Magma in a sentence

(1) Granite is formed from cooled magma.

(2) The brimstony magma bubbled and boiled.

(3) The igneous rock was formed from magma.

(4) Magma can be a source of geothermal energy.

(5) Igneous rocks are formed from molten magma.

(6) Felsic magma is rich in silica and aluminum.

(7) The bathylith is a result of magma intrusion.

(8) The laccolith is composed of solidified magma.

(9) Dacites form from the solidification of magma.

(10) The magma cooled and turned into igneous rock.

Magma sentence

(11) The movement of magma is an endogenic process.

(12) The movement of magma is a result of diapirism.

(13) The crystalisation of magma forms igneous rocks.

(14) Olivines are formed during the cooling of magma.

(15) The mineral exsolved from the magma as it cooled.

(16) The volcano had a magma chamber deep underground.

(17) Igneous rock is formed from molten magma or lava.

(18) Andesytes are formed from magma that cools slowly.

(19) The mafic magma erupted violently from the volcano.

(20) Felsic magma tends to form intrusive igneous rocks.

Magma make sentence

(21) Aplite is formed from the crystallization of magma.

(22) Aphanites are formed from magma that cools quickly.

(23) The magma advects heat towards the Earth's surface.

(24) Igneous rocks are formed from molten lava or magma.

(25) Igneous rocks are formed from molten magma or lava.

(26) Magma can be composed of various minerals and gases.

(27) The asthenospheric zone is where magma is generated.

(28) The trachytic rock was formed from solidified magma.

(29) The volcanic eruption caused magma to exsolve gases.

(30) Dacites are formed from the solidification of magma.

Sentence of magma

(31) Rhyolitic magma is known for its high silica content.

(32) Basaltes are formed from the solidification of magma.

(33) The diapiric ascent of magma can trigger earthquakes.

(34) Felsic magma is viscous and tends to trap gas bubbles.

(35) Diapirs can be formed by the upward movement of magma.

(36) The igneous rock was formed from the cooling of magma.

(37) The liquification of magma leads to volcanic eruptions.

(38) The solidification of the magma formed a volcanic rock.

(39) Felsic magma can generate explosive volcanic eruptions.

(40) The augitic crystals in the rock are formed from magma.

Magma meaningful sentence

(41) The magma chamber originates beneath the Earth's crust.

(42) The dioritic rock was formed from the cooling of magma.

(43) The geothermal plant utilized heat from basaltic magma.

(44) The batholithic formation was a result of magma cooling.

(45) The magma exsolved gases that caused volcanic eruptions.

(46) The devitrified granite was once a molten magma chamber.

(47) The cooling magma solidified into a solid rock formation.

(48) The viscosity of magma determines how easily it can flow.

(49) The andesitic magma contains a high percentage of silica.

(50) The trachytoid rock was formed from the cooling of magma.

Magma sentence examples

(51) The diapiric rise of magma can trigger volcanic eruptions.

(52) The magma mulls beneath the volcano, threatening to erupt.

(53) The peraluminous magma was highly viscous and slow-moving.

(54) The tholeiitic series is one of the two main magma series.

(55) The cooling magma will eventually crystallize into granite.

(56) The formation of pegmatites requires slow cooling of magma.

(57) Underplating can result in the formation of magma chambers.

(58) The xenoliths were formed from the solidification of magma.

(59) The calcalkaline magma is rich in silica and alkali metals.

(60) Aplitic rocks are formed from the crystallization of magma.

Sentence with magma

(61) Dacitic magma is typically more viscous than basaltic magma.

(62) The hypabyssal magma slowly cooled and solidified over time.

(63) The crystals accrete subsequent to the cooling of the magma.

(64) The diapiric ascent of magma can trigger volcanic eruptions.

(65) The core of a volcano is where the magma chamber is located.

(66) The eruption of a volcano releases magma into the atmosphere.

(67) The cooling and solidification of magma forms volcanic rocks.

(68) The movement of magma can create volcanic vents and fissures.

(69) The recalescent magma bubbled and churned inside the volcano.

(70) The extrusive rock was formed from magma that cooled quickly.

Use magma in a sentence

(71) Norite is formed when magma cools and solidifies underground.

(72) The felsic magma is responsible for the formation of granite.

(73) Felsites are formed from the solidification of magma or lava.

(74) The igneous rock was formed from the solidification of magma.

(75) The process of melting rocks to form magma is called melting.

(76) Magma can be forced to the surface through volcanic eruptions.

(77) Andesitic magma is typically more viscous than basaltic magma.

(78) The peralkaline magma is typically formed in subduction zones.

(79) Phonolites can be formed through the crystallization of magma.

(80) The asthenospheric region is where magma chambers are located.

Sentence using magma

(81) The silicic magma is responsible for the formation of granite.

(82) The heat from magma can cause nearby rocks to melt and change.

(83) The asthenosphere is a source of magma for volcanic eruptions.

(84) The movement of magma within the Earth is an endogenic process.

(85) The movement of magma within a volcano is an endogenic process.

