Upload
karen-karczewski
View
219
Download
6
Tags:
Embed Size (px)
DESCRIPTION
For Jeffrey's Science Project, he created an ABC book about Earthquakes.
Citation preview
The ABC's of an
byJeffrey Karczewski
'&rt"
A is for Aftershock. An aftershock is a smallearthquake after a main earthquake but not aspowerful.
.di
Igeas.&
"1ft{riTriit .\C€ l'*il
B is for Bedrock. This is relatively hard, solid
- -J--L-)#
rock that commonly underlies softer rock. Thisis safer in an earthquake.
C is for Crust. Crust is the outer layer of theearth.
D is for Damage. An earthquake causes a lot ofdamage.
E is for Epicenter. An epicenter is the point ofthe earthquake
Caftfornia's
San Andreas Fault
Pctnt Reyee
Daly
San Lub OtiopoC,trizo
San Andreas Fault 'lB,
-r--l&pqndgho lxr6Dalit K Llmh
F is for Fault Line. A fault line is the surfacetrace of a fault.
Sanh Cruz'lJuan BautFtaSan
\\San
G is for Geolosv. Scientists use geology fortracking where an earthquake will be next.
H is for Hazard. Seismichazard is where twoconstantly moving plates meet.
I
[,i[.
lv.
Eqrthquoke lntensityrOnly instrumonts detect theeorlhq.roke.A'ow peope rclice lne 61crkng.Mo"ry p,eopb i^doors fee snokirg.I ong.r g cbjecls swi.rg.Feop16 outdocrs rroy fael groundshaking. Dishes. winoows. ondciocys raftloSleeoing people cre owo(enec.)oors swng: obiects ioll fromshelves.|)aopie hdv6 trouhle wclklng,lomoge is sitghi in poorty-tcuttbulldings.t*p'" have difficulty stonding.f,omoge E consrderobte rn popr1tbuil'l buildngs.)driers hove lrocble s:eering.)OOdy b,Llr Str.rctrjrss s!ffer s€Verecomoge, chlr.rneys rrov foll.
lX. lt'otFbuiit build ngs sJ,Ter co:sde* ,
obledomoge. Sorne unde.ground'pipes ore broken.\4os'l ollldings ore desl.oyed)oms ore s€'icusly domogcc.-orge ondslid€s occur,Siructuros collqp$e Up dgrgroundrjiif iies ore des:rcyod.Armce{ everylh ng s destroycd_ObJecls ore trrown into:h€ oir.' Ad{ra.sa t?r-:1"€ Vodlad trorrc iscolo
XI,
xll.
I is for lntensity. This is how strong anearthquake is.
flo,#
J is for Jello. A wiggling Jello cube is a good
example of how buildings "wiggle" during anearthquake.
G*a
\Pacitlc
lndo-Austalian Plate
K is for Kinematic. Kinematic is the generalmovement patterns and directions of the earthsrocks that produce rock formations.
L is for Lava. Lava causes sea floor spreading.Sea floor spreading causes earthquakes.
250
40r0EIDE rsoItt3tt!ruIaE
t0.
0.35 7 361 35.9 36 0 s.1
lhrttrrftrr lSilF ED8T
M is for Magnitude. Magnitude is the measureof the energy of an earthquake.
N is for Noise. An earthquake produces ALOTof noise.
b#O is for Oceans. A lot of earthquakes happenon the ocean floor.
The Richterscale
[r/lsl!ureE Energy vnaves
emitted b-Y earthguake
r'Dam4eloI well-bultrt tu#turcg,
severe darnagetopoollY brrilt ones
ii - l.$
J L.q
Car be detectedonly bY leirmogroPh
l-ilanging obiedtmay lwlng
(omparabletothe vibrations ofa pasrlng tl-,rck
fvlay break windows'rausa rmall oruPFtable objecrrto h'l
furniture rnQ$FE'
chr.rnks of Phster
@Plff,',*.iiJrnlefi standitrg
whh naked rye
R is for Richter Scale. The Richter Scale wasdesigned by Charles Richter. He applied anumber to how powerful an earthquake was.
S is for Seismosraph. This is a machine thatrecords the P-Waves produced by anearthquake.
T is for Tsunami. A tsunami is a really big wavethat can go up to speeds of 800mph. Tsunamisare often caused by earthquakes in the oceanfloor.
-
\.r
U is for Uplift. This happens when hrvo plates ofthe earth's core collide and one goes above theother.
-dr'sat'6rs8'|a '
V is for Volcano. Earthquakes often occurwhere Volcanos are, due to the movement ofmagma in Volcanos.
rc--\-ri sor*$rncrica.I ...,1
\
W is for Weqener. Alfred Wegener. He came upwith the theory of continental drift. His theoryhelped scientists learn about how the earthsplates shift and move.
Thc distribution of qlacial features can be bcst explainedif the conttnents we*re part of Par€aca.