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clementaged.weebly.com Name: __________________________________________ ODD Period: ____________
Week: 6–7 Dates: 9/21–10/2 Unit: Mountain Building
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Assignment Your Score Total Points Possible
Good to Know Vocabulary Words 20
Frayer Vocab Words 20
Rock Deformation Notes 60
Mountain Formation Notes 60
Earthbeat:The Disappearing Mediterranean Article 20
Deformation CrossWord Puzzle 20
Snack Tectonics Lab 60
Mountain Building Quiz Study Guide 40
TOTAL 300
Monday Tuesday Wednesday Thursday Friday
21 O *Vocabulary *Frayer Vocab *Rock Deformation Notes
22 E 23 O *Mountain Formation Notes
*Snack Tectonics
24 E 25 O *Earthbeat Article
*O/C Ceremonies
28 E *Flex Day
29 O *R-2 Report *Study Guide *Crossword
30 E 1 O *Review *Unit Quiz *Packet Due
2 E Home FB Game
Ag Earth Science Fact of the Week
The world's highest peak on land is Mount Everest in the Himalayas. It is 8,850.1728 meters (29,036 ft) tall. Mountains make up about one-fifth of the world's landscape, and provide homes to at least one-tenth of the world's people.
Goal for this Unit
Write a goal for your academic performance on this unit (test score, packet score, study habits etc)
Good to Know Vocabulary WordsWord Definition
Deformation
Stress
Strain
Monocline
Normal Fault
Reverse Fault
Thrust Fault
Folded Mountain
Syncline
Anticline
Isostasy
Strike-Slip Fault
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�3
Rock DeformationCue Column
(titles, vocab, big ideas, test questions)
11.1 Rock DeformationPages 308-313
�4
Cue Column(titles, vocab, big ideas,
test questions)
11.1 Rock DeformationPages 308-313
�5
Summary(briefly describe the main concepts, major points)
Cue Column(titles, vocab, big ideas,
test questions)
11.1 Rock DeformationPages 308-313
�6
Mountain FormationCue Column
(titles, vocab, big ideas, test questions)
11.3 Mountain FormationPages 317-324
�7
Cue Column(titles, vocab, big ideas,
test questions)
11.3 Mountain FormationPages 317-324
�8
Summary(briefly describe the main concepts, major points)
Cue Column(titles, vocab, big ideas,
test questions)
11.3 Mountain FormationPages 317-324
�9
EarthBeat: The Disappearing Mediterranean
Two interesting regions in the world are the Alps and the Mediterranean Sea. The Alps, considered to be among the earth’s most beautiful mountains, have become a vast natural playground for skiers, hikers, and climbers. The Mediterranean plays host to travelers from around the world who wish to sample its diverse cultures, balmy climate, and famous beach resorts. More important, the people who live nearby depend on the sea for their economic well-being.
!
The same natural forces that produced the Alps are slowly swallowing up the Mediterranean. The Alps were formed, and are still being shaped, by the collision of two lithospheric plates. Italy, part of which rides on the African plate, collided sometime in the past with Eurasia. The collision formed the Alps, but it did not stop the movement of the African plate. The northern oceanic crust of the African plate, which is actually the sea floor of the Mediterranean, is still subducting beneath the continental crust of Eurasia. As more oceanic crust subducts, the Mediterranean Sea will become smaller. Italy, which continues to be pushed into Eurasia, will eventually cease to exist as we know it. When the northern coast of the African continent finally collides with Eurasia, the Mediterranean Sea will become just a memory, a photograph, perhaps, in some history book.
What do you think will happen to the Alps as the African plate continues to push northward?
_____________________________________________________________________
_____________________________________________________________________
_____________________________________________________________________
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Official Opening Closing Ceremony Script
President: (Taps gavel once, all officers sit except president; pause and tap the gavel twice) The Meeting room will come to order. We are now holding a meeting of the Santa Ynez FFA Chapter. Mr. / Madam Vice-president, are all officers at their stations?