(86) The intense pressure caused the rock to liquify and form magma.

(87) Aphanitic textures can be formed by the rapid cooling of magma.

(88) Nephelinite is formed from magma that is low in silica content.

(89) Dacitic magma is typically formed in subduction zone volcanoes.

(90) The viscosity of dacitic magma can lead to explosive eruptions.

Magma example sentence

(91) The subducting plate will cause the formation of magma beneath.

(92) The hot magma cools and recrystallizes into solid igneous rock.

(93) The Vesuvian magma chamber is estimated to be around 8 km deep.

(94) The temperature of magma can reach up to 1,200 degrees Celsius.

(95) The viscosity of magma can be influenced by its silica content.

(96) Magma chambers are underground reservoirs where magma is stored.

(97) The study of magma is an important field of research in geology.

(98) The degassing of volcanic magma can lead to explosive eruptions.

(99) The formation of syenites involves the crystallization of magma.

(100) The rhyolitic magma chamber is located deep beneath the surface.

Sentence with word magma

(101) Basanites is formed when magma cools and solidifies underground.

(102) The rocks near the magma chamber underwent contact metamorphism.

(103) The mafic magma is known for its high density and low viscosity.

(104) The tholeiitic magma series is associated with subduction zones.

(105) Igneous rock is formed from lava or magma, which is melted rock.

(106) Magma is a molten rock that is found beneath the Earth's surface.

(107) The temperature and pressure of magma can influence its behavior.

(108) Felsic magma tends to have a higher gas content than mafic magma.

(109) The peralkaline magma is characterized by its low silica content.

(110) The microseism was a result of the movement of underground magma.

Sentence of magma

(111) The calcalkaline magma can form different types of igneous rocks.

(112) The bathylitic rocks are formed from the solidification of magma.

(113) The monzonitic magma chamber beneath the surface is still active.

(114) Asthenospheres are important for the formation of magma chambers.

(115) The study of magma and volcanic activity is known as volcanology.

(116) The study of magma can help predict and mitigate volcanic hazards.

(117) Felsic magma tends to form at lower temperatures than mafic magma.

(118) The volcanic rocks are formed through the solidification of magma.

(119) The eruptives magma chamber beneath the volcano was highly active.

(120) Baddeleyite is formed through the crystallization of molten magma.

Magma used in a sentence

(121) The cooling magma crystallises into various minerals and crystals.

(122) The amygdaloids in the rock were a result of the cooling of magma.

(123) The process of cooling and solidifying magma creates igneous rock.

(124) Igneous rocks are formed from the solidification of magma or lava.

(125) The cooling rate of magma can affect the texture of igneous rocks.

(126) The viscosity of magma can affect how it behaves during eruptions.

(127) The study of how magma interacts with rocks is known as petrology.

(128) The aplitic dike provided a pathway for magma to reach the surface.

(129) The asthenosphere is a layer that allows for the movement of magma.

(130) The cooling magma crystallizes into various types of igneous rocks.

Magma sentence in English

(131) The peralkaline magma is often associated with alkaline intrusions.

(132) Convections are responsible for the movement of magma in a volcano.

(133) The scoriaceous rocks were formed from the solidification of magma.

(134) The upper mantle is a major source of magma for volcanic eruptions.

(135) Tephrite is commonly found in volcanic regions with alkaline magma.

(136) The liquidus of the magma determines the type of volcanic eruption.

(137) The rock was infusible and had formed from solidification of magma.

(138) Andesite is formed from the solidification of magma and lava flows.

(139) The formation of olivine is influenced by the cooling rate of magma.

(140) Geysers are formed when water gets heated by magma deep underground.

(141) The pressure from rising magma can cause the Earth's crust to crack.

(142) Magma can be a source of valuable resources such as gold and copper.

(143) The composition of magma can change as it rises towards the surface.

(144) The amygdaloidal basalt was formed from the solidification of magma.

(145) The formation of thorites is closely linked to the cooling of magma.

(146) Volcanologists study volcanic deformation to monitor magma movement.

(147) Lamprophyre is formed by the intrusion of magma into existing rocks.

(148) The viscosity of dacitic magma is higher compared to basaltic magma.

(149) The magma had started to calcify beneath the surface of the volcano.

(150) The magma had started to calcify towards the surface of the volcano.

(151) The convections in the magma chamber can lead to volcanic eruptions.

(152) The presence of microlites can indicate the cooling rate of a magma.

(153) The proximate cause of the volcanic eruption was the magma pressure.

(154) The crystallization of magma leads to the formation of igneous rocks.

(155) The porphyritic andesite was formed from the solidification of magma.

(156) The peralkaline magma is known for its high temperature and fluidity.

(157) The formation of felsites is closely related to the cooling of magma.

(158) Trachyte is formed when magma cools rapidly near the Earth's surface.

(159) Volcanology involves studying the behavior of magma within volcanoes.

(160) The volcanic activity upwells magma from beneath the Earth's surface.

(161) Hornblendic minerals can be used to identify the rock's parent magma.

(162) The cooling magma crystallises into different types of igneous rocks.

