mafic lava creates basalt while felsic lava produces andesitic and rhyolite rocks.
5.Either in describing rocks or lava, mafic means that the lava or rock has less silica while felsic implies that the lava or rock has the most silica.
6.Mafic rocks are darker in color than felsic rocks.
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