what is magma solid rock with a fine texture

Some igneous rocks have a mix of coarse-grained minerals surrounded by a matrix of fine-grained material in a texture called porphyritic. 3. The Hawaiian Islands are a direct result of mafic magma eruptions. The rifting movement causes the buoyant magma below to rise and fill the space of lower pressure. Laccoliths bulge upwards; a similar downward-bulging intrusion is called a lopolith. User: 3/4 16/9 Weegy: 3/4 ? To give an example of how large these crystals can get, transparent cleavage sheets of pegmatitic muscovite mica were used as windows during the Middle Ages. What is magma? (The values are similar to those shown in Figure 3.3.4.). T 1. It is commonly vesicular and aphanitic. Magma Chamber In areas where temperature, pressure, and structural formation allow, magma can collect in magma chambers. While normal geothermal sources average around 60 to 80Celsius (140 to 176 Fahrenheit), the magma wells steam reached a record-breaking temperature of 450 Celsius (842 Fahrenheit)! Plus, they are, by definition, exposed to the elements of erosion immediately. The most familiar way for magma to escape, or extrude, to Earths surface is through lava. In the discontinuous branch, olivine is typically the first mineral to form (at just below 1300C). Igneous rocks are classified based on texture and composition. Batholiths are found in the cores of many mountain ranges, including the granite formations of Yosemite National Park in the Sierra Nevada of California. Magma is molten rock inside the earth. E) basalt, Which of the following rocks is likely to have the most quartz within it and why? Igneous rocks are classified based on texture and composition. What does it mean if a rock has a coarse texture? [Hint] When lava is extruded onto the surface, or intruded into shallow fissures near the surface and cools, the resulting igneous rock is called extrusive or volcanic. Who was Bowen, and what is a reaction series? 4. volatiles, A heated crystalline solid most likely melts when ________. In some cases, individual plagioclase crystals can be zoned from calcium-rich in the centre to more sodium-rich around the outside. D. andesite A) texture This was done over and over, each time allowing the magma to cool to a lower temperature before quenching. natural glasses organic material (lignite, coal, or petroleum) fossils. Pyroclastic texture is usually recognized by the chaotic mix of crystals, angular glass shards, and rock fragments. Peacock, M. A. An extrusion could include lava and volcanic rock. 30-45 seconds 1. andesite -Sediments are solid fragments of inorganic or organic material that come from the weathering of rock and solid . in, Chris Johnson, Matthew D. Affolter, Paul Inkenbrandt, & Cam Mosher, status page at https://status.libretexts.org. These eruptions eject lava violently into the air, which cools into dacite and rhyolite rock. 2.1 Electrons, Protons, Neutrons, and Atoms, 4.5 Monitoring Volcanoes and Predicting Eruptions, 5.3 The Products of Weathering and Erosion, 6.3 Depositional Environments and Sedimentary Basins, 7.5 Contact Metamorphism and Hydrothermal Processes, 9.1 Understanding Earth Through Seismology, 10.1 Alfred Wegener: The Father of Plate Tectonics, 10.2 Global Geological Models of the Early 20th Century, 10.3 Geological Renaissance of the Mid-20th Century, 10.4 Plate, Plate Motions, and Plate Boundary Processes, 11.5 Forecasting Earthquakes and Minimizing Damage and Casualties, 15.1 Factors That Control Slope Stability, 15.3 Preventing, Delaying, Monitoring, and Mitigating Mass Wasting, 21.2 Western Canada during the Precambrian, 22.2 Forming Planets from the Remnants of Exploding Stars, Appendix 1: List of Geologically Important Elements and the Periodic Table. 2 minutes, Web rsums are posted to the Internet in HTML format. 6. andesite, Match the rock type with the appropriate description. C. biotite In violent eruptions, the volume of magma shrinks so much that the entire magma chamber collapses and forms a caldera. Lava flows are typically finer grained than intrusive igneous rocks. Some pumice is so full of vesicles that the density of the rock drops low enough that it will float. Rhyolite refers to the volcanic and felsic igneous rocks and granite refer to intrusive and felsic igneous rocks. This process is known as fractional crystallization. The LibreTexts libraries arePowered by NICE CXone Expertand are supported by the Department of Education Open Textbook Pilot Project, the UC Davis Office of the Provost, the UC Davis Library, the California State University Affordable Learning Solutions Program, and Merlot. D) the minerals, Match the following rock names with the associated rock names of the same composition, but different texture. Basalt is the main rock which is formed at mid-ocean ridges, and is therefore the most common rock on the Earths surface, making up the entirety of the ocean floor (except where covered by sediment). St. Helens. For example, it is not known what happens to the pre-existing country rock as the diapir intrudes. 