(163) The calcalkaline magma can also produce explosive volcanic eruptions.

(164) The felsic magma chamber is located deep beneath the Earth's surface.

(165) The temperature of magma can be measured using specialized equipment.

(166) The nucleation of gas bubbles in magma can trigger volcanic eruptions.

(167) The growth of spherulites is influenced by the viscosity of the magma.

(168) The movement of magma beneath the Earth's crust can cause earthquakes.

(169) Magma can remain underground for long periods of time before erupting.

(170) The movement of magma can create volcanic islands and mountain ranges.

(171) Magma can be a source of volcanic ash and other pyroclastic materials.

(172) The formation of feldspars is influenced by the cooling rate of magma.

(173) Porphyrites is formed through the cooling and solidification of magma.

(174) Rhyolitic rocks are formed from the solidification of rhyolitic magma.

(175) Dioritic textures can vary depending on the cooling rate of the magma.

(176) The high pressure caused the rock to liquate and transform into magma.

(177) The Mid-Atlantic Ridge is a boundary where magma rises to the surface.

(178) The heat from magma can create hot springs and geysers at the surface.

(179) The composition of spherulites can vary depending on the type of magma.

(180) The movement of magma through the Earth's crust is a form of diapirism.

(181) The heat from magma can cause rocks to melt and form new igneous rocks.

(182) The study of magma can provide insights into the formation of minerals.

(183) The formation of syenite is often associated with the cooling of magma.

(184) Cairngorm is formed through the slow cooling of magma deep underground.

(185) The exsolution process can occur during the cooling of a magma chamber.

(186) The batholitic formation was a result of magma cooling and solidifying.

(187) The diabasic rock was formed from magma that cooled slowly underground.

(188) The dacitic magma chamber was located deep beneath the earth's surface.

(189) The formation of anorthosite is closely related to the cooling of magma.

(190) The formation of spherulites is influenced by the cooling rate of magma.

(191) The intrusion of magma to form intrusives can generate seismic activity.

(192) The presence of lamprophyre indicates the presence of deep-seated magma.

(193) Tinguaites are formed when magma rises to the surface and cools rapidly.

(194) When komatiite melts, it can form magma that is extremely hot and fluid.

(195) The felspar in this volcanic ash is evidence of the magma's composition.

(196) The tholeiitic magma composition is characterized by low silica content.

(197) The diapiric movement of magma can cause significant geological changes.

(198) The intense pressure caused the rock to liquify and form a magma chamber.

(199) Plagioclase can be used to identify the type of magma that formed a rock.

(200) Phenocrysts can be used to identify the type of magma that formed a rock.

(201) The intense pressure caused the rock to liquefy and form a magma chamber.

(202) Magma can contain dissolved gases such as water vapor and carbon dioxide.

(203) The formation of leucite is associated with the crystallization of magma.

(204) The diapiric rise of magma can result in the formation of volcanic plugs.

(205) The formation of trachytes is influenced by the composition of the magma.

(206) The formation of plutonic rocks occurs through the slow cooling of magma.

(207) The convecting magma beneath the Earth's crust causes volcanic eruptions.

(208) Tephrite is formed when magma with low silica content solidifies quickly.

(209) The rheology of magma is studied to better understand volcanic eruptions.

(210) The subducting plate is melting and causing magma to rise to the surface.

(211) Igneous rocks are formed from the solidification of molten magma or lava.

(212) The aplitic texture of the rock is a result of the slow cooling of magma.

(213) Vulcanism is the process of magma and lava rising to the Earth's surface.

(214) The volcanologist studied the downwellings of magma in the earth's crust.

(215) The viscosity of magma can affect the explosiveness of volcanic eruptions.

(216) Porphyries are formed when magma cools slowly beneath the Earth's surface.

(217) Dacitic eruptions can be explosive due to the high viscosity of the magma.

(218) The presence of felsites indicates the past presence of magma in the area.

(219) The formation of maars involves the interaction of magma with groundwater.

(220) The formation of tridymite is influenced by the cooling rate of the magma.

(221) The cooling magma crystallizes, creating different types of igneous rocks.

(222) The movement of magma through the Earth's mantle is a result of diapirism.

(223) Magma can also be referred to as lava once it reaches the Earth's surface.

(224) The calcalkaline magma can also form intrusive igneous rocks like granite.

(225) The calcalkaline magma can also produce lava flows that cover large areas.

(226) The peralkaline magma chamber is located deep beneath the Earth's surface.

(227) The convection of magma beneath the Earth's crust causes volcanic activity.

(228) The formation of supracrustal rocks is influenced by the presence of magma.

(229) The pyroclastics can be analyzed to determine the composition of the magma.

(230) The diapiric ascent of magma can result in the formation of volcanic necks.

(231) The formation of bathyliths is often associated with the movement of magma.

(232) The cooling of magma causes minerals to crystallize and form igneous rocks.

(233) The hypabyssal rocks were formed from the solidification of magma chambers.

(234) The movement of magma through the Earth's crust is an example of diapirism.

