mafic igneous rocks examples

If they erupt from volcanoes onto the surface as lava, they are called extrusive rocks.By contrast, Intrusive rocks are formed from magma that cools underground. In geology, a pluton is a body of intrusive igneous rock (called a plutonic rock) that is crystallized from magma slowly cooling below the surface of the Earth. Igneous amphibole is made of hornblende, which is composed of an iron-magnesium silicate, a calcium-iron-magnesium silicate and an aluminum-iron-magnesium silicate. Igneous rocks get their name from the latin word for fire “igneus”. 16-45% The quick cooling gives this rock a glassy look. There are a couple things that differ Mafic rocks from Felsic. Felsic Rocks and Mafic Rocks. Rhyolite. Also Mafic rocks are rich in calcium, iron, and magnesium, and poor in silicon. • Magmatic segregation deposits: –formed in intrusive bodies –ore deposits formed during fractional crystallisation • Exceptions: Felsic magmas are the most viscous because of their high silica content. If the intrusive rock cooled underground but near the surface, it is called subvolcanic or hypabyssal, and often has visible, but tiny mineral grains. Course grained example of intermediate igneous rock. Since igneous rocks are characterised by silica content in them, mafic is the one with less silica content (approx. Click any image to enlarge. Basalt. The classification is done based on their silica content, as silica is usually the most abundant of all the oxides present. Igneous Rocks . As per Wikipedia, “Igneous rock (derived from the Latin word ignis meaning fire) is one of the three main rock types, the others being sedimentary and metamorphic.Igneous rock is formed through the cooling and solidification of magma or lava. Differences Of Mafic And FelsicYouTube. All of these minerals contain iron and magnesium. Intrusive igneous rock - forms under the earth’s surface . Igneous rocks are classified on the basis of their composition and their texture. Representative Image: Igneous intrusion. Magma, and the igneous rock it becomes, has a range of chemical compositions. Felsic rocks are rich in silica, potassium, sodium, and aluminum and contain only small amounts of iron, magnesium, and calcium. Figure 2 schematically illustrates the occurrence of igneous (mafic and felsic) rocks in the LHS, with lithological characteristics of the Kali Gandaki Supergroup and inferred depositional environment (modified from Sakai, Iwano, Danhara, Takigami, et al., 2013) with some age information. The Many Uses of Igneous Rock. Igneous rocks are classified on the basis of their composition and their texture. Common mafic rock samples are basalt and gabbro. INTRODUCTORY GEOLOGY IGNEOUS ROCKS 8.8 STUDENT RESPONSES 1. Of all the igneous rock types basalt and granite are found abundantly in the earth . Mafic igneous rocks. What is Igneous Rock. 45-55%) while felsic is the one with a greater silica content (approx.70-90%). The rocks are classified on the basis of the proportions of the feldspar family of minerals, quartz, and the various dark (iron-rich) minerals like biotite, hornblende, augite and olivine. Intermediate magmas are somewhat more viscous than the mafic magmas. Choose from 500 different sets of geology igneous rocks flashcards on Quizlet. Gabbro. Additionally, they contain somewhat more gas than do the mafic magmas, but not quite as much as the felsic magmas (see below). Obsidian with iron. Four Classifications of Igneous Rocks . Amphibole, pyroxene, and olivine are common in mafic igneous rocks, such as gabbro (composed of pyroxene and plagioclase, with accessory amounts of biotite and amphibole). Felsic rocks know the difference sciencestruck Html url Q webcache Mafic rocks have a relatively low silica . Komatiite is a rare rock because volcanic material that comes directly from the mantle is not common, although some examples can be found in ancient Archean rocks [ 2 ]. The mineral compositions of igneous rocks are usually described as being felsic, intermediate, mafic, or ultramafic (as examples, see Figure 4.7 and Figure 4.8). Diorite. There is a contrasting difference even in the appearance of the two igneous rocks; one being dark shaded and the other having light shade. and felsic or mafic. Heavy, dense, and darker in color Magma, and the igneous rock it becomes, has a range of chemical compositions.For example, basalt is a mafic lava flow rock which originates from melting of the upper mantle. View 4. It is not an all inclusive list but a brief pictorial list of some common igneous rocks. Ore deposits related to mafic igneous rocks • Range from largest, most extensive igneous petrologic systems in the world (e.g., Bushveld Complex) down to moderate-sized bodies like carbonatites. Mafic is a term used by geologists to describe igneous rocks and minerals. Now that we have learned that granite, rhyolite, and other common types of rock are igneous, we can think about all the times we see igneous rocks in day-to-day life.Now you can categorize any granite statue you see around as extrusive or intrusive (remember – can you visually see the crystals of pure composition inside?) The way that magma turns into a solid rock gives it a distinctive igneous texture. The dominant mineral of the rock is alkali feldspar which occurs as large crystals. The term mafic is a combination of the words “magnesium” and “ferric.” The majority of mafic minerals are dark green or greenish black and are medium to coarse-grained. Igneous rocks are classified according to their mineral content: Ultramafic rocks are dominated by olivine and/or pyroxene. If the rock is highly dominated by Magnesium and Iron, it is called Ultramafic. What color are mafic igneous rocks and how much feMg. Sample 11 has what mafic color index (MCI)? Examples of Igneous Rocks Felsic - igneous rock that is more than 65% silica with little Fe, Mg, or Ca. See Some Examples. 