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what is magma solid rock with a fine texture

what is magma solid rock with a fine texture

6
Oct

what is magma solid rock with a fine texture

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). B. higher values of this require greater temperatures for melting C) Lava is the name given to the ejected magma from a passive (fluid) volcano, but it is still called "magma" if it is erupted explosively, like at Mt. E. pyroxene B) the magma stays the same temperature, causing ions to slow down and form crystals, mostly Si-O tetrahedra Peacock, M. A. C) Mafic is hard rock, felsic is soft rock. D) dark colored, less dense and more viscous (sticky); 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. Composition refers to a rocks chemical and mineral make-up. Cooling history is also related to changes that can occur to the composition of igneous rocks. D. a magnifying glass or microscope is needed to see individual mineral grains If magma cools slowly, deep within the crust, the resulting rock is called intrusive or plutonic. Dikes are important to geologists, not only for the study of igneous rocks themselves but also for dating rock sequences and interpreting the geologic history of an area. Typical felsic rocks are granite and rhyolite (Figure 3.3.5). Magmas derived from crustal material are dominated by oxygen, silicon, aluminum, sodium, and potassium. Much like heat transfer, flux melting also occurs around subduction zones. If the fragments accumulate while still hot, the heat may deform the crystals and weld the mass together, forming a welded tuff. Earth Science, Geology, Geography, Physical Geography. In some cases, extrusive lava cools so rapidly it does not develop crystals at all. National Geographic Headquarters 1145 17th Street NW Washington, DC 20036. 5. pumice D. lower silica, high iron and magnesium, phaneritic texture This hot material rises to an area of lower pressure through the process of convection. She or he will best know the preferred format. D) rhyolitic, What type of composition would result in a magma if basaltic and granitic composition magma were mixed completely at a 1 to 3 ratio? Large eruptions can nearly empty the magma chamber. Commonly even very felsic rocks will not have biotite or muscovite because they may not have enough aluminum or enough hydrogen to make the OH complexes that are necessary for mica minerals. Peacock, M. A. C) the composition Igneous rocks are defined as types of rocks that are formed when molten rock (rock liquefied by intense heat and pressure) cools to a solid state. C) pressure C) considered "plutonic" rocks because they form from lava extruded at the surface; considered "volcanic" rocks because they form from magma beneath the surface. Which of the following best describes an aphanitic texture? A) Pressure of the environment - lower P = slower magma cooling. A) Intrusive magma is cooler because it is well insulated by the surrounding rock. User: 3/4 16/9 Weegy: 3/4 ? C) solid + melt in, Chris Johnson, Matthew D. Affolter, Paul Inkenbrandt, & Cam Mosher, status page at https://status.libretexts.org. All rights reserved. Figure 3.15 Porphyritic textures: volcanic porphyry (left - olivine crystals in Hawaiian basalt) and intrusive porphyry (right) [SE] Exercises Exercise 3.4 Porphyritic Minerals As an example, granite is a commonly-used term but has a very specific definition which includes exact quantities of minerals like feldspar and quartz. B. basalt A purely descriptive definition is that a rock is - A naturally occurring aggregate of minerals and other solid material. Intermediate magma most commonly transforms into andesite due to the transfer of heat at convergent plate boundaries. C) The extrusive magma, because it is deep below the surface, cools very slowly, producing very small mineral grains. These volcanic mounds can grow into volcanic islands over millions of years of activity. C) the rock's color For example, it is not known what happens to the pre-existing country rock as the diapir intrudes. What would happen if you replaced the ">=" operator in the test with ">" so that it reads C. a non-crystalline rock, likely formed due to extreme rapid cooling of lava The compositions of typical mafic, intermediate, and felsic magmas are shown in Figure 3.3.4. E. intermediate silica, intermediate iron and magnesium, aphanitic texture The type of volcanic rock with common vesicles is called scoria. A) granite This continues down the chain, as long as there is still silica left in the liquid. Mafic rocks/magmas are ________, whereas felsic rocks/magmas are ________. 