(235) Granite is formed from magma that cools slowly beneath the Earth's surface.

(236) Magma can be studied to better understand the Earth's geological processes.

(237) Magma can cause landslides when it interacts with unstable rock formations.

(238) The viscosity of magma can determine the likelihood of explosive eruptions.

(239) The tholeiitic magma series is named after the Tholey Mountains in Germany.

(240) The diapiric intrusion of magma can lead to the formation of igneous rocks.

(241) The graben is a result of the movement of magma beneath the Earth's surface.

(242) The formation of andesites involves the cooling and solidification of magma.

(243) The composition of bathyliths can vary depending on the source of the magma.

(244) The presence of magma deep within the volcano suggests that it is eruptible.

(245) The fumarolic activity is a result of the magma chamber beneath the volcano.

(246) The nucleation of bubbles in magma can lead to explosive volcanic eruptions.

(247) The volcanic eruption was defused by injecting water into the magma chamber.

(248) Seismic activity can be caused by the movement of magma beneath the surface.

(249) Igneous rock is formed from the cooling and solidification of magma or lava.

(250) The geologist envisages underneath the earth's crust a molten core of magma.

(251) The andesitic magma chamber beneath the volcano is slowly building pressure.

(252) Vulcanology involves studying the physical and chemical properties of magma.

(253) The maars are formed when magma interacts with groundwater or surface water.

(254) The basaltic rock was formed through the cooling and solidification of magma.

(255) Magma can provide clues about the history and evolution of the Earth's crust.

(256) The peralkaline nature of the magma determines the type of volcanic eruption.

(257) The inchoative moment of a volcano eruption is when the magma starts to rise.

(258) The ophitic texture is formed during the cooling and solidification of magma.

(259) The movement of magmas beneath the Earth's surface can create magma chambers.

(260) The diapiric movement of magma can result in the formation of volcanic vents.

(261) Lamprophyre is formed through the interaction of magma and surrounding rocks.

(262) The heat will channel up from the magma chamber, causing geothermal activity.

(263) The rhyolitic magma cooled and solidified into a beautiful crystal formation.

(264) The cooling rate of magma determines the type of igneous rock that is formed.

(265) The temperature at which magma cools can affect the texture of igneous rocks.

(266) The process of cooling magma to form igneous rocks is called crystallization.

(267) The devitrified magma had cooled and solidified into a crystalline structure.

(268) The upwellings of magma from the Earth's mantle can cause volcanic eruptions.

(269) The botryoidal formation in the rock was caused by the slow cooling of magma.

(270) Phenocrysts can help geologists determine the cooling rate of a magma chamber.

(271) Magma can create unique geological formations such as lava tubes and calderas.

(272) The xenolith's discovery shed light on the processes of magma crystallization.

(273) Geologists study aplites to understand the processes of magma crystallization.

(274) The presence of syenite indicates the presence of a deep-seated magma chamber.

(275) The trachytoid texture is a result of the cooling and solidification of magma.

(276) The laccolith formed when magma pushed its way into the overlying rock layers.

(277) The lamprophyre magma that formed this rock likely originated from the mantle.

(278) The magma will channel up from the earth's mantle, causing volcanic eruptions.

(279) The calcalkaline magma can also contain metals and minerals of economic value.

(280) Igneous rocks are formed from the cooling and solidification of magma or lava.

(281) Volcanic eruptions often involve the release of magma from the Earth's mantle.

(282) Magma can be used to create obsidian and pumice, both types of volcanic glass.

(283) Magma can be monitored using both ground-based and satellite-based techniques.

(284) The upward movement of magma can result in volcanic eruptions due to diapirism.

(285) The study of magma helps scientists understand the inner workings of the Earth.

(286) Microlites are often used as indicators of magma mixing and mingling processes.

(287) The diapiric ascent of magma can result in the formation of igneous intrusions.

(288) Tachylytes can provide clues about the depth and temperature of magma chambers.

(289) The volcanic eruption was defused by releasing pressure from the magma chamber.

(290) The process of plutonism involves the slow cooling and solidification of magma.

(291) Plutonism is closely linked to the movement of magma within the Earth's mantle.

(292) Magma can contain varying amounts of gases like carbon dioxide and water vapor.

(293) Augite is often used as a geothermometer to determine the temperature of magma.

(294) The petrological examination of the granite showed evidence of magma intrusion.

(295) Porphyries are formed from magma that cools slowly beneath the Earth's surface.

(296) Magma can form intrusive igneous rocks when it cools slowly beneath the surface.

(297) Ophite is formed from the solidification of magma deep within the Earth's crust.

(298) The diatreme is a result of the rapid ascent of magma through the Earth's crust.

(299) The heat from the magma caused the surrounding rocks to turn into igneous rocks.

(300) The composition of magma can vary depending on the location and type of volcano.

(301) The authigenic feldspar in the granite was formed by crystallization from magma.

(302) The petrogenesis of igneous rocks is influenced by the composition of the magma.

(303) Xenocrysts can be used to trace the movement of magma through the Earth's crust.

(304) The formation of pegmatites is influenced by the composition of the parent magma.

