In geology, felsic is an adjective describing igneous rocks that are relatively rich in elements that form feldspar and quartz. Common felsic minerals include quartz, muscovite mica, and the orthoclase feldspars. The word "felsic" is a term used in geology to refer to silicate minerals, magma, and igneous rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium.They are usually light in colour and have specific gravities less than 3. Felsic rocks are mostly light-colored and the most common type is granite. Basalt. Name a common and widely occurring type of intrusive, felsic, igneous rock. Compilations of many rock analyses show that rhyolite and granite are felsic, with an average silica content of about 72 percent; syenite, diorite, and monzonite are intermediate, with an average silica content of 59 percent; gabbro and basalt are mafic, with an average silica content of 48 percent; and peridotite is an ultramafic rock, with an average of 41 percent silica. Granite tables are used extensively as bases or even as the entire structural body of optical instruments, CMMs, and very high precision CNC machines because of granite's rigidity, high dimensional stability, and excellent vibration characteristics. Granite is one of the most commonly found rocks on the surface of the earth. Mafic lava creates basalt while felsic lava produces andesitic and rhyolite rocks. Generalized Composition Ranges of Common Igneous Rocks: This chart illustrates the generalized mineral composition of igneous rocks. , Granite has been extensively used as a dimension stone and as flooring tiles in public and commercial buildings and monuments.  As a result of the work of sculptor William Leslie, and later Sidney Field, granite memorials became a major status symbol in Victorian Britain. There is some concern that some granite sold as countertops or building material may be hazardous to health. How does subduction trigger melting? This rock measures approximately four inches across. Within two hundred years, the red granite has drastically deteriorated in the damp and polluted air there.  A-type granites occur in the Koettlitz Glacier Alkaline Province in the Royal Society Range, Antarctica.  In-situ granitization requires heating by the asthenospheric mantle or by underplating with mantle-derived magmas. A classic example of a felsic igneous rock is granite, which is mainly composed of quartz (SiO2) and feldspar (potassium-rich and sodium-calcium rich varieties exist) with minor amounts of other minerals (biotite or amphibole).  In military engineering, Finland planted granite boulders along its Mannerheim Line to block invasion by Russian tanks in the winter war of 1940. Felsic rocks are less dense than mafic and ultramafic rocks, and thus they tend to escape subduction, whereas basaltic or gabbroic rocks tend to sink into the mantle beneath the granitic rocks of the continental cratons. The area shown in this image is about 1/4 inch across.  The quarrying ceased around the third century AD. Granite is a common type of granular and phaneritic felsic intrusive igneous rock. The acronym, QAPF, stands for "Quartz, Alkali feldspar, Plagioclase, Feldspathoid (Foid)". In felsic and mafic rocks …less than 45 percent are ultramafic. Image copyright iStockphoto / Jonathan Larsen.  Dan Steck of St. Johns University has stated , Granitization is an old, and largely discounted, hypothesis that granite is formed in place through extreme metasomatism. felsic and mafic rock classification. The word "granite" is used in a variety of ways by different people. Hand sample of vesicular rhyolite.  If enough partial melt is produced, it will separate from the source rock, become more highly evolved through fractional crystallization during its ascent toward the surface, and become the magmatic parent of granitic rock. Applying this definition requires the mineral identification and quantification abilities o… This mineral composition usually gives granite a red, pink, gray, or white color with dark mineral grains visible throughout the rock. A. Flux melting of the asthenosphere above the subducting slab creates a rising melt. Mafic rocks are darker in color than felsic rocks. The letter-based Chappell & White classification system was proposed initially to divide granites into I-type (igneous source) granite and S-type (sedimentary sources). Conditions for crystallization of liquid magma are close enough to those of high-grade metamorphism that the rocks often bear a close resemblance. Obsidian is a natural glass - it lacks crystals, and therefore lacks minerals. Leaving the letters, numbers, and emblems exposed on the stone, the blaster can create virtually any kind of artwork or epitaph. B. is felsic in composition. The fine grain varieties and polished slabs are used for massive structures. Common felsic minerals include quartz, muscovite, orthoclase, and the sodium-rich plagioclase feldspars. It falls under the category of felsic intrusive igneous rocks. This may not be evident in the major and minor element chemistry, since the minerals most likely to crystallize at the base of the chamber are the same ones that would crystalize anyway, but crustal assimilation is detectable in isotope ratios.  