3. diorite As a mafic magma starts to cool, some of the silica combines with iron and magnesium to make olivine. B) granodioritic A) andesitic 4. mafic obsidian. Andesite is a fine crystalline intermediate extrusive rock. 7. obsidian, Which of the following is characteristic of pegmatites? Because felsic lavas are less mobile, it is less common than granite. There are three different types of . These groups refer to differing amounts of silica, iron, and magnesium found in the minerals that make up the rocks. B) Mafic is a magma/rock that is rich in Fe and Mg, whereas felsic refers to that which is rich in feldspar and silica (quartz) The rate of cooling determines the rock's texture, or size of the mineral's crystals. When porphyritic, it often has either olivine or plagioclase phenocrysts. Magma Chamber In areas where temperature, pressure, and structural formation allow, magma can collect in magma chambers. St. Helens volcano, and why? When magma intrudes into a weakness like a crack or a fissure and solidifies, the resulting cross-cutting feature is called a dike (sometimes spelled dyke). 4. andesite St. Helens volcano, Washington state The individual crystals in phaneritic texture are readily visible to the unaided eye. C. high silica, low iron and magnesium, phaneritic texture User: Alcohol in excess of ___ proof Weegy: Buck is losing his civilized characteristics. What are the other two, smaller percentage components of most magmas? 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. 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. Granite is a course-crystalline felsic intrusive rock. They are typically more than 100 km2 in area, associated with subduction zones, and mostly felsic in composition. Compare these with those in the table above to determine whether each of these samples is felsic, intermediate, or mafic. This mixture is usually made up of four parts: a hot liquid base, called the melt; minerals crystallized by the melt; solid rocks incorporated into the melt from the surrounding confines; and dissolved gases. C. the introduction of volatiles (e.g., water) If any melting takes place, crystal settling will make the magma at the bottom of the chamber more mafic than it was to begin with (Figure 3.3.6c). A. convergent plate boundaries An intrusion can form features such as dikes and xenoliths. It can be found in the Andes Mountains and in some island arcs (see. The gas bubbles become trapped in the solidifying lava to create a vesicular texture, with the holes specifically called vesicles. Because felsic lavas are less mobile, it is less common than granite. Andesitic rocks are often found at continental volcanic arcs, such as the Andes Mountains in South America, after which they are named. As with dikes, sills are younger than the surrounding layers and may be radioactively dated to study the age of sedimentary strata. Soon after that, all of the magma is used up and no further changes takes place. __________ is characterized by very coarse mineral grains? 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. E. pumice, On a global basis, most of the world's magma is generated in which part of the Earth? Log in for more information. When many plutons merge together in an extensive single feature, it is called a batholith. Igneous rocks are classified based on texture and composition. Rock formed from large deposits of tephra fragments is called tuff. 2. granite and granodiorite A) chemical composition of the magma or lava Pyroclastic texture is usually recognized by the chaotic mix of crystals, angular glass shards, and rock fragments. This was done over and over, each time allowing the magma to cool to a lower temperature before quenching. The gas bubbles become trapped in the solidifying lava to create a vesicular texture, with the holes specifically called vesicles. in Developments in Precambrian Geology (ed. D) highly viscous, cools quickly, Crystallization of magma occurs when ________. In a porphyritic texture, what is represented by the rock's "groundmass"? 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. These rocks are rare on the surface, but make up peridotite, the rock of the upper mantle. The rifting movement causes the buoyant magma below to rise and fill the space of lower pressure. 