(305) The porphyritic texture of the rock suggested a complex history of magma cooling.

(306) The formation of porphyroids involves the intrusion of magma into existing rocks.

(307) The pressure-gradient in the volcano's magma chamber leads to volcanic eruptions.

(308) The albitic composition of this rock suggests it originated from a magma chamber.

(309) Magmatism can lead to the creation of magma chambers beneath the Earth's surface.

(310) The process of underplating involves the intrusion of magma into the lower crust.

(311) The formation of dacitic magma involves the partial melting of the Earth's crust.

(312) The ferromagnesian content of this mineral is indicative of a mafic magma source.

(313) The convective flow of magma beneath the Earth's crust causes volcanic eruptions.

(314) The composition of eucrite suggests that it was formed from the cooling of magma.

(315) The gabbroic layer beneath the earth's crust is believed to be a source of magma.

(316) Granites are formed from the slow cooling of magma deep within the Earth's crust.

(317) The hypabyssal magma cooled slowly, resulting in the formation of large crystals.

(318) Intrusive igneous rock forms when magma cools slowly beneath the Earth's surface.

(319) Intrusive igneous rocks form when magma cools slowly beneath the Earth's surface.

(320) Magma can be used in geothermal power generation as a source of renewable energy.

(321) Magma chambers are large bodies of molten rock found beneath the Earth's surface.

(322) Magma can carry minerals that are important for industrial and economic purposes.

(323) The study of magma and volcanic systems can help prevent future volcanic hazards.

(324) Crystallizing in the heat of the volcano, the magma solidified into igneous rock.

(325) Andesitic magma can form intrusive igneous rocks such as diorite and granodiorite.

(326) The silica-rich magma can silicify the surrounding rocks during volcanic activity.

(327) Batholiths are formed when magma cools and solidifies beneath the Earth's surface.

(328) The diapiric movement of magma can cause significant changes in the Earth's crust.

(329) The bathylith's formation can create magma chambers deep within the Earth's crust.

(330) The allanitic composition of this rock suggests a complex history of magma mixing.

(331) Underthrusting can cause the melting of rocks and the formation of magma chambers.

(332) The felsitic composition of this rock suggests it originated from a magma chamber.

(333) The presence of phlogopite in a rock can indicate its origin from a magma chamber.

(334) The movement of magma beneath the Earth's surface contributes to crustal movement.

(335) The trachytes in this area were formed through a process of magma crystallization.

(336) The lamprophyre magma that formed this rock likely originated from a mantle plume.

(337) Andesites are formed from the solidification of magma beneath the Earth's surface.

(338) The dacitic magma chamber was responsible for the volcanic activity in the region.

(339) Granite is formed from the slow cooling of magma deep beneath the Earth's surface.

(340) When magma cools slowly beneath the Earth's surface, it can create large crystals.

(341) Rifting is often associated with the movement of magma beneath the Earth's surface.

(342) The greisen alteration is commonly associated with the intrusion of granitic magma.

(343) The presence of orthoclase in a rock can indicate its origin from a granitic magma.

(344) The bathylite's formation process involved the cooling and solidification of magma.

(345) The abundance of xenocrysts in this sample indicates a high degree of magma mixing.

(346) The phreatic activity is a result of the interaction between magma and groundwater.

(347) Lamprophyre is formed when magma intrudes into the Earth's crust and cools rapidly.

(348) Intraplate earthquakes can be triggered by the movement of magma beneath the crust.

(349) The calcalkaline magma can interact with groundwater and create geothermal systems.

(350) The formation of a laccolith is a result of magma intrusion into the earth's crust.

(351) The unique shape of the laccolith is a result of the pressure exerted by the magma.

(352) The amygdaloidal rocks were formed from magma that had interacted with groundwater.

(353) The subjacent layer of magma was responsible for the volcanic activity in the area.

(354) The formation of augites is associated with the cooling and solidification of magma.

(355) The formation of ferromagnesian minerals is influenced by the cooling rate of magma.

(356) The composition of magma can vary depending on the location and geological activity.

(357) Andesitic magma can interact with water to produce explosive steam-driven eruptions.

(358) The gabbroic composition of this rock suggests that it formed from a basaltic magma.

(359) The formation of tholeiite is influenced by the cooling and solidification of magma.

(360) The mineral assemblage of tholeiite can provide clues about the source of the magma.

(361) The batholith's formation can result in the formation of deep-seated magma chambers.

(362) The formation of anorthosites is often associated with the crystallization of magma.

(363) Dacites can exhibit flow banding due to the movement of magma during solidification.

(364) The cooling of the magma caused minerals to precipitate over time, forming crystals.

(365) The size and shape of microlites can vary depending on the composition of the magma.

(366) Microlites can also be used to track the movement of magma within a volcanic system.

(367) Dacite is formed from the solidification of magma or lava that has a high viscosity.

(368) The hollow below the surface of the volcano was where the magma chamber was located.

(369) The convective motion of magma beneath the Earth's crust leads to volcanic eruptions.

