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Qaagi - Book of Why

Causes

Effects

a great earthquake in history(passive) caused bycrustal deformation

earthquake - related and volcanic processescausecrustal deformation

the 2011 off the Pacific coast of Tohoku Earthquake(passive) caused bycrustal deformation

Fault movement ( earthquake ) under the seafloorcausescrustal deformation

the 2016 Kumamoto earthquake revealed by GEONET / Satoshi Kawamoto in Bulletin of the GeoSpatial Information authority of Japan(passive) caused byCrustal deformation

the Nepal ( Gorkha ) Earthquake Using ALOS-2 SAR Interferometry(passive) Caused byCrustal Deformation

magma migration in the northern Izu Islands , Japan , Geophys(passive) caused byCrustal deformation

glacioisostatic uplift , which is going on until now(passive) caused bycrustal deformation

the tectonics activities(passive) caused byCrustal deformation

the 2016 Kumamoto Earthquake Revealed by GEONET Satoshi KAWAMOTO , Yohei HIYAMA , Reiko KAI , Fumio SUGA , Kazunori YAMAGUCHI , Tomoaki FURUYA , Satoshi ABE and Naofumi TAKAMATSU GNSS observation over the area of the 2016 Kumamoto Earthquake(passive) Caused by・Crustal Deformation

seasonal filling and emptying of four surface reservoirs of varying dimensions located in different geological domains of India(passive) caused bycrustal deformation

subsidence ( a decrease in the ground ’s elevation ) , landslides , earthquakes and volcanic activity(passive) caused bycrustal deformation

megathrust faulting ( Kato et al . 2011(passive) caused bycrustal deformation

an eruption of Mount Shinmoe(passive) caused byCrustal deformation

magmatic and tectonic processes(passive) caused bycrustal deformation

plate tectonics , earthquakes , landslides and volcanic eruptions(passive) caused bycrustal deformation

changing polar ice on a viscoelastic earth(passive) caused bycrustal deformation

changes in the weight of a column of air(passive) caused bycrustal deformation

subduction of the underlying lithosphere(passive) caused bycrustal deformation

glacial meltwater loading of the Indian Ocean basin(passive) caused bycrustal deformation

loading of glacier ice(passive) caused bycrustal deformation

fault ... the faultcausedcrustal deformation

Changing Polar Ice on a Visco - Elastic Earth , Surveys in Geophysics(passive) Caused byCrustal Deformation

disturbances arising at plate boundaries(passive) caused bycrustal deformation

the subducting oceanic plates(passive) caused bycrustal deformation

changes in the weight of a column of water(passive) caused bycrustal deformation

the parameters of the fault slipcausedcrustal deformation

elastic , viscous , and plastic deformation(passive) is ... caused bycrustal deformation

land subsidence from aquifer withdrawal , seasonal cycles of aquifer rehydration(passive) caused bycrustal deformation

glacial isostatic adjustment ( GIA(passive) caused bycrustal deformation

This interseismic stress relaxationcausescrustal deformation

Orogenesiscausescrustal deformation

three mechanismscausingcrustal deformation

hot spots and volcanic lava(passive) caused bycrustal deformation

time - varying TWS(passive) caused bycrustal deformation

extension in the western USA , Nature , 464 , Number 7290(passive) caused bywidespread crustal deformation

subduction of the underlying mantle(passive) caused bycrustal deformation

the rifting and spreading of the Okinawa Trough , which is viewed as a continuation of the Beppu – Shimabara graben ( Tada 1985(passive) caused bycrustal deformation

the intrusion of a magma body into the shallow depth region(passive) caused bycrustal deformation

the earthquakes along the fault(passive) caused bycrustal deformation

from glaco build - up and decay of great ice sheetsresultingfrom glaco build - up and decay of great ice sheets

to a positive feedback between erosion at the surface and shortening of the crust[Avouac and Burov , 1996]leadingto a positive feedback between erosion at the surface and shortening of the crust[Avouac and Burov , 1996]

gravity change(passive) are caused bygravity change

from the subduction of the Juan de Fuca oceanic plate beneath the North American continentresultingfrom the subduction of the Juan de Fuca oceanic plate beneath the North American continent

fluid migration(passive) caused byfluid migration

separation along a boundary of rock types ... typically between so - called crystalline " basement " rock and overlying sedimentary rockscausesseparation along a boundary of rock types ... typically between so - called crystalline " basement " rock and overlying sedimentary rocks

cracks that are much better conductors than solid rockcreatescracks that are much better conductors than solid rock

a Fault - a major cross - formation break with accompanying displacement o … f one side against the other(passive) caused tectonically bya Fault - a major cross - formation break with accompanying displacement o … f one side against the other

a glaciation cyclecausesa glaciation cycle

in increased crustal thickness and possibly dehydration and/or melting of thickened lower continental crustresultingin increased crustal thickness and possibly dehydration and/or melting of thickened lower continental crust

Horizontal and vertical offset(passive) caused byHorizontal and vertical offset

Subsidence , which refers to “ the loss of surface elevation due to removal of subsurface support , ” ... sediment compaction ; withdrawal of groundwater , hydrocarbons , geothermal fluids or minerals ( sulphur ) ; and dewatering of organic soils(passive) is caused bySubsidence , which refers to “ the loss of surface elevation due to removal of subsurface support , ” ... sediment compaction ; withdrawal of groundwater , hydrocarbons , geothermal fluids or minerals ( sulphur ) ; and dewatering of organic soils

several geophysical phenomenacausesseveral geophysical phenomena

to fracturesleadsto fractures

faulting(passive) caused byfaulting

from ALOS-2 / PALSAR-2 datacreatedfrom ALOS-2 / PALSAR-2 data

from the ongoing extensionalresultingfrom the ongoing extensional

gravity anomaliescausesgravity anomalies

from natural hazards at hourly intervalsresultingfrom natural hazards at hourly intervals

zones of weakness within the cratonic ( basement ) layer which in turn produced channels through which magma could move , thereby forming intrusive and extrusive rockscreatedzones of weakness within the cratonic ( basement ) layer which in turn produced channels through which magma could move , thereby forming intrusive and extrusive rocks

in both faults and foldsresultsin both faults and folds

to the preservation of subsided marshesmay also contributeto the preservation of subsided marshes

from instantaneous events ( e.g. earthquakesresultingfrom instantaneous events ( e.g. earthquakes

from earthquakes and volcanoesresultingfrom earthquakes and volcanoes

to great - earthquakes in Sumatra over the last 7,000 yearsleadingto great - earthquakes in Sumatra over the last 7,000 years

the surface of the Earth to change constantlycausesthe surface of the Earth to change constantly

to tectonic consequencesleadingto tectonic consequences

from convergence of the two tectonic platesresultingfrom convergence of the two tectonic plates

to geochemical variation in emitted gasesledto geochemical variation in emitted gases

to the stratigraphycontributingto the stratigraphy

gravity changes(passive) caused bygravity changes

volcanic eruption or near field earthquake action such as reservoircould triggervolcanic eruption or near field earthquake action such as reservoir

shallower earthquakes at a great distance from the trench(passive) to be caused byshallower earthquakes at a great distance from the trench

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