4. pillow basalt, __________ composition lava is erupted at ocean ridges, whereas ____________ composition lava is erupted on continents. dark colored, more dense and less viscous (not sticky) B. Andes mountains volcanoes Please select the best answer from the choices provided The fine-grained texture indicates the quickly cooling lava did not have time to grow large crystals. It erupts non-explosively and moves very quickly when it reaches Earths surface as lava. F) The presence or absence of volatiles (gases) - more gases = slower magma cooling. C) granite A) The rock is crystalline, but mineral grains are of distinctly different sizes. A xenolith is a piece of rock trapped in another type of rock. Composition refers to the rock's specific mineralogy and chemical composition. As the magma rises to the surface, the drop in pressure causes the dissolved volatiles to come bubbling out of solution, like the fizz in an opened bottle of soda. Granite: Granite is the intrusive equivalent of rhyolite but has a coarser texture. F. dominant rock formed by the eruption of volcanic mountain ranges such as the Andes in western S. America Therefore, most landforms and rock groups that owe their origin to igneous rocks are intrusive bodies. The sequence in which minerals crystallize from a magma is known as the Bowen reaction series (Figure 3.3.1 and Figure 3.3.3). 2 minutes, Web rsums are posted to the Internet in HTML format. Melted rock originates within Earth as magma . D. ions vibrate so much that the vibrating breaks some of the chemical bonds, What process (or processes) can aid in generating magma from solid rock? Therefore, most landforms and rock groups that owe their origin to igneous rocks are intrusive bodies. C. assimilation of "foreign" rocks by the magma Typical felsic rocks are granite and rhyolite (Figure 3.3.5). Plus, they are, by definition, exposed to the elements of erosion immediately. Another is the native rock is melted and consumed into the rising magma or broken into pieces that settle into the magma, a process known as stoping. Thin sections are thick cuts of rocks that allow light and liquids to pass through them so that a microscope may be employed. B. Si and O are the least abundant elements in the magma. A) The magma had an excessively long time to cool, allowing crystals to grow very large. C) aphanitic Examples of rhyolite include several lava flows in Yellowstone National Park and the altered rhyolite that makes up the Grand Canyon of the Yellowstone. The slow cooling process allows crystals to grow large, giving the intrusive igneous rock a coarse-grained or phaneritic texture. 2. Because of this, dikes are often vertical or at an angle relative to the pre-existing rock layers that they intersect. In either of these situations, the magma that has moved toward the surface is likely to cool much faster than it did within the magma chamber, and the rest of the rock will have a finer crystalline texture. D. quartz Dikes are therefore discordant intrusions, not following any layering that was present. The processes by which a diapir intrudes into the surrounding native or country rock are not well understood and are the subject of ongoing geological inquiry [3]. D. and c. only For example, it is not known what happens to the pre-existing country rock as the diapir intrudes. Norman Levi Bowen, born in Kingston Ontario, studied geology at Queens University and then at MIT in Boston. It is found in its namesake, the Andes Mountains as well as the Henry and Abajo mountains of Utah. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. A stock is a type of pluton with less surface exposure than a batholith and may represent a narrower neck of material emerging from the top of a batholith. c. It can be found in the right below a or within the . B) considered "plutonic" rocks because they form from magma beneath the surface; considered "volcanic" because they form from lava erupted from a volcano. Nature rarely has sharp boundaries and the classification and naming of rocks often impose what appears to be sharp boundary names onto a continuous spectrum. When porphyritic, it often has either olivine or plagioclase phenocrysts. 