(370) The volcanic activity in the area causes hot magma to upwell from the Earth's mantle.

(371) Understanding the hydrodynamical behavior of magma is important in volcanic research.

(372) The rocks underwent contact metamorphism due to their proximity to the magma chamber.

(373) Intraplate earthquakes can be triggered by the movement of magma beneath the surface.

(374) Lamprophyre is formed from the solidification of magma deep within the Earth's crust.

(375) The cooling and solidification of magma is a key process in the formation of plutons.

(376) Underplating can lead to the formation of magma chambers beneath the Earth's surface.

(377) Lapadite, which was often found in volcanic rock, was formed by the cooling of magma.

(378) The phreatomagmatic activity was a result of the interaction between magma and water.

(379) Tholeiitic rocks are formed from magma that has undergone fractional crystallization.

(380) Igneous rocks are formed from cooled magma, and they can be found all over the world.

(381) The formation of anorthosite is thought to be related to the crystallization of magma.

(382) The cooling and solidification of magma underground leads to the formation of plutons.

(383) The pressure inside the volcano's magma chamber is building up and may erupt off soon.

(384) The presence of microcline in a rock can indicate its association with granitic magma.

(385) The formation of feldspathoids is influenced by the chemical composition of the magma.

(386) The study of amygdules can help geologists understand the evolution of magma chambers.

(387) The hornblendic rock formation is a result of the cooling and solidification of magma.

(388) Scientists use geodynamics to study the movement of magma beneath the Earth's surface.

(389) The formation of phonolites is closely linked to the process of magma differentiation.

(390) The convections in the magma beneath the Earth's surface can cause volcanic eruptions.

(391) The vulcanological study of the region revealed the presence of active magma chambers.

(392) The ultrabasic magma that formed this rock cooled slowly, resulting in large crystals.

(393) The asthenosphere is a zone of the Earth's mantle, and it is where magma is generated.

(394) The laminar flow of magma in a volcano can be disrupted by the presence of gas bubbles.

(395) The peraluminous composition of the rock suggests a complex history of magma evolution.

(396) The mineralogy of syenites can vary depending on the specific composition of the magma.

(397) The formation of aplites is closely related to the cooling and solidification of magma.

(398) The formation of cristobalite can occur during the cooling and solidification of magma.

(399) Amygdules can be used to determine the composition of the magma from which they formed.

(400) The ignimbrites in this region are a result of the interaction between magma and water.

(401) The study of laccoliths can help scientists understand the dynamics of magma intrusion.

(402) The abundance of xenocrysts in this sample suggests a prolonged period of magma mixing.

(403) The upward movement of magma through the Earth's crust is a manifestation of diapirism.

(404) The rheologic properties of the magma were studied to understand the volcanic eruption.

(405) The lopolith intrusion is believed to have been caused by magma rising from the mantle.

(406) The formation of igneous rocks can be influenced by the presence of gases in the magma.

(407) The xenolith's presence in the rock formation indicated the presence of a magma chamber.

(408) The movement of magma beneath the Earth's surface is closely linked to crustal movement.

(409) The study of aplites helps geologists understand the processes of magma differentiation.

(410) The formation of gabbro can take millions of years as magma slowly cools and solidifies.

(411) Plutonism provides a framework for understanding the movement of magma within the Earth.

(412) Tholeiite is formed through the crystallization of magma at relatively low temperatures.

(413) The formation of elaeolite is closely linked to the cooling and solidification of magma.

(414) The cooling of hot magma in the Earth's mantle causes it to crystallize into solid rock.

(415) The movement of magma beneath the Earth's surface is often associated with diastrophism.

(416) The movement of magma during diastrophism can lead to the formation of volcanic islands.

(417) The vulcanological study identified the presence of a magma chamber beneath the volcano.

(418) The pluton's formation likely involved the intrusion of magma into existing rock layers.

(419) The pluton's size indicates a significant amount of magma was involved in its formation.

(420) Bowen's reaction series is a sequence of minerals that form during the cooling of magma.

(421) The dioritic rock was formed from the cooling of magma deep beneath the earth's surface.

(422) The seismic disturbance was caused by the movement of magma beneath the Earth's surface.

(423) Seismic disturbances can be caused by the movement of magma beneath the Earth's surface.

(424) Magma can release toxic gases like sulfur dioxide and hydrogen sulfide during eruptions.

(425) The formation of plutons can take millions of years as magma slowly cools and solidifies.

(426) The formation of melilite is influenced by the presence of certain elements in the magma.

(427) The cooling of magma deep within the Earth's crust allows it to crystallize into granite.

(428) The presence of xenocrysts in this rock suggests a complex history of magma interactions.

(429) Diapirism can cause the formation of salt domes, or it can lead to the movement of magma.

(430) The cooling of the magma caused minerals to precipitate during the formation of the rock.

(431) Phonolites are formed from magma that has undergone partial melting of the Earth's crust.

(432) Intrusive igneous rocks form when magma cools and solidifies beneath the Earth's surface.

(433) The xenolith's presence in the rock formation suggested a complex history of magma mixing.