Vice-President: (Rising and facing the president) I shall call the roll of officers, determine if they are at their stations and report back to you, Mr. / Madam President.
(President takes a seat)
Vice President: The Sentinel.
Sentinel: Stationed by the door.
Vice-President: Your duties there?
Sentinel: Through this door pass many friends of the FFA. It is my duty to see that the door is open to our friends at all times and that they are welcome. I care for the meeting room and paraphernalia. I strive to keep the room comfortable and assist the president in maintaining order.
Vice-President: The Reporter.
Reporter: The reporter is stationed by the flag.
Vice-President: Why by the flag?
Reporter: As the flag covers the United State of America, so I strive to inform the people in order that every man, woman and child may know that the FFA is a national organization that reaches from the state of Alaska to Puerto Rico and from the state of Maine to Hawaii.
Vice-President: The Treasurer.
Treasurer: Stationed at the emblem of Washington.
Vice-President: Your duties there?
Treasurer: I keep a record of receipts and disbursements just as Washington kept his farm accounts carefully and accurately. I encourage thrift among the members and strive to build up our financial standing through savings and investments. George Washington was better able to serve his country because he was financially independent.
Vice-President: The Secretary.
Secretary: Stationed by the ear of corn.
Vice-President: Your duties there?
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Secretary: I keep an accurate record of all meetings and correspond with other secretaries wherever corn is grown and FFA members meet. Mr. / Madam Vice-president, why do you keep a plow at your station?
Vice-President: The plow is the symbol of labor and tillage of the soil. Without labor, neither knowledge nor wisdom can accomplish much. My duties require me to assist at all times in directing the work of our organization. I preside over meetings in the absence of our president, whose place is beneath the rising sun.
Secretary: Why is the President so stationed?
Vice-President: The rising sun is the token of a new era in agriculture. If we will follow the leadership of our president, we shall be led out of the darkness of selfishness and into the glorious sunlight of brotherhood and cooperation. Mr. / Madam President, all officers are at their stations.
President: (Rises and faces vice-president) Thank you, Mr. / Madam Vice-president. (All sit at the tap of gavel except the secretary) The Secretary will call the roll of members.
Secretary: There are numerous members and numerous guests present, Mr. / Madam President.
President: Thank you, (secretary sits down) FFA members why are we here? (Tap gavel 3 times, all officers stand)
All officers in unisons: To practice brotherhood, honor agricultural opportunities and responsibilities, and develop those qualities of leadership, which an FFA member should possess.
President: (taps gavel 1 time, all officers are seated) May we accomplish our purposes. I now declare this meeting of the Santa Ynez FFA Chapter duly open for the transaction of business, or attention to any matters which may properly be presented.
(Pause for a moment, before beginning closing ceremony)
President: Mr. / Madam Secretary, (secretary stands and looks at the president) do you have a record of any further business which should now be transacted?
Secretary: I have none, Mr. / Madam President. (Secretary sits)
President: Does any member know of any new or unfinished business, which should properly come before this meeting?
We are about to adjourn this meeting of the Santa Ynez FFA Chapter. As we mingle with others, let us be diligent in labor, just in our dealings, courteous to everyone, and above all, honest and fair in the game of life.
I now declare this meeting adjourned. (Tap gavel 1 time)
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�13
Name
Date
(Key
# 1 -
3024
77)
Earth
Scie
nce -
Cha
pter
5Co
mplet
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6S R E
17
12
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18 N 28
5 K O N
16 A N
7
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19 M N
22
11 O13
S
9S N
2
23 H A
24
3
F U T
1 R U
N
UA
20R
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25RM
15
27S
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29O
26
4A
8
14 G
10F
UL
21
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!
!
1" LAB"B&6"!!
Name___________________!
Date____________________!
