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of fluid lava flow(passive) are composedShield volcanoes
This kind of lavacreatesshield volcanoes
runny lavacreateshield ’ volcanoes
Mt. The lavacreatesshield volcanoes
lava piling(passive) created bya shield volcano
Basaltic / mafic lavacreatesshield volcanoes
the highly fluid lava that erupts from the , and which travels further than the lava from stratovolcanoes(passive) is caused byShield Volcanoes
of quiet lava flows(passive) are composedShield volcanoes
primarily of lava flows(passive) are composedShield volcanos
Repeated outpourings of lavamay createshield volcanos
flows of very liquid lava(passive) was created bya shield volcano
the gradual addition of countless layers of lava(passive) created bya shield volcano ,
of relatively thin lava flows built up over a central vent(passive) are composed almost entirelyShield volcanoes
from fluid basalt lava flows(passive) are createdShield volcanos
of thousands of thin basalt lava(passive) are composedShield volcanoes
almost entirely of basalt(passive) are also composedShield volcanoes
of layers of basaltic lava flows(passive) are composed mostlyShield volcanoes
slow crawling of lava down its slopes(passive) was created bya massive shield volcano
The least viscous ( easy flowing ) lavacreatesshield volcanoes
a fissure to vent out directly as lava on the surfacecreatesshield volcanoes
of basalt ( whose lava flows easily and quickly(passive) are composed mostlyShield volcanoes
when lava emerges out from fissures in the earth 's crust(passive) are createdShield volcanoes
when red hot lava oozes out from cracks , or fissures in the earth 's crust(passive) are createdShield volcanoes
lightweight lava that is able to spread over a wider area of surface land creating a shield - like shape(passive) is created bya shield volcano
a hot spot in the earth(passive) are caused byShield volcanoes
flows of magma(passive) are caused byShield volcanoes
of which magma ( circle(passive) are usually composedShield volcanoes
runny magmacreatesshield volcanoes
as the hawaiian emperor seamount chain the hotspot locationclimaxesresultingin a shield volcano
of the same basalt that creates cinders(passive) are composedShield volcanoes
The hotspot position climaxes ,creatinga shield volcano
The hotspot location climaxes ,resultingin a shield volcano
subterranean drainage from the central magma chamber to rift zone(passive) caused bya shield volcano
a gap allowing rising magma to erupt st the surface ... then solidifyto createa shield volcano
As that gas escaped into the atmosphere , the rest of the magma would have poured out sluggishlyto createshield volcanoes
through the eruption of basaltic magmas , which flow easily and thus are capable of flowing over the landscape many miles from(passive) are createdShield volcanoes
on tensional plates ( plates which are moving apart(passive) are createdShield volcanoes
Instead , they ooze and spattercreatingshield volcanoes
usually(passive) are ... composedShield volcanoes
Volcanic hotspots and tectonic divergent boundariescreateshield volcanoes
of fluid lavascomposedof fluid lavas
from alternate layers of lava flowscreatedfrom alternate layers of lava flows
from a single caldera in the centre of the islandcreatedfrom a single caldera in the centre of the island
from a single caldera in the center of the Islandcreatedfrom a single caldera in the center of the Island
when the Indo - Australian tectonic plate moved over a hot - spot in the earth 's crustcreated almost seven million years agowhen the Indo - Australian tectonic plate moved over a hot - spot in the earth 's crust
almost entirely of hardened basaltic lava flowsis composedalmost entirely of hardened basaltic lava flows
of rhyolite lava flows and ash - flow tuffs of similar compositioncomposedof rhyolite lava flows and ash - flow tuffs of similar composition
of basaltic andesite that lies in Juab County about 20 miles northwest of Delta , Utahcomposedof basaltic andesite that lies in Juab County about 20 miles northwest of Delta , Utah
of old lava flowscomposedof old lava flows
primarily from fluid lava flowsresultsprimarily from fluid lava flows
gently sloping hills and mountains with a more - or - less domed shapecreategently sloping hills and mountains with a more - or - less domed shape
of basalt , which makes for fluid lava that rises from rather thancomposed mostlyof basalt , which makes for fluid lava that rises from rather than
almost entirely of fluid lava flowscomposedalmost entirely of fluid lava flows
of basalt , which makes for fluid lava[4 ] that rises from rather thancomposed mostlyof basalt , which makes for fluid lava[4 ] that rises from rather than
an island ... with frequent gentle eruptions that often results in lava flowing into the seahas createdan island ... with frequent gentle eruptions that often results in lava flowing into the sea
in the Battlement Mesa volcanic featuresmore easterly resultingin the Battlement Mesa volcanic features
an island roughly 30 kilometers ( 19 miles ... in diameter ... with a large crater in the centercreatedan island roughly 30 kilometers ( 19 miles ... in diameter ... with a large crater in the center
of nested about thirteen vents , calderas and craters composed of basaltic lavas and tephras ( air borne material produced by volcanic eruptionscomposedof nested about thirteen vents , calderas and craters composed of basaltic lavas and tephras ( air borne material produced by volcanic eruptions
in what was a shallow sea in prehistoric timessetin what was a shallow sea in prehistoric times
of rock fragments , volcanic ash , and other material formed by earlier eruptionscomposedof rock fragments , volcanic ash , and other material formed by earlier eruptions
from : Userresultfrom : User
into collapsed craters and calderashas resultedinto collapsed craters and calderas
lava tubescan sometimes createlava tubes
of lava flows , flow brecciascomposedof lava flows , flow breccias
thin , mafic lava(passive) are composedthin , mafic lava
of soda- and lime- rich feldspar and ferromagnesian minerals with small amounts of quartzcomposed mostlyof soda- and lime- rich feldspar and ferromagnesian minerals with small amounts of quartz
large , broad plateaus with gently sloping sides that resemble a shieldcreatelarge , broad plateaus with gently sloping sides that resemble a shield
the large diameter(passive) typically created bythe large diameter
flat slopes and a wide base that are created from lava flowcreateflat slopes and a wide base that are created from lava flow
from the eruption of basaltic lava in runny flows that can travel for milesresultfrom the eruption of basaltic lava in runny flows that can travel for miles
lava flows that gently glide down the slope of the mountain rather than spew out the top of the conecreatelava flows that gently glide down the slope of the mountain rather than spew out the top of the cone
of rhyolitic and andesitic lavas ( Mt. St. HelensComposedof rhyolitic and andesitic lavas ( Mt. St. Helens
mainlyComposedmainly
of andesitic magmacomposed mostlyof andesitic magma
in multiple different wayscan be createdin multiple different ways
of various lava streamscomposedof various lava streams
beautiful beaches , lagoons , and cavescreatedbeautiful beaches , lagoons , and caves
A volcano the size of New Mexico or the British Isles has been identified under the Pacific Ocean , about 1,000 miles ( 1,600 kilometers ) east of Japan , making it the biggest volcano on Earth and one of the biggest in the solar systemDISCOVEREDA volcano the size of New Mexico or the British Isles has been identified under the Pacific Ocean , about 1,000 miles ( 1,600 kilometers ) east of Japan , making it the biggest volcano on Earth and one of the biggest in the solar system
over several small lava flows and includes numerous peakswas createdover several small lava flows and includes numerous peaks
disastrous loss of life and property ... especially in densely populated regions of the worldcan causedisastrous loss of life and property ... especially in densely populated regions of the world