(434) The presence of tephrite in a volcanic rock can indicate a more evolved magma composition.

(435) The effects of contact metamorphism can be seen in the altered rocks near a magma chamber.

(436) The pluton's composition suggests it may have originated from a deep-seated magma chamber.

(437) The formation of gabbros involves the slow cooling of magma deep within the Earth's crust.

(438) The intense pressure and heat in the Earth's mantle lapidify molten rock into solid magma.

(439) The formation of dacites is often associated with the interaction between magma and water.

(440) The formation of plutons can take millions of years, as magma slowly cools and solidifies.

(441) The rhyolitic rock was formed from the solidification of magma with a high silica content.

(442) The formation of the lopolith was caused by the intrusion of magma into the earth's crust.

(443) The geomorphological features of volcanic landscapes are a result of magma and lava flows.

(444) Laccoliths are igneous intrusions that form when magma is injected into the earth's crust.

(445) The formation of anorthosite can be attributed to the cooling and solidification of magma.

(446) Bornite is a primary mineral, meaning it forms directly from magma or hydrothermal fluids.

(447) The subducting process can result in the formation of magma chambers and volcanic activity.

(448) The ophitic texture is a result of the slow cooling of magma deep within the Earth's crust.

(449) The formation of a batholite involves the intrusion of magma into existing rock formations.

(450) The composition of plutonic rocks can vary greatly depending on the type of magma involved.

(451) The monzonitic texture is often associated with the cooling of magma at intermediate rates.

(452) The pressure heaved up between the magma and the earth's crust, causing volcanic eruptions.

(453) The perlitic texture of the igneous rock suggested that it had formed from a magma chamber.

(454) The diatreme is a geological feature that is formed by a violent eruption of gas and magma.

(455) The formation of granitoids is often associated with tectonic activity and magma intrusion.

(456) The formation of hornblendes is closely related to the cooling and solidification of magma.

(457) Magnetic anomalies can be used to detect the presence of magma beneath the Earth's surface.

(458) The formation of intrusives often involves the intrusion of magma into existing rock layers.

(459) The formation of dolerites is often associated with the cooling and solidification of magma.

(460) The formation of aplites is often associated with the final stages of magma crystallization.

(461) The presence of pyroxenes in a rock can indicate the type of magma from which it was formed.

(462) Gabbro is formed from the cooling and solidification of magma deep within the Earth's crust.

(463) The formation of anorthosites is closely related to the cooling and solidification of magma.

(464) The xenocrysts in this rock are thought to have originated from a deep-seated magma chamber.

(465) Metasomatism can be caused by a variety of fluids, including water, magma, and hydrocarbons.

(466) The phreatomagmatic event was caused by the sudden release of pressure in the magma chamber.

(467) The diatreme is a type of volcanic vent that is formed by a sudden release of gas and magma.

(468) The growth of spherulites is influenced by the availability of certain minerals in the magma.

(469) The syncline's formation was influenced by the movement of magma beneath the Earth's surface.

(470) The formation of laccoliths occurs when magma is injected between layers of sedimentary rock.

(471) The composition of microlites can vary depending on the type of magma from which they formed.

(472) The formation of melilite is influenced by the chemical composition of the surrounding magma.

(473) The subducting plate can trigger the formation of magma chambers beneath the Earth's surface.

(474) The cooling magma in the Earth's crust crystallizes to form different types of igneous rocks.

(475) Intraplate seismicity can be influenced by the movement of magma beneath the Earth's surface.

(476) The presence of ferromagnesian minerals can indicate that the rock formed from a mafic magma.

(477) The formation of norite is typically associated with the cooling and solidification of magma.

(478) The liquidus temperature of a magma determines the type of volcanic eruption that will occur.

(479) The formation of igneous rocks can be affected by the presence of gases in the magma or lava.

(480) The molten magma erupted from the volcano, and it covered the surrounding landscape with ash.

(481) The abundance of baddeleyites in a rock sample can provide information about the magma source.

(482) Geologists believe that granophyre was formed during the late stages of magma crystallization.

(483) Diabases are formed from the solidification of magma or lava deep beneath the Earth's surface.

(484) Diorite is often found in mountainous regions and is formed through the slow cooling of magma.

(485) The formation of hornblende is closely associated with the cooling and solidification of magma.

(486) The seismicity in this region is a result of the movement of magma beneath the Earth's surface.

(487) The crystalisation of minerals in volcanic rocks can indicate the cooling history of the magma.

(488) Nephelinite can be found in volcanic regions with a high concentration of mantle-derived magma.

(489) The monzonitic texture is often associated with the crystallization of magma at shallow depths.

(490) The process of contact metamorphism is driven by the transfer of heat from a nearby magma body.

(491) If diapirism is present, it can cause the upward movement of magma towards the Earth's surface.

(492) The mafic magma chamber beneath the volcano is thought to be the source of the recent eruption.

(493) The peralkaline magma that formed this mountain range is estimated to be millions of years old.

(494) The diatreme is a type of volcanic vent that is formed by a violent explosion of gas and magma.