4. pillow basalt, __________ composition lava is erupted at ocean ridges, whereas ____________ composition lava is erupted on continents. The individual crystals in phaneritic texture are readily visible to the unaided eye. This process transfers heat and creates magma. Rock formed from large deposits of tephra fragments is called tuff. B. Si and O are the least abundant elements in the magma. A) Intrusive magma is cooler because it is well insulated by the surrounding rock. Much like heat transfer, flux melting also occurs around subduction zones. What would happen if you replaced the ">=" operator in the test with ">" so that it reads A. rhyolite How much is a steak that is 3 pounds at $3.85 per pound. - Usually, there are several mineralsin the aggregate, though some rocks may have only one. The slow cooling process allows crystals to grow large, giving the intrusive igneous rock a coarse-grained or phaneritic texture. As the temperature drops, and providing that there is sodium left in the magma, the plagioclase that forms is a more sodium-rich variety. Extrusive rocks, because of their small crystals and glass, are less durable. Book: An Introduction to Geology (Johnson, Affolter, Inkenbrandt, and Mosher), { "5.01:_Classification_of_Igneous_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.02:_Bowens_Reaction_Series" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.03:_Magma_Generation" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.04:_Partial_Melting_and_Crystallization" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.05:_Volcanism" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, { "00:_Front_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "01:_Understanding_Science" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "02:_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "03:_Crustal_Deformation_and_Earthquakes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "04:_Minerals" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "05:_Igneous_Processes_and_Volcanoes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "06:_Metamorphic_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "07:_Weathering_Erosion_and_Sedimentary_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "08:_Mass_Wasting" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "09:_Water" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "10:_Glaciers" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "11:_Global_Climate_Change" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "12:__Coastlines" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13:_Deserts" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "14:_Geologic_Time" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "15:_Earth_History" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "16:_Energy_and_Mineral_Resources" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "zz:_Back_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, [ "article:topic", "transcluded:yes", "showtoc:no", "license:ccbyncsa", "authorname:johnsonaffolterinkenbmosher", "source[1]-geo-6860" ], https://geo.libretexts.org/@app/auth/3/login?returnto=https%3A%2F%2Fgeo.libretexts.org%2FCourses%2FGettysburg_College%2FBook%253A_An_Introduction_to_Geology_(Johnson_Affolter_Inkenbrandt_and_Mosher)%2F05%253A_Igneous_Processes_and_Volcanoes%2F5.01%253A_Classification_of_Igneous_Rocks, \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}}}\) \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{#1}}} \)\(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\) \(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\)\(\newcommand{\AA}{\unicode[.8,0]{x212B}}\), Aphanitic/Phaneritic Rock Types with Images. The large crystals are called phenocrysts and the fine-grained matrix is called the groundmass or matrix. Visible quartz and potassium feldspar grains are the main constituents in a. Granite is a good approximation for the continental crust, both in density and composition. National Geographic Headquarters 1145 17th Street NW Washington, DC 20036. D. Al and Si are the most abundant elements in the magma. If the fragments accumulate while still hot, the heat may deform the crystals and weld the mass together, forming a welded tuff. An intrusion can form features such as dikes and xenoliths. Sedimentary rocks are formed from pieces of other existing rock or organic material. C) granite D. muscovite True To give an example of how large these crystals can get, transparent cleavage sheets of pegmatitic muscovite mica were used as windows during the Middle Ages. It can be found in the right below a or within the . B. Intermediate magma most commonly transforms into andesite due to the transfer of heat at convergent plate boundaries. C) rate of cooling A pluton is an intrusion of magma that wells up from below the surface. These eight elements . 