How to use in-sentence of “magma”:
– Also, lunar samples do not have expected ratios of volatile elements, iron oxide, or siderophilic elements, and there is no evidence that the Earth ever had the magma ocean implied by the hypothesis.
– The magma forming this lava is often felsic, with high-to-intermediate levels of silica, and less mafic magma.
– The Snake River Plain was formed by magma rising up below the North American Plate.
– The rocks are Intrusiveplutonic, formed when molten magma is trapped under the Earth’s surface and cools into a crystalline mass.
– Melted material from the mantle and crust moves up through the crust and collects in magma chambers.
– Aqua and Magma agents and the leaders, Archie, leader of Aqua, and Maxie, leader of Magma, play a part in Pokémon R/S/E.
– During certain types of gigantic eruptions, the volcano’s magma chamber may empty enough for an area above it to subside.
Example sentences of “magma”:
– In a volcanic eruption, Magma is blown apart by volcanic gases and steam.
– From these magma erupts as gases, lava, and ejecta.
– The motivating force for seafloor spreading ridges is tectonic plate pull rather than magma pressure, although there is typically significant magma activity at spreading ridges.Tan, Yen Joe, et al.
– He played in the progressive rock/jazz fusion band Magma in the 1970s.
– New magma of basalt composition emerges at and near the axis because of decompression melting in the underlying Earth’s mantle.
– Immediately after the impact, the Earth’s mantle was vigorously convectionconvecting, the surface was a large magma ocean.
– As the rock slowly cools into a solid, the different parts of the magma Crystallizationcrystallize into minerals.
– Feldspar forms crystals from magma 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.
– When magma comes out from the ground in a volcano it is called lava.
– The crystallized magma forms new crust of basalt and gabbro.
- In a volcanic eruption, Magma is blown apart by volcanic gases and steam.
- From these magma erupts as gases, lava, and ejecta.
- The motivating force for seafloor spreading ridges is tectonic plate pull rather than magma pressure, although there is typically significant magma activity at spreading ridges.Tan, Yen Joe, et al.
– Felsic magma is thick and has silica minerals.
– These particles are small, slaggy pieces of magma and rock that have been tossed into the air by outbursts of steam and other gases.
– The giant Norilsk nickel-copper-palladium deposit formed within the magma flows in the main Siberian Traps.
– The name of the magma would be “The integers under multiplication”.
– Changes in stress caused by large earthquakes may be enough to cause volcanovolcanic eruptions, when the magma system of the volcano is close to a critical state.
– The changes that occur are greatest where the magma comes into contact with the rock.
– It has its own magma plumbing under the Earth that goes down under the Earths crust by 60 km.
– Sometimes, the magma comes out quickly and sometimes it comes slowly.
More in-sentence examples of “magma”:
– When large tectonic plates collided about 100 million years, magma escaped between these plates and solidified between other rocks.
– These planes or weakened areas allow the intrusion of a thin sheet-like body of magma paralleling the existing strata.
– Then magma enters these lines of weakness.
– The magma does not have to reach the surface in order to create a mountain: magma that solidifies below ground can still form dome mountains, such as Navajo Mountain in the states of Utah and Arizona, in the United States.
– New magma emerges onto the ocean floor near the ridge axis.
– Sometimes the amount of magma erupted is so large that the top of the volcano collapses.
– The great earthquake in 1707 may have changed pressure in the magma under Mount Fuji.
– Then we give the magma the label.
– Sills are fed by dykes as they form from a lower magma source.
– Such melting can take place near a hotspot, resulting in a mixture of magma from the depths of the hotspot with superficial magma produced by a mantle plume.
– However, magma was found under the ground three times in geothermal drilling projects twice in Iceland and once in Hawaii.
– This sudden uplift was likely caused by rising magma of the Mackenzie plume, which caused the Mackenzie hotspot.
– Other volcanic mountains form over hot spots, pockets of magma beneath the crust which erupt onto Earth’s surface.
– The study of magma is usually done in lava flows.
– The cause of these earthquakes is believed to be the rising of molten magma because there are no faults or tectonic plate boundaries.
– The existing rocks must split to create the planes along which the magma moves in.
– At these ridges, hot magma rises into the crust and cools, pushing the crust apart at the ridge.
– The teams Aqua and Magma did not play a part in the anime very much.
– The magma is forced between other layers of rock by the pressure under the Earth’s surface.
– Large bodies of magma that solidify underground before they reach the surface of the crust are called plutons.
– Team Aqua and Team Magma are the two feuding crime syndicates in the Hoenn region and in the games “Pokémon Ruby, Sapphire, and Emerald” as well as their remakes “Omega Ruby” and “Alpha Sapphire”.
– Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers.
– As it forms, a plug may cause an extreme build-up of pressure if gas-charged magma is trapped beneath it.
– In such an eruption the volcano’s magma chamber is empty enough for the ground above it to drop.
– Mid-ocean ridges are geologically active, with new magma constantly emerging onto the ocean floor and into the crust at and near rifts along the ridge axes.
– Xenoliths may be covered in the margins of a magma chamber, torn loose from the walls of a flow of lava or picked up along the ground by flowing lava on Earth’s surface.
- When large tectonic plates collided about 100 million years, magma escaped between these plates and solidified between other rocks.
- These planes or weakened areas allow the intrusion of a thin sheet-like body of magma paralleling the existing strata.
– 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 ejected.
– Many types of minerals are made when molten rock, or magma cools and turns into a solid.
– These felsic protocontinents probably formed at hot spots rather than subduction zones, from a variety of sources: mafic magma melting more felsic rocks, partial melting of mafic rock, and from the metamorphic alteration of felsic sedimentary rocks.
– Subaerial-submarine evidence of structures feeding magma to Stromboli Volcano, Italy, and relations with edifice flank failure and creep.
– Officials said hundreds of volcanic earthquakes had been recorded on the mountain over the weekend of 23–24 October, and that the magma had risen to about 1 kilometre below the surface due to the seismic activity.
– Several new features were seen, such as the “whaleback” which is solid magma being pushed to the top of the volcano by magma under it.
– Some magma may even reach the Earth’s surface as lava.
– Igneous rocks are formed when molten magma cools, either above or below the surface.
– The molten magma under great pressure forces its way through the fissure of underground rocks and reaches the Earth’s surface to form “igneous extrusion”.
– An intrusion is magma which cools and becomes solid under the Earth’s surface.
– Lava or magma can cause weathering when molten rock touches older rock.
– As the magma cools, these minerals form crystals.
– They formed about 300,000 years ago when magma from the Geomonoreum parasitic volcano cooled.
– It happens most in igneous rock when magma is fluid enough to flow round more solid rock.
– The Watchung basalt flows of the Watchung Mountains are eruptions onto the surface of the same magma that created the Palisades Sill.Kodama K.P., 1983.
– The eruption emptied the magma chamber under the area to the point of collapse.
– Volcanoes are places where magma reaches the earth’s surface.
– This newly formed magma rises toward the Earth’s surface to erupt, forming a chain of volcanoes.Public domain material from the United States Geological Survey document: “Pacific – Cascades Volcanic Province”.
– Volcanism is the Volcanic eruptioneruption of magma onto the surface of the Earth.
– Intrusive rocks are made when the magma slowly cools to form rocks under the surface.
– As the plate moved westward, the magma melted rock under the plate.
– Contact metamorphism occurs when magma is injected into the surrounding solid rock.
– At the rift, the boundary between tectonic plates, magma from the mantle reaches the seafloor.