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of fluid lava flow(passive) are composedShield volcanoes
of relatively thin lava flows built up over a central vent(passive) are composed almost entirelyShield Volcanoes Shield volcanoes
Basaltic / mafic lavacreatesshield volcanoes
almost entirely of basalt(passive) are also composedShield volcanoes
from layers of lava(passive) are createdShield volcanoes
This kind of lavacreatesshield volcanoes
Mt. The lavacreatesshield volcanoes
runny lavacreateshield ’ volcanoes
of layers of basaltic lava flows(passive) are composed mostlyShield volcanoes
from fluid basalt lava flows(passive) are createdShield volcanos
of thousands of thin basalt lava(passive) are composedShield volcanoes
the highly fluid lava that erupts from the , and which travels further than the lava from stratovolcanoes(passive) is caused byShield Volcanoes
Repeated outpourings of lavamay createshield volcanos
primarily of lava flows(passive) are composedShield volcanos
of quiet lava flows(passive) are composedShield volcanoes
The widespread lava flowsoriginatefrom small shield volcanoes
of basalt ( whose lava flows easily and quickly(passive) are composed mostlyShield volcanoes
In addition , addition has a considerable level of hotspot / heat pipe volcanismleadingto large shield volcanoes
a continual eruption of lava at one spot(passive) are created bybroad shield volcanoes
The least viscous ( easy flowing ) lavacreatesshield volcanoes
a fissure to vent out directly as lava on the surfacecreatesshield volcanoes
The widespread , thin pahoehoe lava flowsoriginatefrom small shield volcanoes
when lava emerges out from fissures in the earth 's crust(passive) are createdShield volcanoes
of andesite ( a related , less dense type of lava(passive) are composedA few shield volcanoes
of the same basalt that creates cinders(passive) are composedShield volcanoes
when red hot lava oozes out from cracks , or fissures in the earth 's crust(passive) are createdShield volcanoes
flows of magma(passive) are caused byShield volcanoes
of which magma ( circle(passive) are usually composedShield volcanoes
runny magmacreatesshield volcanoes
Hawaiian eruptions ... most frequentlycreateshield - shaped volcanoes
from divergent boundaries or hotspots(passive) are createdShield Volcanoes
Volcanic hotspots and tectonic divergent boundariescreateshield volcanoes
As that gas escaped into the atmosphere , the rest of the magma would have poured out sluggishlyto createshield volcanoes
more than 80 percent of the volcanismhas resultedin shield volcanoes
usually(passive) are ... composedShield volcanoes
Instead , they ooze and spattercreatingshield volcanoes
a hot spot in the earth(passive) are caused byShield volcanoes
a volcanic complexcomposedof overlapping shield 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
that spreads outto createshield volcanoes
The Hawaiian Islands(passive) are composedThe Hawaiian Islands
lava tubescan sometimes createlava tubes
of rhyolite lava flows and ash - flow tuffs of similar compositioncomposedof rhyolite lava flows and ash - flow tuffs of similar composition
The caldera(passive) is composedThe caldera
almost entirely of fluid lava flowscomposedalmost entirely of fluid lava flows
thin , mafic lava(passive) are composedthin , mafic lava
The Hawaiian island chain(passive) was created byThe Hawaiian island chain
from alternate layers of lava flowscreatedfrom alternate layers of lava flows
of lava flows , flow brecciascomposedof lava flows , flow breccias
gently sloping hills and mountains with a more - or - less domed shapecreategently sloping hills and mountains with a more - or - less domed shape
one island when their flows overlappedcreatedone island when their flows overlapped
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
large , broad plateaus with gently sloping sides that resemble a shieldcreatelarge , broad plateaus with gently sloping sides that resemble a shield
broad flat slopescreatebroad flat slopes
from volcanic eruptionsresultingfrom volcanic eruptions
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
of alkaline lavas ( Mt. Choke and Gugugftu , 22 Mamainly composedof alkaline lavas ( Mt. Choke and Gugugftu , 22 Ma
of rhyolitic and andesitic lavas ( Mt. St. HelensComposedof rhyolitic and andesitic lavas ( Mt. St. Helens
mainlyComposedmainly
from the ocean floororiginatefrom the ocean floor
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
large mountains , known as Mons(passive) caused bylarge mountains , known as Mons
the largest and highest mountainshave createdthe largest and highest mountains
from : Userresultfrom : User
Other Features(passive) Created byOther Features
to Mazama 's growthcontributedto Mazama 's growth
the large diameter(passive) typically created bythe large diameter
in multiple different wayscan be createdin multiple different ways