1. ROCK FORMING MINERALS 1.) The following is an example of igneous rocks. Igneous Rock # 1. 0-15%MCI 2. b. Fine grained example of intermediate igneous rock. Dark, mostly feMg. Igneous rocks are those that form via the process of melting and cooling. Mineral cleavage and hardness are additional features to help discern between minerals. Basalt and gabbro are the extrusive and intrusive names for mafic igneous rocks, and peridotite is ultramafic, with komatiite as the fine-grained extrusive equivalent. Plutonic rocks are igneous rocks that solidified from a melt at great depth. This lesson will examine the definition of this term and how to relates to earth processes. Felsic rocks are made of light-colored, low-density minerals such as quartz and feldspar. Felsic rocks are rich in silicon, oxygen, aluminium, sodium, and potassium, while the mafic rocks are rich in magnesium and iron. Igneous rocks consist of primarily 12 types of oxides. Accordingly, there are two major types of Igneous rocks are produced viz. For example, basalt is a mafic lava flow rock which originates from melting of the upper mantle. Difference Between Mafic and Felsic Rocks. Typical felsic rocks are dacite and rhyolite. Tend to be light-colored and less dense. The way that magma turns into a solid rock gives it a distinctive igneous texture. Also known as lava rock. Learn geology igneous rocks with free interactive flashcards. First Mafic rocks are darker and denser than Felsic rocks. Mafic - igneous rock that is less than 52% silica and rich in Fe, Mg, and Ca. Course grained example of mafic igneous rock. It is a light coloured rock. A great example of a glass igneous rock is obsidian, which cools quickly on the surface of the earth after erupting from a volcano. Mafic rock is an example of igneous rock which is dominated by olivine, silicates pyroxene, mica, and amphibole. Mafic rock is a dark-colored category of igneous rock, the type of rock that forms from solidified magma. In geology, mafic is a term which describes an igneous rock or a silicate mineral rich in iron and magnesium. Granite: Granite and other rocks of the granite family are the most widely distributed of the deeper plutonic igneous rocks forming the major component of the earth’s crust. Plutons include batholiths, stocks, dikes, sills, laccoliths, lopoliths, and other igneous formations. You may have noticed that there are many kinds of rocks, from the soft sandy rocks that form the cliffs at Scripps beach to the hard rocks … Intrusive igneous are used for a variety of purposes, including decoration, building, stonework, and jewelry. a. Back. Get Price; Igneous Rock Granite. Igneous rocks are derived from the Latin word Ignis which means of fire or heat, the name best describes these rocks since they are born of fire. Rocks composed mostly of hornblende and intermediate plagioclase feldspars make up the intermediate family of igneous rocks. A common mafic rock is basalt. ; Mafic rocks are dominated by plagioclase and pyroxene (even if you can't see them with the naked eye) and smaller amounts of olivine. Beneath the … Igneous rock is one of the three main types of rocks; other ones are sedimentary rocks and metamorphic rocks.Igneous rock is formed from the cooling and solidification of molten magma. Examples of igneous rocks from the mafic (A), intermediate (B), and felsic (C) rock compositions. The name is appropriate because these rocks are born of fire. ES10 - EARTH Lecture 6 - Igneous Rocks Lisa Tauxe Rocks - a brief overview The solid Earth (the mantle and crust) is made of rock. Examples of intrusive igneous rocks are granite, diorite, gabbro, and peridotite. Igneous rocks are basically used in . Gabbro. The four classifications of igneous rocks are ultramafic, mafic, intermediate, and felsic. Igneous Rocks.pdf from GOVT 1403 at Lone Star College System. Lectures 10&11. Examples of metal depleted mafic rocks associated with economic or subeconomic concentrations of Ni-Cu-PGE sulfide mineralization are recognized in several other large igneous provinces: 1. Definitions Gabbro is an example of a mafic rock. The difference in elemental composition causes mafic rocks to be denser than felsic rocks. Introduction As we learned last time, melting of the mantle usually produced basaltic magmas, compositions that are referred to as mafic because of their high proportions of Mg and Fe. Andesite. Therefore, rocks are divided into ultramafic, mafic, intermediate, and felsic. 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