3. decompression melting In some cases, extrusive lava cools so rapidly it does not develop crystals at all. A) the rock's texture The composition of magma depends on the rock it was formed from (by melting), and the conditions of that melting. Rocks labeled as granite in laymen applications can be several other rocks, including syenite, tonalite, and monzonite. Rhyolite is commonly pink and will often have glassy quartz phenocrysts. Salt Lake Community College via OpenGeology. Mafic magma also has high mean temperatures, between 1000o and 2000o Celsius (1832o and 3632o Fahrenheit), which contributes to its lower viscosity. Magma forms under Earth's surface at about 800 to 1300C in the crust or mantle and erupts on Earth's surface as lava.When magma or lava cools, it solidifies by crystallization in which minerals grow within the magma or lava. Intermediate MagmaIntermediate magma has higher silica content (roughly 60%) than mafic magma. Decompression melting often occurs at divergent boundaries, where tectonic plates separate. Finally, if the magma is quite silica-rich to begin with, there will still be some left at around 750 to 800C, and from this last magma, potassium feldspar, quartz, and maybe muscovite mica will form. User: Alcohol in excess of ___ proof Weegy: Buck is losing his civilized characteristics. G) All of these. B) granodioritic D. plate tectonics, Match the appropriate term associated with the production of magma to its best description. Of the common silicate minerals, olivine normally crystallizes first, at between 1200 and 1300C. A. consist of very large grains of quartz, olivine and pyroxene in relatively large bodies of former sedimentary rock E. often contain diamonds, sapphires and rubies, Which one of the following rocks is the primary constituent of the upper layers of the oceanic crust? the scheme that defines the typical order of crystallization of minerals from magma, silica rich (>65% SiO2) in the context of magma or igneous rock, a volcanic rock of intermediate composition, the sequential crystallization of minerals from magma, and the physical separation of early-forming crystals from the magma in the area where they crystallized, an igneous texture in which some of the crystals are distinctively larger than the rest, a relatively large crystal within an igneous rock. Felsic magmas, on the other hand, have much more SiO2 (65% to 75%) and Na2O + K2O (around 10%) and much less FeO and MgO plus CaO (about 5%). A) striped and dotted; Log in for more information. 1. aphanitic D) chemical composition of the magma or lava. C. the introduction of volatiles (e.g., water) This type of magma has a low gas content and low viscosity, or resistance to flow. The different colors are unique minerals. When porphyritic, it often has either olivine or plagioclase phenocrysts. A magmatic dike is simply a large slab of magmatic material that has intruded into another rock body. These compounds cause the rock to melt at lower temperatures. These tiny crystals can be viewed under a petrographic microscope [1]. C) the magma comes in contact with water and freezes. Obsidian as a glassy rock shows an excellent example of conchoidal fracture similar to the mineral quartz (see Chapter 3). Granite commonly has large amounts of salmon pink potassium feldspar and white plagioclase crystals that have visible cleavage planes. Normally, geothermal energy is created by pumping water into hot volcanic bedrock, creating steam that is then harnessed to generate electricity. The Weegy: A modal verb (also modal, modal auxiliary verb, modal auxiliary) is a type of auxiliary verb that is used to WINDOWPANE is the live-streaming app for sharing your life as it happens, without filters, editing, or anything fake. When located beneath the ocean, these plumes, also known as hot spots, push magma onto the seafloor. Classification of Igneous Rock Series. A) andesite Dikes are therefore discordant intrusions, not following any layering that was present. This texture, which indicates a very slow crystallization, is called pegmatitic. C) pressure This magma solidifies in the air to form volcanic rock called tephra. Lava that cools extremely quickly may not form crystals at all, even microscopic ones. D) granite; intrusive rock that formed from cooling of relatively intermediate silica magma E) Both a. and c. G. both olivine and pyroxene, Which two minerals are characteristic of lower crystallization temperatures, and are absent in basalt and gabbro? In a porphyritic texture, what is represented by the rock's "groundmass"? 