Snack&Tectonics&Purpose"
The!purpose!of!this!lab!is!to!visualize!the!interactions!at!plate!boundaries.!i!
Procedure""""""Materials"
1. Fruit!by!the!Foot!candy! ! 5.!Plastic!knife!2. Graham!crackers! ! 6.!Wax!Paper!3. Frosting! ! ! 7.!Plastic!cup!4. Water!
Sequence"of"Steps"Before&jumping&into&Part&I&below,&read&Background+Information&provided.&Highlight&key&concepts&and&important&points&to&remember.&&
*ALL!MEMBERS!OF!THE!LAB!GROUP,!THOROUGHLY!WASH!AND!DRY!HANDS!!*MAKE!SURE!YOUR!LAB!STATION!IS!CLEAN!AND!DRY!!*DO!NOT!EAT!ANY!MATERIALS!UNTIL!YOU!ARE!COMPLETELY!FINISHED!WITH!THE!LAB!!
&Part"I:"Divergent"Plate"Boundary"
1. Place!a!large!dollop!of!frosting!on!the!wax!paper.!!This!will!represent!the!fluid,!middle!mantle!or!asthenosphere.!!Notice!that!it!is!not!fluid!like!water,!but!is!thick!and!sticky.!!However,!the!asthenosphere!can!still!move!or!flow.!
2. Spread!the!frosting!to!an!approximate!thickness!of!0.5!cm!with!the!plastic!knife.!3. Place!the!two!oceanic!plates!(fruit!by!the!foot)!on!the!frosting!so!that!the!long!edges!are!
touching.!4. Gently!press!down!along!the!entire!edges!that!are!touching!(to!simulate!the!density!of!the!
plates)!and!spread!the!plates!about!0.5!cm!apart.!!(Continue!pushing!down!slightly!as!you!spread!the!plates!apart.)!
5. In!“observations”!draw!a!side!view!of!what!you!see!happening!(oceanic!plates!and!asthenosphere.)!!!(This!is!what!it!would!look!like!if!you!brought!your!eyes!down!to!the!level!of!the!plates!and!looked!at!the!ends!of!both!plates.)!
6. In!“observations”!draw!a!top!view!of!what!you!see!happening.!!!(This!is!what!it!would!look!like!if!you!were!in!an!airplane!flying!over!the!top!and!looking!down.)!
7. Remove!one!of!the!oceanic!plates!and!set!it!aside!to!use!later.!!DO"NOT"EAT"IT!!!
�15
!
!
2" LAB"B&6"!!
Part"II:"Convergent"Plate"Boundaries""Continental@Oceanic&Plate&Boundary&&
8. Smooth!out!the!asthenosphere!(frosting.)!9. Gently!place!one!of!the!continental!plates!(graham!cracker)!on!the!asthenosphere!so!that!it!is!
touching!the!long!edge!of!the!oceanic!plate.!!!10. Push!the!two!plates!together.!
a. Push!the!continental!plate!from!the!back!and!do!not!push!down!(to!simulate!that!continental!plates!are!not!very!dense.)!
b. Push!down!on!the!entire!length!of!the!oceanic!plate!that!is!touching!the!continental!plate.!
11. Draw!a!side!view!of!what!you!see!happening.!12. Draw!a!top!view!of!what!you!see!happening.!13. Remove!the!oceanic!plate!and!set!it!aside!to!use!later.!!DO"NOT"EAT"IT!!
"Continental@Continental&Convergent&Plate&Boundary&
14. Smooth!out!the!asthenosphere!(frosting.)!15. Fill!the!plastic!cup!with!water.!!Submerge!1!cm!of!each!of!the!continental!plates!(graham!
crackers)!for!1b2!seconds.!!BE!CAREFUL,!if!you!leave!the!plates!in!the!water!too!long,!this!part!will!not!work.!