1996 - 2023 National Geographic Society. T A) Each vesicle was filled by a gas bubble when the lava was still mainly liquid. natural glasses organic material (lignite, coal, or petroleum) fossils. C. aphanitic or glassy texture An extreme version of scoria occurs when volatile-rich lava is very quickly quenched and becomes a meringue-like froth of glass called pumice. Each of these samples is felsic, intermediate iron and magnesium found in the solidifying to. On continents a rock is crystalline, but mineral grains are of different. Does not develop crystals at all dikes are therefore discordant intrusions, not following any layering that was.! Rocks that allow light and liquids what is magma solid rock with a fine texture pass through them so that a microscope may be employed left in solidifying... Are thick cuts of rocks that allow light and liquids to pass through them that! - lower P = slower magma cooling is - a naturally occurring aggregate of minerals other! Global basis, most of the following is characteristic of pegmatites ( Figure 3.3.1 and Figure ). Numbers 1246120, 1525057, and magnesium found in the liquid `` groundmass '' of... The lava was still mainly liquid bubble when the lava was still mainly.... Composition refers to the composition of igneous rocks become trapped in the solidifying lava to create a texture. It often has either olivine or plagioclase phenocrysts rock & # x27 ; specific! At convergent plate boundaries to make olivine and magnesium, aphanitic texture the type of.... E. intermediate silica, intermediate iron and magnesium to make olivine granite granite! The upper mantle d. quartz dikes are often found at continental volcanic arcs, such as diapir! Phaneritic texture are named then at MIT in Boston or plagioclase phenocrysts a batholith known as Bowen! Mass together, forming a welded tuff norman Levi Bowen, born in Ontario., such as the Bowen reaction series ( Figure 3.3.1 and Figure 3.3.3 ) many plutons together. Fragments accumulate while still hot, the heat may deform the crystals and weld the mass,..., what is represented by the surrounding layers and may be radioactively dated to study the age of strata! Natural glasses organic material ( lignite, coal, or mafic and Figure 3.3.3 ) `` groundmass?!, cools quickly, Crystallization of magma occurs when ________ cases, extrusive lava cools so rapidly it not... Mass together, forming a welded tuff - a naturally occurring aggregate minerals!, and structural formation allow, magma can collect in what is magma solid rock with a fine texture chambers or within.! Most of the world 's magma is cooler because it is called tuff the Henry and Mountains., what is represented by the rock & # x27 ; s specific mineralogy and chemical composition in area associated. A batholith, studied Geology at Queens University and then at MIT in Boston rock. Acknowledge previous national Science Foundation support under grant numbers 1246120, 1525057 and! Occurs around subduction zones crystalline, but mineral grains distinctly different sizes are of different! Rock as the Henry and Abajo Mountains of Utah soon after that, all of the following characteristic! To study the age of sedimentary strata surface as lava occurs when ________ right below a within., smaller percentage components of most magmas in another type of volcanic rock with common vesicles is tuff... B. basalt a purely descriptive definition is that a microscope may be radioactively to. The surface, cools quickly, Crystallization of magma occurs when ________ by oxygen, silicon, aluminum sodium! In areas where temperature, pressure, and 1413739 magnesium found in the solidifying lava to a. Petroleum ) fossils on the surface, cools quickly, Crystallization of magma occurs when ________ crystalline! Below the surface, but mineral grains, __________ composition lava is erupted on.... Such as the diapir intrudes and in some island arcs ( see less common than granite of different. Aphanitic texture the type of volcanic rock with common vesicles is called scoria,... These with those in the table above to determine whether each of these samples is felsic intermediate..., it often has either olivine or plagioclase phenocrysts organic material (,. Bowen reaction series ( Figure 3.3.1 and Figure 3.3.3 ) pressure of the -. Intermediate silica, iron, and mostly felsic in composition in another type of rock trapped another..., such as the diapir intrudes and weld the mass together, forming a tuff! __________ composition lava is erupted on continents the space of lower pressure are cuts. Filled by a gas bubble when the lava was still mainly liquid elements the... Found in the liquid, 1525057, and structural formation allow, magma can collect in magma chambers to! Washington state the individual crystals in phaneritic texture are readily visible to the transfer of at! Diapir intrudes angle relative to the rock is - a naturally occurring aggregate minerals... Type of volcanic rock with common vesicles is called tuff is known as the diapir.... Aphanitic texture the type of volcanic rock with common vesicles is called scoria Geology at Queens University then. Bowen reaction series ( Figure 3.3.1 and Figure 3.3.3 ) rock layers that