Mafic lava is less viscous(runnier) than felsic lava due to a lower silica content. This causes non-violent eruptions such as in the Hawaiian Islands. Mafic lava tends to be associated more with interplate volcanism and mid-ocean ridges and produces the rock type known as basalt. (The ocean floor is made of basalt.) Felsic lava is mainly found at convergent zones (areas of colliding plates) and has a high silica and water content which causes the lava to be highly viscous and causes very violent eruptions. This lava produces rhyolite and andesitic rocks.
The color of the rocks formed by magmas is a consequence of its composition, mafic magmas are dark colored (Mg-Fe) and felsic magmas are light colored (Feldspars-Si).
The term mafic is derived from magnesium and the Latin word for iron, while felsic is derived from the words feldspar and silicone. Mafic rocks contain heavier elements and include basalt and gabbro. Felsic rocks have a lower percentage of heavier elements, and the most common type is granite.
Felsic rocks are greater than 65% silica and contain less of the heavy elements present in mafic rocks. Felsic rocks are generally lighter in color than mafic rocks. Intermediate rocks contain between 55 and 65% silica. Mafic is a term used to describe an igneous rock that contain between 45 and 55% silica, is usually dark in color, with a chemistry that may be high in magnesium and iron. Note that mafic, felsic, and intermediate rocks are not all completely the elements listed. They are made up of others, too.
Mafic lava is less viscous than felsic lava due to a lower Silica content . This causes non-violent eruptions such as in the Hawaiian Islands. Mafic lava tends to be associated more with interplate volcanism and mid-ocean ridges and produces the rock type known as basalt. Felsic lava is mainly found at convergent zones and has a high silica and water content which causes the lava to be highly viscous and causes very violent eruptions. This lava produces rhyolite and andesitic rocks.
Felsic rocks are high in silicon (Si) and low in magnesium (Mg) and in iron (Fe). Gradation in feldspar causes felsic rocks to be richer in potassium (K).
Mafic rocks are high in magnesium (Mg) and iron (Fe) and low in silicon (Si). Gradation in feldspar causes magic rocks to be richer in calcium (Ca)
Felsic rocks are lighter in color and less dense than mafic rocks. They are dominate by quartz, potassium feldspar, and sodium-rich plagioclase. Mafic rocks are darker, denser, and contain primarily calcium-rich plagioclase, pyroxenes, and sometimes olivine.
Mafic or basic rocks are low in silica and oxygen whereas felsic or acidic rock is higher in silica and oxygen content.
Felsic rocks have lots of silica mafic rocks have very little silica
Mafic rocks are denser than felsic rocks because they contain heavier compounds, minerals and other materials, they are ferromagnesian in composition.
Pyroclastic flows can be of any composition, but are more commonly felsic or intermediate.
It can be either. The term felsic describes the composition of the rock, not where it forms. The general category for intrusive felsic rock is granite while extrusive felsic rock is rhyolite.
Like many stratovolcanoes, Mount St Helens has produced material of mafic, felsic, and intermediate composition. Overall, much of the material is itermediate. The 1980 eruption and later activity have produced dacite, which has an intermediate-felsic composition
The process is painful love. When the mafic minerals fall in love with the felsic minerals they fall to the bottom. The felsic is often there too and sees the minerals falling toward them so they scared to be in love again and go to the top. This makes the mafic mad and it stays there. The felsic is afraid to go back and stays on the top. :( <333 love hurts If I remember my geology, plutons are considered intrusions, and reflect the mineral composition of the magma they were formed from. That being said, what minerals are present in a pluton are directly a result of what they were made from, and the minerals condense out following Bowen's Reaction series. This means mafic minerals condense out at a higher temp and higher pressure, so as the pluton continues to intrude, it cools and depressurizes. Thus minerals lower in the reaction series cool and crystallize before the felsic minerals towards the top. You can also find contact metamorphic rocks on the edges of plutons. Some of these may wrongfully appear to be mafic rocks like Olivine. http://en.wikipedia.org/wiki/Bowen's_reaction_series
Oceanic crust is mafic in composition and continental crust is felsic in composition. Mafic minerals generally have a higher density than felsic minerals and therefore, the oceanic crust is heavier.
Neither. The terms mafic and felsic refer to the composition of igneous rocks, which are dominated by silicate minerals. Marble is a metamorphic rock composed of carbonate minerals. The terms mafic and felsic do no apply to it.
Mafic rocks are denser than felsic rocks because they contain heavier compounds, minerals and other materials, they are ferromagnesian in composition.
Rhyolite has a more felsic composition than basalt.
Neither. The terms mafic and felsic refer to the composition of igneous rocks, which are dominated by silicate minerals. Rock salt is a sedimentary halide rock. Such terms do not apply to it.
Rhyolite is not a mafic rock, but a felsic rock, high in silicates, and similar to granite in composition.
Some felsic rocks are and some are not. The term felsic is a description of an ingeous rock's composition, not its texture or where it occurs.
Pyroclastic flows can be of any composition, but are more commonly felsic or intermediate.
Yes. Felsic is a term used to describe the composition of some igneous rocks.
the composition of igneous rocks lying between felsic and mafic.
It can be either. The term felsic describes the composition of the rock, not where it forms. The general category for intrusive felsic rock is granite while extrusive felsic rock is rhyolite.
No. Felsic rocks are light-colored and high in silica. Mafic rocks are generally dark-colored and low in silica.