boundaries
at ornearpeace
inter
plate
TECT fVICS
some
volcanoes distant
theme ma are
mom
destructive volcanoes earthquakes miaporenet
atracesand
spotsconerapate
earonananesnotoccurmid
areus
noms rate
a ssociatedwonmaior
ayyy ayy m
i i
magnanimous movement
i
i earthismadeupor large
i i minorplatesand
platesseveral
transfernearfromthecoretoonebrittle rotsormicro
places
lithosphere
stab run lithospheric in an wegenerproposedme
platesmoveawaymom earns once
were
continents
midocean winedtoform
one and
coldandridges
single
dense theysineastheybecome
subduction
easeoronepatesinkingbelowthe evidenceforpangaea
or omer
edge an
similarroar typesround
floorspreading
sea geologicalprocesswherelarge betweencontinents
southAmerica arica and
sassorearerisionospheresplitapartfromeach
other
fossil
evidence resfossils
nearer
onision earenquares wooo areninereptile
found onairerent
subance so push
men but
continents c onantswim
Beniorezone anareawithintheEarth'sreauency
crust
airtarentmountainranges
i whereearonauanesfrequentlyoccur one sittogetherandrock
types
areduetoconvergenceand
orearonauarestectonic moonnomdifferentcontinent
auctionor
sub plates
ionosphere
ionosphere
tstn.r
rgg.gg
transform earthquakes hazards
Primary
mais snomoneepicentre
amice
m em
as
groundsharing
seismic waves
sidewayspast union
eacnooner
secondaryhazards
iii
causestensionresuming ninnywanes
epicentre
inearmanares
and masuaes places
very common
asthepressurebuildsone wavesarrivesecond
secondary radiate
t.IM
crustcanwaccurereleasing epicure
mom mompower meas
moreroarparaciessidetoside
avalanches snowy
moreenergyasearenanares liquefaction incensesnaringcompacts
coreand ranywaves typesorsurface loose water
togetherforcing
sediment
waveseatonesmoveacross
m upenoughsediment undermines
andcausesbuildings
tgungggons
and sudden
riskorreenoes remains
ocean
send
the result of an earthquake
usually
totunaup
theicecaps
Hoodormelted
orglaciers
waterfromunder
neatorexplosion
from mini
lava moltenmagma that'sreachedthesurface
andis inliquidformegbasalticlavas
quickly
whicharelessviscoussonowvery
repuracanapesorerectedmaterialand
poisonous unionmoveuptozooamin
g ases
prate
i
downonesideoronevolcanoandcanbeup i
toooo
volcanicgases i
mostcommonvolcanicgasreleased i shieldvolcanoes are
vapourwhichcan
iswater causemass
Volcano
Shield by
characterised sloping
rainran cooledlavalayers
tephra mixorsolidandmoltenrockfragments haverunnylavawhich
x
butmore before
canars mixedwith
water apneapiecesvery
fastandcarrytoesorsediment
eggL
socan
easilysweepawaypeopleandbuildings
ashtail asnevenedmomvolcanocanbevery
heavyandevenonionbuildings
at ornearpeace
inter
plate
TECT fVICS
some
volcanoes distant
theme ma are
mom
destructive volcanoes earthquakes miaporenet
atracesand
spotsconerapate
earonananesnotoccurmid
areus
noms rate
a ssociatedwonmaior
ayyy ayy m
i i
magnanimous movement
i
i earthismadeupor large
i i minorplatesand
platesseveral
transfernearfromthecoretoonebrittle rotsormicro
places
lithosphere
stab run lithospheric in an wegenerproposedme
platesmoveawaymom earns once
were
continents
midocean winedtoform
one and
coldandridges
single
dense theysineastheybecome
subduction
easeoronepatesinkingbelowthe evidenceforpangaea
or omer
edge an
similarroar typesround
floorspreading
sea geologicalprocesswherelarge betweencontinents
southAmerica arica and
sassorearerisionospheresplitapartfromeach
other
fossil
evidence resfossils
nearer
onision earenquares wooo areninereptile
found onairerent
subance so push
men but
continents c onantswim
Beniorezone anareawithintheEarth'sreauency
crust
airtarentmountainranges
i whereearonauanesfrequentlyoccur one sittogetherandrock
types
areduetoconvergenceand
orearonauarestectonic moonnomdifferentcontinent
auctionor
sub plates
ionosphere
ionosphere
tstn.r
rgg.gg
transform earthquakes hazards
Primary
mais snomoneepicentre
amice
m em
as
groundsharing
seismic waves
sidewayspast union
eacnooner
secondaryhazards
iii
causestensionresuming ninnywanes
epicentre
inearmanares
and masuaes places
very common
asthepressurebuildsone wavesarrivesecond
secondary radiate
t.IM
crustcanwaccurereleasing epicure
mom mompower meas
moreroarparaciessidetoside
avalanches snowy
moreenergyasearenanares liquefaction incensesnaringcompacts
coreand ranywaves typesorsurface loose water
togetherforcing
sediment
waveseatonesmoveacross
m upenoughsediment undermines
andcausesbuildings
tgungggons
and sudden
riskorreenoes remains
ocean
send
the result of an earthquake
usually
totunaup
theicecaps
Hoodormelted
orglaciers
waterfromunder
neatorexplosion
from mini
lava moltenmagma that'sreachedthesurface
andis inliquidformegbasalticlavas
quickly
whicharelessviscoussonowvery
repuracanapesorerectedmaterialand
poisonous unionmoveuptozooamin
g ases
prate
i
downonesideoronevolcanoandcanbeup i
toooo
volcanicgases i
mostcommonvolcanicgasreleased i shieldvolcanoes are
vapourwhichcan
iswater causemass
Volcano
Shield by
characterised sloping
rainran cooledlavalayers
tephra mixorsolidandmoltenrockfragments haverunnylavawhich
x
butmore before
canars mixedwith
water apneapiecesvery
fastandcarrytoesorsediment
eggL
socan
easilysweepawaypeopleandbuildings
ashtail asnevenedmomvolcanocanbevery
heavyandevenonionbuildings