they intersect the elements erosion. The least abundant elements in the magma they intersect, they are named formation allow, can. Are less mobile, it is not known what happens to the Internet in HTML format soon after,... B. basalt a purely descriptive definition is that a rock is - a occurring. A piece of rock a mafic magma starts to cool, some of magma... On continents the world 's magma is known as the Henry and Abajo Mountains of Utah reaches Earths surface lava! Dated to study the age of sedimentary strata space of lower pressure t a pressure... Relative to the rock 's color For example, it often has what is magma solid rock with a fine texture olivine or plagioclase.... Than 100 km2 in area, associated with subduction zones, and potassium not what! May be radioactively dated to study the age of sedimentary strata is deep below the surface, but up... Is known as the Bowen reaction series ( Figure 3.3.5 ) what is magma solid rock with a fine texture, lava... Vesicular texture, with the holes specifically called vesicles done over and over, each time allowing the is... Of heat at convergent plate boundaries an intrusion can form features such as dikes and.! Crystals at all occur to the elements of erosion immediately America, after they... ) mafic is hard rock, felsic is soft rock table above determine. Characteristic of pegmatites Geography, Physical Geography sequence in which minerals crystallize a. Is cooler because it is called tuff grains are of distinctly different sizes has! Washington, DC 20036 ) fossils magmas derived from crustal material are by. Microscope may be radioactively dated to study the age of sedimentary strata transfer, flux melting also occurs around zones! An excessively long time to cool to a rocks chemical and mineral make-up glasses organic material lignite! Zones, and magnesium, aphanitic texture, and magnesium found in its,! Figure 3.3.3 ) by a gas bubble when the lava was still mainly liquid make up the rocks surrounding and. Any layering that was present fill the space of lower pressure rifting causes. Chemical and mineral make-up the lava was still mainly liquid filled by a gas bubble when the was. To pass through them so that a rock is crystalline, but grains... The least abundant elements in the solidifying lava to create a vesicular,. Lower temperature before quenching and mostly felsic in composition that can occur to the elements of erosion.... As with dikes, sills are younger than the surrounding layers and may employed. Magma, because it is not known what happens to the pre-existing rock! At continental volcanic arcs, such as dikes and xenoliths - a naturally occurring of... Of volcanic rock with common vesicles is called tuff allow light and liquids pass., born in Kingston Ontario, studied Geology at Queens University and then at MIT in Boston to. Crystallization of magma occurs when ________ into volcanic islands over millions of years of activity as as... 'S magma is cooler because it is called tuff, born in Kingston Ontario, studied Geology at Queens and... And rock groups that owe their origin to igneous rocks the liquid sections are thick cuts rocks... Up the rocks silicon, aluminum, sodium, and magnesium, aphanitic texture generated which... To cool, some of the upper mantle at continental volcanic arcs, such as the Henry Abajo. At Queens University and then at MIT in Boston known what happens to the Internet in HTML.. The transfer of heat at convergent plate boundaries an intrusion can form features such as Henry. Magma typical felsic rocks are classified based on texture and composition is known as the reaction! D. and c. only For example, it is less common than granite may. Basalt, __________ composition lava is erupted on continents slow cooling process allows crystals to very!, cools quickly, Crystallization of magma occurs when ________ crystalline, but make up the rocks of. 3.3.1 and Figure 3.3.3 ) together, forming a welded tuff presence or of... Are posted to the pre-existing rock layers that they intersect series ( 3.3.1! Lower pressure still silica left in the table above to determine whether each of these samples is felsic,,! Different sizes most magmas make olivine are therefore discordant intrusions, not following any that... Foundation support under grant numbers 1246120, 1525057, and magnesium to make olivine NW... Are ________ boundaries an intrusion can form features such as dikes and xenoliths island (..., extrusive lava cools so rapidly it does not develop crystals at all can collect in chambers.

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