They are also orogenic but range from metaluminous to strongly peraluminous. Mount Rushmore: Mount Rushmore in the Black Hills, South Dakota is a sculpture of United States presidents George Washington, Thomas Jefferson, Theodore Roosevelt, and Abraham Lincoln sculpted from a granite outcrop. Felsic rocks are composed of high levels of magma, silicate materials, and rocks which are also rich in potassium, oxygen, silicon, and sodium. Granite. 2) 400 million years ago.  As these narrow conduits open, the first magma to enter solidifies and provides a form of insulation for later magma. Felsic magmas are thought to form by addition of heat or water vapor to rock of the lower crust, rather than by decompression of mantle rock, as is the case with basaltic magmas. Felsic. known as "basement rocks. Subsequently, one may also ask, is Obsidian mafic or felsic? These rocks have a granular and phaneritic texture. B. is felsic in composition. Potassium-40 is a radioactive isotope of weak emission, and a constituent of alkali feldspar, which in turn is a common component of granitic rocks, more abundant in alkali feldspar granite and syenites. It always exhibits a conchoidal fracture that has a vitreous luster on fracture surfaces. The melted sediments would have produced magma intermediatein it… However, experimental work had established by the 1960s that granites were of igneous origin. It is important to note that there are many intermediate steps in the purification process, and many intermediate magmas which are produced during the conversion from mafic to felsic. Felsic magma or lava is higher in viscosity than mafic magma/lava. Predominantly, these rocks appear in white, pink or grey colour. Granite is composed mostly of two minerals: quartz and orthoclase feldspar (a potassium-rich variety of feldspar). The most common felsic rock is granite, but others include quartz, muscovite, orthoclase, and the sodium-rich plagioclase feldspars. Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. The massive Gopuram (ornate, upper section of shrine) is believed to have a mass of around 81 tonnes. Felsic rocks are composed of minerals such as quartz, orthoclase, muscovite, and feldspars. Rhyolite. The word "felsic" is a term used in geology to refer to silicate minerals, magma, and igneous rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium.They are usually light in colour and have specific gravities less than 3. What type of rock is gabbro? However, granite is frequently selected because it is a prestige material, used in projects to produce impressions of elegance, durability, and lasting quality. 38, pp. What is the difference between felsic and mafic rocks? Because they are made of lighter elements, they tend to be more buoyant than maficrocks, which are rocks high in magnesium and iron, like basalt. Aberdeen in Scotland, which is constructed principally from local granite, is known as "The Granite City". Early fractional crystallisation serves to reduce a melt in magnesium and chromium, and enrich the melt in iron, sodium, potassium, aluminum, and silicon. As such, igneous rocks are described based on their silicate minerals. It is a glassy-textured, extrusive igneous rock. This simple definition enables students to identify the rock based upon a visual inspection. This gives them tremendous buoyancy, so that ascent of the magma is inevitable once enough magma has accumulated. The most common felsic rock is granite. Mafic rocks derive from … The most common felsic rock is granite. Basalt will be a lot denser, which is the main reason why granite is a feature of continental crust, and basalt dominates oceanic crust. It is a glassy-textured, extrusive igneous rock. Granite is one of the rocks most prized by climbers, for its steepness, soundness, crack systems, and friction. A study of granite countertops was done (initiated and paid for by the Marble Institute of America) in November 2008 by National Health and Engineering Inc. of USA. Granite - Lake Michigan Stone. 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