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The ABC's of an by Jeffrey Karczewski

Jeffrey Karczewski Science Project

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For Jeffrey's Science Project, he created an ABC book about Earthquakes.

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Page 1: Jeffrey Karczewski Science Project

The ABC's of an

byJeffrey Karczewski

Page 2: Jeffrey Karczewski Science Project

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A is for Aftershock. An aftershock is a smallearthquake after a main earthquake but not aspowerful.

Page 3: Jeffrey Karczewski Science Project

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B is for Bedrock. This is relatively hard, solid

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rock that commonly underlies softer rock. Thisis safer in an earthquake.

Page 4: Jeffrey Karczewski Science Project

C is for Crust. Crust is the outer layer of theearth.

Page 5: Jeffrey Karczewski Science Project

D is for Damage. An earthquake causes a lot ofdamage.

Page 6: Jeffrey Karczewski Science Project

E is for Epicenter. An epicenter is the point ofthe earthquake

Page 7: Jeffrey Karczewski Science Project

Caftfornia's

San Andreas Fault

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San Andreas Fault 'lB,

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F is for Fault Line. A fault line is the surfacetrace of a fault.

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Page 8: Jeffrey Karczewski Science Project

G is for Geolosv. Scientists use geology fortracking where an earthquake will be next.

Page 9: Jeffrey Karczewski Science Project

H is for Hazard. Seismichazard is where twoconstantly moving plates meet.

Page 10: Jeffrey Karczewski Science Project

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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.

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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

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I is for lntensity. This is how strong anearthquake is.

Page 11: Jeffrey Karczewski Science Project

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J is for Jello. A wiggling Jello cube is a good

example of how buildings "wiggle" during anearthquake.

Page 12: Jeffrey Karczewski Science Project

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lndo-Austalian Plate

K is for Kinematic. Kinematic is the generalmovement patterns and directions of the earthsrocks that produce rock formations.

Page 13: Jeffrey Karczewski Science Project

L is for Lava. Lava causes sea floor spreading.Sea floor spreading causes earthquakes.

Page 14: Jeffrey Karczewski Science Project

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M is for Magnitude. Magnitude is the measureof the energy of an earthquake.

Page 15: Jeffrey Karczewski Science Project

N is for Noise. An earthquake produces ALOTof noise.

Page 16: Jeffrey Karczewski Science Project

b#O is for Oceans. A lot of earthquakes happenon the ocean floor.

Page 17: Jeffrey Karczewski Science Project

The Richterscale

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emitted b-Y earthguake

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severe darnagetopoollY brrilt ones

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R is for Richter Scale. The Richter Scale wasdesigned by Charles Richter. He applied anumber to how powerful an earthquake was.

Page 18: Jeffrey Karczewski Science Project

S is for Seismosraph. This is a machine thatrecords the P-Waves produced by anearthquake.

Page 19: Jeffrey Karczewski Science Project

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.

Page 20: Jeffrey Karczewski Science Project

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U is for Uplift. This happens when hrvo plates ofthe earth's core collide and one goes above theother.

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Page 21: Jeffrey Karczewski Science Project

V is for Volcano. Earthquakes often occurwhere Volcanos are, due to the movement ofmagma in Volcanos.

Page 22: Jeffrey Karczewski Science Project

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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.