(495) The formation of batholites is closely linked to the movement of magma within the Earth's crust.

(496) The diabases in this area are believed to have formed from magma that cooled slowly underground.

(497) The diatreme is a result of the explosive release of magma and gases during a volcanic eruption.

(498) The presence of ferromagnesian minerals can indicate that the rock formed from a basaltic magma.

(499) The cooling of magma in the Earth's mantle causes it to crystallize into various types of rocks.

(500) The petrogenesis of plutonic rocks is influenced by the depth and duration of magma emplacement.

(501) The formation of igneous rocks can be affected by the chemical composition of the magma or lava.

(502) The petrogenetic analysis revealed that the granite was formed from the crystallization of magma.

(503) The mineralogy of aplites can provide clues about the source of the magma from which they formed.

(504) The study of xenocrysts can help determine the source of the magma that formed a particular rock.

(505) The crystals accrete with regard to the cooling of the magma, creating unique mineral formations.

(506) The granodiorite formation is a result of the slow cooling of magma deep within the Earth's crust.

(507) Granites are formed deep within the Earth's crust through the cooling and solidification of magma.

(508) The ophitic texture is a result of the crystallization of minerals within a cooling magma chamber.

(509) The rheologic model accurately predicted the flow behavior of the magma during volcanic eruptions.

(510) The mineralogy of anorthosites can vary depending on the specific composition of the parent magma.

(511) The formation of anorthosites is thought to be related to the cooling and solidification of magma.

(512) Hornfels is commonly found in areas where there has been volcanic activity or intrusions of magma.

(513) The asthenosphere is a region of the Earth's mantle that is responsible for the movement of magma.

(514) The composition of igneous rocks can vary depending on the type of magma or lava that formed them.

(515) The formation of igneous rocks can be influenced by the chemical composition of the magma or lava.

(516) The formation of hot springs is a geologic process that occurs when groundwater is heated by magma.

(517) The formation of amygdaloids is a complex process that involves the interaction of magma and gases.

(518) The presence of xenocrysts suggests that the magma incorporated foreign material during its ascent.

(519) The formation of analcime is influenced by the temperature and composition of the surrounding magma.

(520) The formation of melilite is influenced by the cooling rate of the magma from which it crystallizes.

(521) The composition of a batholite can vary depending on the type of magma that intrudes into the crust.

(522) The study of tachylytes helps scientists understand the behavior of magma during volcanic eruptions.

(523) Xenocrysts can be used to trace the origin of volcanic eruptions and their associated magma sources.

(524) Eucrites are thought to have formed from the cooling and solidification of magma on Vesta's surface.

(525) The xenocrysts in this sample suggest that the magma chamber was mixing with other sources of magma.

(526) The texture of igneous rocks can be used to determine the type of magma from which they were formed.

(527) The seismic activity in the region is a result of the movement of magma beneath the earth's surface.

(528) The formation of lamprophyre is associated with the intrusion of magma into existing rock formations.

(529) Diorite is formed through the slow cooling and solidification of magma deep within the Earth's crust.

(530) The concretionary shapes in the volcanic ash were created by the cooling and solidification of magma.

(531) The felsic magma chamber beneath the surface is responsible for the geothermal activity in this area.

(532) Laccoliths are igneous rock formations that result from the intrusion of magma into the Earth's crust.

(533) The augitic composition of this rock indicates that it formed from a magma rich in iron and magnesium.

(534) The trachytes in this area were formed from the solidification of magma deep within the Earth's crust.

(535) The formation of nephelite is often associated with the cooling of magma deep within the Earth's crust.

(536) The formation of nephelite is influenced by the availability of certain chemical elements in the magma.

(537) The xenocrysts in this sample are believed to have been transported by a process called magma mingling.

(538) The texture of diorites can provide clues about the cooling history of the magma from which they formed.

(539) The chemistry of feldspathoids can provide insights into the source of the magma from which they formed.

(540) The cooling of hot magma in the Earth's crust causes it to crystallize into different types of minerals.

(541) Phonolite is commonly found in volcanic regions and is formed from magma that has a high silica content.

(542) Old Faithful's eruptions are caused by the heating of groundwater by a magma chamber beneath the surface.

(543) The formation of dolerites is often associated with the intrusion of magma into existing rock formations.

(544) Microlites can be used to track the evolution of magma chambers and the processes that occur within them.

(545) The formation of diorites involves the cooling and solidification of magma deep within the Earth's crust.

(546) The gabbroic composition of this rock suggests that it originated from a magma chamber beneath a volcano.

(547) The term phreatomagmatic refers to volcanic eruptions that occur when magma comes into contact with water.

(548) The presence of xenocrysts suggests that the magma underwent a complex history of mixing and assimilation.

(549) The composition of tephra can vary depending on the type of volcano and the minerals present in the magma.

(550) Dacites, which have a high viscosity, tend to erupt explosively due to the trapped gases within the magma.

The word usage examples above have been gathered from various sources to reflect current and historical usage of the word Magma. They do not represent the opinions of TranslateEN.com.