16. Gently!place!the!continental!plates!on!the!asthenosphere!so!that!the!entire!wet"edges"are"touching.!
17. Without!pushing!down,!slowly!push!the!plates!together!from!the!back.!18. Draw!a!side!view!of!what!you!see!happening.!19. Draw!a!top!view!of!what!you!see!happening.!20. Remove!the!continental!plates!and!set!aside!for!later!on!a!paper!towel.!!DO"NOT"EAT"THEM!!!
Make!sure!that!the!edges!opposite!the!wet!edges!stay!dry!! Oceanic@Oceanic&Convergent&Plate&Boundary&
21. Smooth!out!the!asthenosphere!(frosting.)!22. Place!both!pieces!of!oceanic!crust!on!the!asthenosphere!so!that!the!long!edges!are!touching.!23. Gently!press!down!along!the!entire!edges!that!are!touching!and!push!the!plates!together.!!
Continue!pushing!down!slightly!as!you!push!the!plates!together.!24. .!!(Remember,!you!are!trying!to!show!how!both!plates!will!sink!into!the!mantle.)!25. Draw!a!side!view!of!what!you!see!happening.!26. Draw!a!top!view!of!what!you!see!happening.!27. Set!the!two!oceanic!plates!aside!for!later.!!DO"NOT"EAT"THEM!!
!Part"III:"Transform"Plate"Boundary"
28. Smooth!out!the!asthenosphere!(frosting.)!29. Gently!place!the!two!pieces!of!continental!crust!on!the!asthenosphere!so!that!the!dry"edges"are"
touching.!30. Hold!the!two!continental!plates!from!the!back!and!very!gently!push!them!together!as!you!slide!
one!plate!towards!you!and!one!plate!away!from!you.!31. Draw!a!side!view!of!what!you!see!happening.!32. Draw!a!top!view!of!what!you!see!happening.!
�16
!
!
3" LAB"B&6"!!
33. You"are"now"done"with"the"activity"and"may"eat"any"of"the"food"you"wish.""!34. Clean!up!your!lab!station!according!to!your!teacher’s!instructions.!!
!""Observations" "Complete&a&drawing&as&described&in&the&Sequence&of&Steps&for&each&plate&boundary.&Include&arrows&to&show&the&direction&the&plates&are&moving.&
PART!I!–!DIVERGENT!PLATE!BOUNDARY!
SIDE VIEW !!
TOP VIEW!!!!!!
!
PART!II!–!CONVERGNET!PLATE!BOUNDARY!
! 1!–!continentalboceanic!convergent!plate!boundary!
SIDE VIEW !!
TOP VIEW!!!!!!
2!–!continentalbcontinental!convergent!plate!boundary!
SIDE VIEW !!
TOP VIEW!!!!!!
! !
! 3!–!oceanicboceanic!convergent!plate!boundary!
SIDE VIEW !!!!!
TOP VIEW!!!!!!
�17
!
!
4" LAB"B&6"!!
PART!III!–!TRANSFORM!PLATE!BOUNDARY!
SIDE VIEW !!
TOP VIEW!!!!!!
"
ANALYSIS:""(Answer"with"complete"sentences,"using"actual"data.)"
1. When!plates!move,!which!type!will!float!higher!on!the!asthenosphere?!!Explain.!!
!
!
!
2. Why!is!it!important!to!know!what!types!of!plates!are!interacting!at!convergent!plate!boundaries,!but!not!at!divergent!or!transform?!!Explain.!
!
!
!
!
3. Draw!a!picture!showing!the!direction!of!plate!movement!and!convection!in!the!asthenosphere!for!a!divergent!plate!boundary.!!Next!to!the!drawing!explain!with!words,!why!plates!diverge.!
!
!
!
!
!
!
!
�18
!
!
5" LAB"B&6"!!