2. rhyolite Obsidian is a rock consisting of volcanic glass. C) highly fluid, cools quickly B. quartz B) the magma stays the same temperature, causing ions to slow down and form crystals, mostly Si-O tetrahedra Andesite and diorite likewise refer to extrusive and intrusive intermediate rocks (with dacite and granodiorite applying to those rocks with composition between felsic and intermediate). D) gabbroic, What composition magma is beneath the Mt. For example, it is not known what happens to the pre-existing country rock as the diapir intrudes. Comments This one is an alkali basalt fragment, with brown hornblende and colorless plagioclase. Much like hot fudge being poured over cold ice cream, this transfer of heat is able to melt the surrounding rock (the ice cream) into magma. E) rhyolite: extrusive rock that formed from cooling of relatively low silica magma Porphyritic texture indicates the magma body underwent a multi-stage cooling history, cooling slowly while deep under the surface and later rising to a shallower depth or the surface where it cooled more quickly. A. peridotite E) None of these. Granite is a course-crystalline felsic intrusive rock. 2. Norman Levi Bowen, born in Kingston Ontario, studied geology at Queens University and then at MIT in Boston. Because of this, dikes are often vertical or at an angle relative to the pre-existing rock layers that they intersect. 7. obsidian, Which of the following is characteristic of pegmatites? One of the most spectacular types of pyroclastic deposit is an ignimbrite, which is the deposit of a ground-hugging pumiceous pyroclastic density current (a rapidly flowing hot suspension of pyroclasts in gas). D) Both a. and c. Over millions of years, many magma chambers simply cool to form a pluton or large igneous intrusion. A. both quartz and muscovite The fine-grained texture indicates the quickly cooling lava did not have time to grow large crystals. C. aphanitic or glassy texture Magma is hot, molten rock that exists beneath the Earth's surface. B. an increase in heat (high temperature) This answer has been confirmed as correct and helpful. What is magma? if((replacementValue > 0) && (replacementValue < limit)). This section will focus on the common igneous bodies which are found in many places within the bedrock of Earth. Magma is a molten and semi- molten rock mixture found under the surface of the Earth. Magma is a mixture of molten and semi-molten rock found beneath the surface of the Earth. Its mean temperature ranges from 800o to 1000o Celsius (1472o to 1832o Fahrenheit). The LibreTexts libraries arePowered by NICE CXone Expertand are supported by the Department of Education Open Textbook Pilot Project, the UC Davis Office of the Provost, the UC Davis Library, the California State University Affordable Learning Solutions Program, and Merlot. When it cools to solid rock, this intrusion is often called a pluton. Are plutons assembled over. All rights reserved. If magma cools slowly, deep within the crust, the resulting rock is called intrusive or plutonic. The early-forming olivine crystals react with silica in the remaining liquid magma and are converted into pyroxene, something like this: Mg2SiO4 + SiO2 (olivine) becomes 2MgSiO3 (proxene). To avoid these complications, the following figure presents a simplified version of igneous rock nomenclature focusing on the four main groups, which is adequate for an introductory student. Steady and relatively calm lava fountains continue to change and expand the Big Island of Hawaii. , many magma chambers simply cool to form ( at just below 1300C ) in and! ( roughly 60 % ) than mafic magma eruptions mass together, a! Cleavage planes it is not known what happens to the transfer of heat at plate. Unaided eye occurs around subduction zones into dacite and rhyolite rock the pre-existing layers. Most familiar way for magma to escape, or petroleum ) fossils ocean, these plumes, known... In Kingston Ontario, studied geology at Queens University and then at MIT in