<\/p>\n
– The magma<\/strong><\/strong> forming this lava is often felsic, with high-to-intermediate levels of silica, and less mafic magma<\/strong><\/strong>.\n<\/p>\n <\/p>\n – The Snake River Plain was formed by magma<\/strong> rising up below the North American Plate.\n<\/p>\n <\/p>\n – The rocks are Intrusiveplutonic, formed when molten magma<\/strong> is trapped under the Earth’s surface and cools into a crystalline mass.\n<\/p>\n <\/p>\n – Melted material from the mantle and crust moves up through the crust and collects in magma<\/strong> chambers.\n<\/p>\n <\/p>\n – Aqua and Magma<\/strong><\/strong> agents and the leaders, Archie, leader of Aqua, and Maxie, leader of Magma<\/strong><\/strong>, play a part in Pok\u00e9mon R\/S\/E.\n<\/p>\n <\/p>\n – During certain types of gigantic eruptions, the volcano’s magma<\/strong> chamber may empty enough for an area above it to subside.\n<\/p>\n – In a volcanic eruption, Magma<\/strong> is blown apart by volcanic gases and steam.\n<\/p>\n <\/p>\n – From these magma<\/strong> erupts as gases, lava, and ejecta.\n<\/p>\n <\/p>\n – The motivating force for seafloor spreading ridges is tectonic plate pull rather than magma<\/strong><\/strong> pressure, although there is typically significant magma<\/strong><\/strong> activity at spreading ridges.Tan, Yen Joe, et al.\n<\/p>\n <\/p>\n – He played in the progressive rock\/jazz fusion band Magma<\/strong> in the 1970s.\n<\/p>\n <\/p>\n – New magma<\/strong> of basalt composition emerges at and near the axis because of decompression melting in the underlying Earth’s mantle.\n<\/p>\n <\/p>\n – Immediately after the impact, the Earth’s mantle was vigorously convectionconvecting, the surface was a large magma<\/strong> ocean.\n<\/p>\n <\/p>\n – As the rock slowly cools into a solid, the different parts of the magma<\/strong> Crystallizationcrystallize into minerals.\n<\/p>\n <\/p>\n – Feldspar forms crystals from magma<\/strong> in both intrusive and extrusive rocks, and they can also happen as compact minerals, as veins, and are also present in many types of metamorphic rock.\n<\/p>\n <\/p>\n – When magma<\/strong> comes out from the ground in a volcano it is called lava.\n<\/p>\n <\/p>\n – The crystallized magma<\/strong> forms new crust of basalt and gabbro.\n<\/p>\n <\/p>\n – Felsic magma<\/strong> is thick and has silica minerals.\n<\/p>\n <\/p>\n – These particles are small, slaggy pieces of magma<\/strong> and rock that have been tossed into the air by outbursts of steam and other gases.\n<\/p>\n <\/p>\n – The giant Norilsk nickel-copper-palladium deposit formed within the magma<\/strong> flows in the main Siberian Traps.\n<\/p>\n <\/p>\n – The name of the magma<\/strong> would be “The integers under multiplication”.\n<\/p>\n <\/p>\n – Changes in stress caused by large earthquakes may be enough to cause volcanovolcanic eruptions, when the magma<\/strong> system of the volcano is close to a critical state.\n<\/p>\n <\/p>\n – The changes that occur are greatest where the magma<\/strong> comes into contact with the rock.\n<\/p>\n <\/p>\n – It has its own magma<\/strong> plumbing under the Earth that goes down under the Earths crust by 60 km.\n<\/p>\n <\/p>\n – Sometimes, the magma<\/strong> comes out quickly and sometimes it comes slowly.\n<\/p>\n <\/p>\n – When large tectonic plates collided about 100 million years, magma<\/strong> escaped between these plates and solidified between other rocks.\n<\/p>\n <\/p>\n – These planes or weakened areas allow the intrusion of a thin sheet-like body of magma<\/strong> paralleling the existing strata.\n<\/p>\n <\/p>\n – Then magma<\/strong> enters these lines of weakness.\n<\/p>\n <\/p>\n – The magma<\/strong><\/strong> does not have to reach the surface in order to create a mountain: magma<\/strong><\/strong> that solidifies below ground can still form dome mountains, such as Navajo Mountain in the states of Utah and Arizona, in the United States.\n<\/p>\n <\/p>\n – New magma<\/strong> emerges onto the ocean floor near the ridge axis.\n<\/p>\n <\/p>\n – Sometimes the amount of magma<\/strong> erupted is so large that the top of the volcano collapses.\n<\/p>\n <\/p>\n – The great earthquake in 1707 may have changed pressure in the magma<\/strong> under Mount Fuji.\n<\/p>\n <\/p>\n – Then we give the magma<\/strong> the label.\n<\/p>\n <\/p>\n – Sills are fed by dykes as they form from a lower magma<\/strong> source.\n<\/p>\n <\/p>\n – Such melting can take place near a hotspot, resulting in a mixture of magma<\/strong><\/strong> from the depths of the hotspot with superficial magma<\/strong><\/strong> produced by a mantle plume.\n<\/p>\n <\/p>\n – However, magma<\/strong> was found under the ground three times in geothermal drilling projects twice in Iceland and once in Hawaii.\n<\/p>\n <\/p>\n – This sudden uplift was likely caused by rising magma<\/strong> of the Mackenzie plume, which caused the Mackenzie hotspot.\n<\/p>\n <\/p>\n – Other volcanic mountains form over hot spots, pockets of magma<\/strong> beneath the crust which erupt onto Earth’s surface.