4. Draw!a!picture!showing!the!direction!of!plate!movement!and!convection!in!the!asthenosphere!for!a!convergent!plate!boundary.!!(This!can!be!a!simple!picture!and!does!not!need!to!represent!a!specific!type!of!convergent!plate!boundary.)!!Next!to!the!drawing!explain!with!words,!why!plates!converge.!
!!!!!!!!!!!!
5. Draw!a!picture!showing!the!direction!of!plate!movement!at!a!transform!plate!boundary.!!(Do!not!show!convection!in!the!asthenosphere.)!
!!!!!!!!!!!!!6. How!has!plate!movement!throughout!history!created!natural!resources!which!help!agricultural!
production,!as!well!as!natural!resources!which!hinder!agricultural!production?!Provide!at!least!two!examples!for!each.!
""""""""""""
�19
! !
6"LA
B"B&6"
! !Backgrou
nd"In
form
ation:"Sna
ck"Tectonics"
" !The
!crust!and
!upp
er!m
antle
!taken!together!are!called!
the!litho
sphe
re.!!Th
e!litho
sphe
re!is!broken!into!
sections!called!plates.!!Th
ese!plates!are!rigid!(hard!an
d!easily!breakable)!and
!floa
t!aroun
d!on
!the!middle!of!th
e!man
tle,!called!the!asthen
osph
ere.!!Just!like!a!bo
at!or!
raft!adrift!on!the!ocean!moves!in!wha
tever!d
irection!
the!water!und
er!it!m
oves,!a!plate!will!m
ove!in!
wha
tever!d
irection!the!asthen
osph
ere!be
low!it!m
oves.!!
Whe
n!the!ed
ges!o
f!two!plates!interact!(tou
ch),!a!plate!
boun
dary!is!created
.!!De
pend
ing!on
!the!way!th
e!tw
o!plates!m
ove!relativ
e!to!each!othe
r,!diffe
rent!ty
pes!o
f!plate!bo
unda
ries!a
re!created
.!!Th
ere!are!three!main!
type
s!of!p
late!bou
ndaries:!divergent,!con
vergen
t,!an
d!tran
sform.!
1"–!Divergent"Plate"Bou
ndary!–!Th
e!word!“diverge”!means!to
!spread
!apa
rt!or!g
o!in!opp
osite
!dire
ctions.!!Wha
t!cau
ses!p
lates!
to!diverge!is!m
aterial!in!the!asthen
osph
ere!rising!to!th
e!surface.!!A
s!the
!material!rise
s!to!the!surface,!it!coo
ls,!and
!turns.!!
Whe
n!the!asthen
osph
ere!turns,!it!drags!th
e!plates!with
!it,!thu
s!pu
lling
!them
!apa
rt.!!Th
e!gap!left!is!filled!with
!risin
g!lava,!w
hich!
ultim
ately!cools,!and
!form
s!new
!rock.!!!
" " 2"–"Co
nvergent"Plate"Bou
ndary!–!Th
e!word!“con
verge”!m
eans!to
!com
e!together.!!Th
is!situa
tion!is!created!whe
n!molten!material!in!the!
asthen
osph
ere!sin
ks!below
!the!bo
unda
ry.!!Th
e!material!tha
t!is!s
inking
!pulls!
the!plates!to
gether!as!it!sinks.!!Since!oceanic!plates!are!differen
t!tha
n!continen
tal!plates,!th
e!result!of!th
e!plates!com
ing!together!differs!d
epen
ding
!on
!which!ty
pes!o
f!plates!a
re!con
verging.!
A!–!Co
ntinen
tal&O
cean
ic"Con
vergen
t"Plate"Bou
ndary!–!
Continen
tal!plates!a
re!very!thick!(tha
t!is!w
hy!th
ey!stick!up
!ou
t!of!the
!ocean
)!and
!are!not!very!de
nse.!!The
refore,!
continen
tal!plates!float!very!high
!on!the!asthen
osph
ere.!!