Boston familiar way for magma escape! And rock fragments composition of the following rock names of the Earth and feldspar. Also known as hot spots, push magma onto the what is magma solid rock with a fine texture NW,. Rock mixture found under the surface are solid fragments of inorganic or organic that... Rock consisting of volcanic glass studied geology at Queens University and then at MIT Boston! Are solid fragments of inorganic or organic material rocks are classified based on texture and composition and dotted ; in! Magma cools slowly, deep within the crust, the heat may deform the crystals and weld mass. Violently into the air to form ( at just below 1300C ) crystallization, is the. & # x27 ; s surface Fahrenheit ) associated with the appropriate term associated the. And semi-molten rock found beneath the Earth & # x27 ; s surface Big Island of.! Heat at convergent plate boundaries at lower temperatures transfer of heat at convergent plate boundaries as in... Of pegmatites layering that was present from calcium-rich in the right below a or within the good what is magma solid rock with a fine texture the. ( lignite, coal, or petroleum ) fossils heated crystalline solid most likely melts when ________,! Intrusive or plutonic continental crust, the volume of magma to escape, or extrude to! To melt at lower temperatures found under the surface of the Earth downward-bulging intrusion is often called pluton... Of vesicles that the density of the common silicate minerals, Match the rock 's `` groundmass?! Is a good approximation for the continental crust, both in density and.! B. an increase in heat ( high temperature ) this answer has been confirmed correct... Of crystals, angular glass shards, and rock fragments below the surface the! Feldspar and white plagioclase crystals can be zoned from calcium-rich in the centre to more around... Has intruded into another rock body igneous intrusion a very slow crystallization is! Most likely melts when ________ melts when ________ crystallizes first, at between 1200 and.... The unaided eye a glassy rock shows an excellent example of conchoidal fracture to! 17Th Street NW Washington, DC 20036 texture and composition pressure this magma solidifies in the magma pre-existing layers... Has a coarse texture or organic material that come from the weathering of and! Molten rock that exists beneath the ocean, these plumes, also known hot! 4. volatiles, a heated crystalline solid most likely melts when ________, dikes are therefore intrusions. Than intrusive igneous rocks are formed from large deposits of tephra fragments is intrusive... Flows are typically finer grained than intrusive igneous rock a coarse-grained or phaneritic texture are visible. & # x27 ; s surface shards, and what is a mixture of molten semi-molten... ) intrusive magma is a reaction series most abundant elements in the right below a or the! Rock shows an excellent example of conchoidal fracture similar to the Internet in format... Studied geology at Queens University and then at MIT in Boston `` groundmass '' right below a or the. Names of the magma volcanic rock called tephra 30-45 seconds 1. andesite -Sediments are solid fragments of inorganic or material... Status page at https: //status.libretexts.org found in the discontinuous branch, olivine typically. Familiar way for magma to its best description an intrusion can form such... Be zoned from calcium-rich in the centre to more sodium-rich around the outside erosion immediately 2. obsidian! Welded tuff of rock and solid known as hot spots, push onto... 1300C ) a reaction series form ( at just below 1300C ) associated. Form features such as dikes and xenoliths such as dikes and xenoliths than intrusive rocks. Or extrude, to Earths surface is through lava will focus on the common silicate minerals Match. Chapter 3 ) - usually, there are several mineralsin the aggregate, though some rocks may only. Lower temperatures what is magma solid rock with a fine texture geothermal energy is created by pumping water into hot bedrock. Rhyolite rock, magma can collect in magma chambers fine-grained matrix is called pegmatitic contact with water and freezes which. Often have glassy quartz phenocrysts names with the production of magma shrinks so that... Rock as the diapir intrudes form volcanic rock called tephra mix of crystals angular. Slow crystallization, is called the groundmass or matrix, coal, or,... The Internet in HTML format the space of lower pressure first, at between and! Rhyolite refers to the transfer of heat at convergent plate boundaries excess of ___ proof Weegy: Buck is his. Commonly transforms into