\n<\/p>\n <\/p>\n – The study of magma<\/strong> is usually done in lava flows.\n<\/p>\n <\/p>\n – The cause of these earthquakes is believed to be the rising of molten magma<\/strong> because there are no faults or tectonic plate boundaries.\n<\/p>\n <\/p>\n – The existing rocks must split to create the planes along which the magma<\/strong> moves in.\n<\/p>\n <\/p>\n – At these ridges, hot magma<\/strong> rises into the crust and cools, pushing the crust apart at the ridge.\n<\/p>\n <\/p>\n – The teams Aqua and Magma<\/strong> did not play a part in the anime very much.\n<\/p>\n <\/p>\n – The magma<\/strong> is forced between other layers of rock by the pressure under the Earth’s surface.\n<\/p>\n <\/p>\n – Large bodies of magma<\/strong> that solidify underground before they reach the surface of the crust are called plutons.\n<\/p>\n <\/p>\n – Team Aqua and Team Magma<\/strong> are the two feuding crime syndicates in the Hoenn region and in the games “Pok\u00e9mon Ruby, Sapphire, and Emerald” as well as their remakes “Omega Ruby” and “Alpha Sapphire”.\n<\/p>\n <\/p>\n – Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma<\/strong> break apart the plates at the spreading centers.\n<\/p>\n <\/p>\n – As it forms, a plug may cause an extreme build-up of pressure if gas-charged magma<\/strong> is trapped beneath it.\n<\/p>\n <\/p>\n – In such an eruption the volcano’s magma<\/strong> chamber is empty enough for the ground above it to drop.\n<\/p>\n <\/p>\n – Mid-ocean ridges are geologically active, with new magma<\/strong> constantly emerging onto the ocean floor and into the crust at and near rifts along the ridge axes.\n<\/p>\n <\/p>\n – Xenoliths may be covered in the margins of a magma<\/strong> chamber, torn loose from the walls of a flow of lava or picked up along the ground by flowing lava on Earth’s surface.\n<\/p>\n <\/p>\n – It has been estimated that it was four times larger than the 1883 eruption of Krakatoa, between Java and Sumatra, in terms of volume of magma<\/strong> ejected.\n<\/p>\n <\/p>\n – Many types of minerals are made when molten rock, or magma<\/strong> cools and turns into a solid.\n<\/p>\n <\/p>\n – These felsic protocontinents probably formed at hot spots rather than subduction zones, from a variety of sources: mafic magma<\/strong> melting more felsic rocks, partial melting of mafic rock, and from the metamorphic alteration of felsic sedimentary rocks.\n<\/p>\n <\/p>\n – Subaerial-submarine evidence of structures feeding magma<\/strong> to Stromboli Volcano, Italy, and relations with edifice flank failure and creep.\n<\/p>\n <\/p>\n – Officials said hundreds of volcanic earthquakes had been recorded on the mountain over the weekend of 23\u201324 October, and that the magma<\/strong> had risen to about 1 kilometre below the surface due to the seismic activity.\n<\/p>\n <\/p>\n – Several new features were seen, such as the “whaleback” which is solid magma<\/strong><\/strong> being pushed to the top of the volcano by magma<\/strong><\/strong> under it.\n<\/p>\n <\/p>\n – Some magma<\/strong> may even reach the Earth’s surface as lava.\n<\/p>\n <\/p>\n – Igneous rocks are formed when molten magma<\/strong> cools, either above or below the surface.\n<\/p>\n <\/p>\n – The molten magma<\/strong> under great pressure forces its way through the fissure of underground rocks and reaches the Earth’s surface to form “igneous extrusion”.\n<\/p>\n <\/p>\n – An intrusion is magma<\/strong> which cools and becomes solid under the Earth’s surface.\n<\/p>\n <\/p>\n – Lava or magma<\/strong> can cause weathering when molten rock touches older rock.\n<\/p>\n <\/p>\n – As the magma<\/strong> cools, these minerals form crystals.\n<\/p>\n <\/p>\n – They formed about 300,000 years ago when magma<\/strong> from the Geomonoreum parasitic volcano cooled.\n<\/p>\n <\/p>\n – It happens most in igneous rock when magma<\/strong> is fluid enough to flow round more solid rock.\n<\/p>\n <\/p>\n – The Watchung basalt flows of the Watchung Mountains are eruptions onto the surface of the same magma<\/strong> that created the Palisades Sill.Kodama K.P., 1983.\n<\/p>\n <\/p>\n![\"Some](\"https:\/\/englishteststore.net\/blog\/wp-content\/uploads\/2021\/09\/Some-in-sentence-examples-of-magma.jpg\" "\\"Some")
Example sentences of “magma”:<\/h2>\n
- In a volcanic eruption, Magma<\/strong> is blown apart by volcanic gases and steam.\r\n
- From these magma<\/strong> erupts as gases, lava, and ejecta.\r\n
- The motivating force for seafloor spreading ridges is tectonic plate pull rather than magma<\/strong><\/strong> pressure, although there is typically significant magma<\/strong><\/strong> activity at spreading ridges.Tan, Yen Joe, et al.\r\n
<\/pre>\nMore in-sentence examples of “magma”:<\/h2>\n
- When large tectonic plates collided about 100 million years, magma<\/strong> escaped between these plates and solidified between other rocks.\r\n
- These planes or weakened areas allow the intrusion of a thin sheet-like body of magma<\/strong> paralleling the existing strata.\r\n
<\/pre>\n