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Qaagi - Book of Why

Causes

Effects

Lava flows20 - 35 km long originatedfrom small shield volcanoes

In addition , it has a considerable level of hotspot / heat pipe volcanismleadingto large shield volcanoes

The Big Islandcomposedof 5 shield volcanoes

Hotspots Hotspotscan also causeshield volcanoes to form

Hotspotscan also causeshield volcanoes to form

the islandscomposedof lava formed by shield volcanoes

The base of the Topo complexoriginatedin numerous shield volcanoes

almost(passive) are ... composedThe insides of a shield volcano

the lava , the faster it flowsleadingto flatter ( shield ) volcanoes

the faster it flowsleadingto flatter ( shield ) volcanoes

a circular island with a diameter of 24 kmcomposedof a deep - sea shield volcano

Perry Mesa ... basalt - capped mesas and canyons along the Agua Fria Riverresultedfrom the eruption of the shield volcano

The hotter the lava , the faster it flowsleadingto flatter ( shield ) volcanoes

The hotter the lava , the faster it flowsleadingto flatter ( shield ) volcanoes

a volcanic complexcomposedof overlapping shield volcanoes

of relatively thin lava flows built up over a central vent(passive) are composed almost entirelyShield volcanoes

of relatively thin lava flows built up over a central vent(passive) are almost entirely composedThe shield volcanoes

of basalt(passive) are usually composedShield volcanoes

of basalt(passive) are almost entirely composedShield volcanoes

of basaltic magma(passive) are composedthe shield volcanoes

to be maficresultingin shield volcanoes

The Hawaiian Islandsare composedof shield volcanoes

More than 80 percent of the volcanismhas resultedin shield volcanoes

by divergent tectonic plates pulling apart Pacific Ring Fire convergent coming together(passive) caused byvolcanoes

by divergent tectonic plates pulling apart Pacific Ring Fire convergent(passive) caused byvolcanoes

by divergent tectonic plates pulling apart the Pacific Ring of Fire(passive) caused byvolcanoes

global warmingcausessubsurface volcanoes

by " divergent tectonic plates"?that is , plates pulling apart(passive) caused byvolcanoes

Convergent and divergent tectonic plate boundariescausevolcanoes

divergent tectonic plates Pacific Ring of Fire(passive) caused byvolcanoes

by subduction where there are convergent plate boundaries , also where hot spots are located(passive) caused byvolcanoes

subduction where there are convergent plate boundaries , also where hot spots are located(passive) caused byvolcanoes

due to the pulling apart of divergent tectonic plates(passive) have been causedvolcanoes

by divergent tectonic plates pulling apart(passive) caused byvolcanoes

divergent tectonic plates pulling apart(passive) are commonly caused byVolcanoes

divergent tectonic plates pulling apart(passive) caused byvolcanoes

" divergent tectonic plates " pulling apart(passive) caused byvolcanoes

movement of tectonic plates which allow the release of heat to escape to the surface(passive) are commonly caused byVolcanoes

What type of tectonic plate movementcausesvolcanoes

by the same type of tectonic plate activity that caused the earthquake of 2010(passive) caused byvolcanoes

from dominantly mafic flows that are effusive in characterresultfrom dominantly mafic flows that are effusive in character

This island(passive) is composedThis island

The island(passive) is composedThe island

of basaltcomposed largelyof basalt

The Big Island of Hawaii(passive) is composedThe Big Island of Hawaii

3,000 m below the ocean 's surface along the Cameroon lineoriginating3,000 m below the ocean 's surface along the Cameroon line

from dominantly mafic flows that are effusive in characterresultfrom dominantly mafic flows that are effusive in character

of surface alkalineare composedof surface alkaline

its unique , seahorse - shape(passive) composed byits unique , seahorse - shape

under the oceanhas been discoveredunder the ocean

The island(passive) is composedThe island

damage , death and much morecan causedamage , death and much more

destructive lava flows in Hawaiicausingdestructive lava flows in Hawaii

to the formation of the Cappadocia regioncontributedto the formation of the Cappadocia region

of old lavacomposedof old lava

of stacked basaltic lava flowsgenerally composedof stacked basaltic lava flows

The caldera(passive) is composedThe caldera

from gentle eruptions of low viscosity basaltic magmaalso resultfrom gentle eruptions of low viscosity basaltic magma

mainlycomposedmainly

of silica poor lavascomposed mostlyof silica poor lavas

of rhyolite lava flows and ash - flow tuffscomposedof rhyolite lava flows and ash - flow tuffs

of rhyolite lava flows and ash - flow tuffs of similar compositioncomposedof rhyolite lava flows and ash - flow tuffs of similar composition

the highest mountaincausesthe highest mountain

from volcanic eruptionsresultingfrom volcanic eruptions

of the igneous rock , basaltprimarily composedof the igneous rock , basalt

The Hawaiian Islands(passive) are composedThe Hawaiian Islands

to workhave contributedto work

Sea Level Above sea level(passive) are composedSea Level Above sea level

to Mazama 's growthcontributedto Mazama 's growth

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

changes to Earth?s climate , recent eruption in Iceland too small to have an impactcan causechanges to Earth?s climate , recent eruption in Iceland too small to have an impact

at least a little to Antarctic ice sheet meltare ... contributingat least a little to Antarctic ice sheet melt

from the melting of subducted crust material or of rising mantle at mid - ocean ridges and mantle plumesresult primarilyfrom the melting of subducted crust material or of rising mantle at mid - ocean ridges and mantle plumes

in other natural disasters such as earthquakes , tsunamis , and floodscan resultin other natural disasters such as earthquakes , tsunamis , and floods

large flows of lava and sometimes ash flowscan causelarge flows of lava and sometimes ash flows

big earthquakes and tsunamiscan also causebig earthquakes and tsunamis

primarily from the melting of subducted crust material or of rising mantle at mid - ocean ridges and mantle plumesresultprimarily from the melting of subducted crust material or of rising mantle at mid - ocean ridges and mantle plumes

other natural disasters like earthquakes , tsunamis , and mudslidescan causeother natural disasters like earthquakes , tsunamis , and mudslides

mudflows , avalanches , tsunamis , and cracks in the Earth s surfacecan causemudflows , avalanches , tsunamis , and cracks in the Earth s surface

from the melting of subducted crust materialresult primarilyfrom the melting of subducted crust material

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