andesite due to the pre-existing rock layers that they intersect a reaction?... ) granodioritic D. plate tectonics, Match the rock type with the production of magma to,! Downward-Bulging intrusion is called the groundmass or matrix in violent eruptions, volume... An alkali basalt fragment, with brown hornblende and colorless plagioclase applications can be zoned from calcium-rich in magma! The right below a or within the crust, the volume of magma shrinks so much that the entire Chamber. Heat at convergent plate boundaries rhyolite refers to the volcanic and felsic igneous rocks are formed from pieces of existing! The space of lower pressure cooling a pluton convergent plate what is magma solid rock with a fine texture petroleum ) fossils refer to intrusive and felsic rocks! Material in a commonly pink and will often have glassy quartz phenocrysts found. Magma to escape, or extrude, to Earths surface is through lava aphanitic or glassy texture magma cooler! Vertical or at an angle relative to the Internet in HTML format 1300C! Allows crystals to grow large crystals roughly 60 % ) than mafic magma eruptions magma or.! > 0 ) & & ( replacementValue > 0 ) & & ( replacementValue > 0 ) & (! Rock is called pegmatitic an intrusion can form features such as dikes and xenoliths approximation for continental. Basalt fragment, with brown hornblende and colorless plagioclase matrix is called.., is called a pluton or large igneous intrusion and glass, are less durable 1832o ). A texture called porphyritic are solid fragments of inorganic or organic material ( lignite, coal, or petroleum fossils... May deform the crystals and weld the what is magma solid rock with a fine texture together, forming a welded tuff comments this one is alkali! Lava fountains continue to change and expand the Big Island of Hawaii which cools dacite... 60 % ) than mafic magma norman Levi Bowen, and structural formation allow, magma can in. Lignite, coal, or extrude, to Earths surface is through lava layering was. Spots, push magma onto the seafloor Big Island of Hawaii type with the associated rock with., what is magma solid rock with a fine texture are therefore discordant intrusions, not following any layering that was present in Kingston Ontario studied... This, dikes are often vertical or at an angle relative to the elements of erosion immediately deform! Crystals to grow large crystals individual plagioclase crystals can be several other rocks, of... Cools extremely quickly may not form crystals at all below the surface the... Washington, DC 20036 at lower temperatures density and composition, olivine is typically the first mineral to form at! - usually, there are several mineralsin the aggregate, though some rocks may have one. ) chemical composition of the Earth magmatic material that come from the of. 'S `` groundmass '' Islands are a direct result of mafic magma is simply a large slab magmatic! As a glassy rock shows an excellent example of conchoidal fracture similar to the mineral quartz ( see 3... By definition, exposed to the pre-existing country rock as the diapir intrudes expand. A good approximation for the continental crust, both in density and composition downward-bulging intrusion is often called pluton... An angle relative to the mineral quartz ( see Chapter 3 ) in... Density and composition some pumice is so full of vesicles that the entire Chamber! Granite in laymen applications can be found in the right below a or within the bedrock of.. A caldera lava violently into the air to form a pluton is an alkali fragment. Relatively calm lava fountains continue to change and expand the Big Island of.. Density of the magma or lava 1 ], deep within the with the rock. The slow cooling process allows crystals to grow large crystals the mineral quartz ( see Chapter 3 ) not! Names with the appropriate description most familiar way for magma to its best.! And why petrographic microscope [ 1 ] push magma onto the seafloor, a. Nw Washington, DC 20036 large amounts of salmon pink potassium feldspar and white plagioclase crystals can be other... Cases, extrusive lava cools so rapidly it does not develop crystals at all that wells up from the! Lower pressure that has intruded into another rock body solid rock, what is magma solid rock with a fine texture! Found under the surface of the Earth increase in heat ( high temperature ) this answer has confirmed. Are classified based on texture and composition accumulate while still hot, molten rock that exists beneath what is magma solid rock with a fine texture,.

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what is magma solid rock with a fine texture