to the dramacan contributeto the drama

from volcano inflationresultingfrom volcano inflation

the damages or disasters(passive) caused bythe damages or disasters

from the passage of seismic waves during an earthquake eventresultedfrom the passage of seismic waves during an earthquake event

of sensors of different types and able to measure the deformations of the volcano with millimetric precisioncomposedof sensors of different types and able to measure the deformations of the volcano with millimetric precision

scientists to conclude that the source of magma erupted by Chaiten was an inclined reservoir system that originated about 12.5 miles beneath Michinmahuida volcano , 10 miles east of Chaitenledscientists to conclude that the source of magma erupted by Chaiten was an inclined reservoir system that originated about 12.5 miles beneath Michinmahuida volcano , 10 miles east of Chaiten

scientists to conclude that the source of magma erupted by Chaitén was an inclined reservoir system that originated about 12.5 miles beneath Michinmahuida Volcano , located 10 miles east of Chaiténledscientists to conclude that the source of magma erupted by Chaitén was an inclined reservoir system that originated about 12.5 miles beneath Michinmahuida Volcano , located 10 miles east of Chaitén

scientists to conclude that the source of magma erupted by Chaitén was an inclined reservoir system that originated about 20 km ( 12.5 miles ) beneath Michinmahuida Volcano , located 17 km ( 10 miles ) east of Chaiténledscientists to conclude that the source of magma erupted by Chaitén was an inclined reservoir system that originated about 20 km ( 12.5 miles ) beneath Michinmahuida Volcano , located 17 km ( 10 miles ) east of Chaitén

in non - uniform settlements or change in earth pressuresresultingin non - uniform settlements or change in earth pressures

structures to settle or tipcausingstructures to settle or tip

by an imposed load 2causingby an imposed load 2

high pore pressures in excess of equilibrium hydrostatic valuescausehigh pore pressures in excess of equilibrium hydrostatic values

damage to the near - by structures , buildings , pipelinesmay causedamage to the near - by structures , buildings , pipelines

movements(passive) caused bymovements

a debris avalanchecausesa debris avalanche

to significant problemscan leadto significant problems

serious environmental issues such as infrastructure damage , ground compaction , and reducing the ground capacity to store watercan causeserious environmental issues such as infrastructure damage , ground compaction , and reducing the ground capacity to store water

from the movement of magma undergroundresultingfrom the movement of magma underground

from the landslideresultingfrom the landslide

buried structures and utilities from potential ruptures(passive) are ... caused byburied structures and utilities from potential ruptures

hazards such as flooding and damages to urban infrastructures , both above and below the ground surface , including buildings , roads , railway systems and water supply and sewage systemscan causehazards such as flooding and damages to urban infrastructures , both above and below the ground surface , including buildings , roads , railway systems and water supply and sewage systems

adjacent panels to move independentlycausingadjacent panels to move independently

the interferometric phase(passive) caused bythe interferometric phase

cracking(passive) caused bycracking

to small changes in the reflected radar signalsleadsto small changes in the reflected radar signals

from fault displacementresultingfrom fault displacement

from shield tunnelling in soft claysresultingfrom shield tunnelling in soft clays

a large bending moment(passive) caused bya large bending moment

from the last two GPS surveys carried out in March 2006 and September 2007 on the Lipariresultingfrom the last two GPS surveys carried out in March 2006 and September 2007 on the Lipari

in 1 fringe ( 2 radiansresultingin 1 fringe ( 2 radians

to possible structure failuresleadingto possible structure failures

from magma intruding beneath the Leilani Estates subdivisionresultingfrom magma intruding beneath the Leilani Estates subdivision

using data from satellite passes from 1996 through 2000createdusing data from satellite passes from 1996 through 2000

the propagation of numerous cracks in the invertcausedthe propagation of numerous cracks in the invert

from accumulation of magma beneath the surfaceresultingfrom accumulation of magma beneath the surface

the processes(passive) caused bythe processes

in the separationresultingin the separation

of broad subsidence affecting the entire volcanic edifice andcomposedof broad subsidence affecting the entire volcanic edifice and

from the levee construction and to modify construction activities accordingly to mitigate further movementcausedfrom the levee construction and to modify construction activities accordingly to mitigate further movement

in earthquakes and volcanic activity on an apocalyptic scalewill resultin earthquakes and volcanic activity on an apocalyptic scale