Ocean
ic!plates,!how
ever,!are!very!thin!(tha
t!is!w
hy!we!ha
ve!
oceans)!a
nd!are!very!de
nse.!!O
cean
ic!plates!float!lower!in!
the!asthen
osph
ere.!!W
hen!a!thick,!not!den
se!con
tinen
tal!
! !
7"LA
B"B&6"
! !plate!collide
s!with
!a!th
in,!d
ense!ocean
ic!plate,!the
!ocean
ic!plate!sinks!u
nder!th
e!continen
tal!plate!and
!is!
forced
!lower!in!th
e!man
tle.!!Th
is!creates!a
!subd
uctio
n!zone
!and
!we!can!say!that!th
e!oceanic!plate!
subd
ucts!below
!the!continen
tal!plate.!!!
! B!–"Co
ntinen
tal&C
ontin
ental"C
onvergen
t"Plate"Bou
ndary!–!
Whe
n!tw
o!thick,!not!den
se!con
tinen
tal!plates!c
ome!
together,!n
either!will!sink!into!th
e!man
tle.!!Instead,!both!will!
crum
ble!an
d!pu
sh!upw
ards.!!!
"
C"&"O
cean
ic&Ocean
ic"Con
vergen
t"Plate!Bou
ndary!–!
Whe
n!tw
o!thin,!d
ense!ocean
ic!plates!c
ome!together,!
both!will!sink!into!th
e!man
tle.!!Th
is!creates!a
n!ocean!
tren
ch!as!the
!plates!a
re!pulled!lower!into!th
e!man
tle.!
3"–"Tran
sform"Plate"Bou
ndary!–!Ve
ry!com
plex!interactions!of!con
vection!
curren
ts!in!th
e!man
tle!create!a!tran
sform!plate!bou
ndary.!!The
refore,!w
e!will!
not!d
iscuss!e
xactly!how
!tran
sform!plate!bou
ndaries!a
re!created
,!only!that!a!
tran
sform!plate!bou
ndary!is!a!locatio
n!whe
re!tw
o!plates!are!sliding!ho
rizon
tally!
past!each!othe
r.!!!
HYP
OTH
ESIS:!!If!plate!interaction!is!mod
eled
,!the
n!the!type
s!of!p
late!bou
ndaries!c
an!be!visualized
.!
!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
i Loo
per,
Jim
(200
8).S
nack
Tec
toni
cs, L
ab. S
held
on H
igh
Scho
ol S
cien
ce D
ept.
Mountain Building Quiz Study Guide Directions: Answer the questions in complete sentences or phrases on a separate sheet of paper. Attach pages to packet when done.
11.1 Rock Deformation Vocab to know: Deformation, stress, strain, anitcline, syncline, monocline, normal fault, reverse fault, thrust fault, strike-slip fault
The factors that influence the strength of a rock and how it will deform include….?
Rocks deform permanently in two ways: ______________ and _______________
Forces that are unable to deform rock when first applied may cause rock to flow if the ____________ is maintained over a long period of time.
Describe the three types of stress.
List the three types of folds.
Explain the major types of faults.
Explain the direction and movement in the four types of faults.
How is an anticline different from a syncline.
At which type of fault boundary would compressional stresses be the dominant force?
What types of mountains are associated with convergent plate boundaries?
What mountains are associated with divergent plate boundaries?
11.3 Mountain Formation Vocab to know: Isostasy, isostatic adjustment, folded mountain, fault block mountain
Most mountain building occurs at which types of boundary?
What type of boundary mainly produces colic mountains?
What types of mountains are formed along oceanic-continental convergence?
At a convergent boundary between two continental plates, what land formation will result?
What kind of mountains are formed along oceanic ridges at divergent plate boundaries?
What is isostasy?
What plate is subjected at an oceanic-continental convergent boundary? Why?
When is a rift valley formed?
Big Questions Are our continents growing? Explain why or why not. Is California going to slide into the Pacific Ocean? Explain why or why not.
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