convergent boundaries - mr. schermer, crescent middle school · 2018-09-07 · symbols white arrows...

2
Mountains & valleys Spreading center—Fast Spreading center—Slow Divergent boundaries occur mostly along spreading centers where the magma rises forming new crust. (Ex. East Pacific Rise, Mid Atlantic Ridge.) Spreading zones (no graphic) on continents create parallel mountains and valleys as the crust pulls apart (ex: Basin & Range, U.S. and the Great Rift Valley, Africa. ) Divergent Boundaries & Spreading Zones L ithosphere Asthenosphere Oceanic crust Mantle Partial melt Asthenosphere Crust Mantle L ithosphere Partial melt Convergent Boundaries Mountain Range Old oceanic crust Continental crust High Plateau Continental crust Lithosphere Lithosphere Asthenosphere Trench Oceanic crust Continental crust Lithosphere Lithosphere Asthenosphere Asthenosphere Island arc Oceanic crust When two plates move toward each other, crust is destroyed as one plate dives (is subducted) beneath the other. The location where sinking of a plate occurs is called a subduction zone. Ocean-Ocean—Ocean plate dives beneath another ocean plate; volcanic island chain forms above the zone (ex:. The Marianas) Ocean-Continent: Ocean plate dives beneath a continental plate. Volcanic mountain chain forms inland. (ex:. Cascade Range, Sumatra, Japan) Continent-Continent: Two thick continental plates collide and buckle into high mountains. (ex: Himalaya Mountain Range.) Trench Continental crust Lithosphere Lithosphere Asthenosphere Volcanic arc . . . . . . . . . . . . . . . . . . . . Oceanic crust Transform Boundaries As surrounding plates are driven by deep forces to move apart or crunch together, the in-between areas are pushed around on the surface. This forces them to slide past each other horizontally. Transform faults are where two plates are moving away from a spreading ridge and fracture zones develop (ex: ocean floor) Asthenosphere Crust Lithosphere Asthenosphere Crust Transform fault Lithosphere Spreading ridge Partial melt Spreading ridge Strike slip faults result from two plates moving horizontally in opposite directions (ex: San Andreas Fault, California). Page-size map on next page for World Tectonic Map Activity The T O TLE Picture T e a c h e r s o n t h e L e a d i n g E d g e Earthquakes Volcanoes Tsunamis . . .

Upload: others

Post on 01-Jun-2020

2 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Convergent Boundaries - Mr. Schermer, Crescent Middle School · 2018-09-07 · SYMBOLS White arrows show plate motion direction Volcanoes (generalized) Hot spot (arrow = direction

Mountains & valleys

Spreading center—Fast Spreading center—SlowDivergent boundaries occur mostly along spreading centers where the magma rises forming new crust. (Ex. East Pacific Rise, Mid Atlantic Ridge.)

Spreading zones (no graphic) on continents create parallel mountains and valleys as the crust pulls apart (ex: Basin & Range, U.S. and the Great Rift Valley, Africa. )

Divergent Boundaries & Spreading Zones

Lithosphere

Asthenosphere

Oceanic crust

Mantle

Partial meltAsthenosphere

Crust

MantleL ithosphere

Partial melt

Convergent Boundaries

Mo

un

tain

Ran

ge

Old oceanic crust

Cont inental crust

HighPlateau

Continental crust

L i thosphere Lithosphere

Asthenosphere

Trench

Oceanic crust

Cont inental c rust

L i thosphere Lithosphere

Asthenosphere

Asthenosphere

Isla

nd

arc

Oceanic crust

When two plates move toward each other, crust is destroyed as one plate dives (is subducted) beneath the other. The location where sinking of a plate occurs is called a subduction zone.

Ocean-Ocean—Ocean plate dives beneath another ocean plate; volcanic island chain forms above the zone (ex:. The Marianas)

Ocean-Continent: Ocean plate dives beneath a continental plate. Volcanic mountain chain forms inland. (ex:. Cascade Range, Sumatra, Japan)

Continent-Continent: Two thick continental plates collide and buckle into high mountains. (ex: Himalaya Mountain Range.)

Trench

Cont inental c rust

L i thosphere Lithosphere

Asthenosphere

Vo

lca

nic

a

rc

..

..

..

........

..

.. . .

Oceanic crust

Transform Boundaries

As surrounding plates are driven by deep forces to move apart or crunch together, the in-between areas are pushed around on the surface. This forces them to slide past each other horizontally.

Transform faults are where two plates are moving away from a spreading ridge and fracture zones develop (ex: ocean floor)

Asthenosphere

Crust

L i thosphere

Asthenosphere

Crust

Transform fault

L i thosphere

Spreading ridge

Partial melt

Spreading ridge

Strike slip faults result from two plates moving horizontally in opposite directions (ex: San Andreas Fault, California).

Page-size map on next page for World Tectonic Map Activity

The TOTLE Picture

Teac

hers on the Leading Edge

Earthquakes Volcanoes Tsunamis

. ..

Page 2: Convergent Boundaries - Mr. Schermer, Crescent Middle School · 2018-09-07 · SYMBOLS White arrows show plate motion direction Volcanoes (generalized) Hot spot (arrow = direction

SY

MB

OL

S

Wh

ite

arro

ws

sho

w p

late

mo

tio

n d

irec

tio

n

Volc

ano

es (g

ener

aliz

ed)

Ho

t sp

ot

(arr

ow

= d

irec

tio

n o

f pla

te m

oti

on

)

Gre

at e

arth

qu

akes

sin

ce 1

900;

bef

ore

190

0

Div

erge

nt m

argi

n

Conv

erge

nt m

argi

n

Tran

sfo

rm fa

ult

(arr

ow

s sh

ow

rela

tive

mo

tio

n)

PL

AT

E B

OU

ND

AR

IES

Mo

st o

f th

e w

orl

d’s

eart

hq

uak

es a

nd

vo

lcan

oes

are

fo

un

d a

t o

r nea

r th

e b

ou

nd

ary

bet

wee

n t

wo

tect

on

ic

pla

tes.

Fri

ctio

n b

etw

een

th

e p

late

s ke

eps

them

fro

m

slid

ing.

Wh

en t

he

fric

tio

nal

str

ain

is o

verc

om

e, t

he

gro

un

d s

ud

den

ly s

nap

s al

on

g fa

ult

s an

d fr

actu

res

rele

asin

g e

ner

gy

as e

arth

qu

akes

. Vo

lcan

oes

occ

ur a

t di

verg

ent m

argi

ns (w

her

e m

agm

a ri

ses

and

eru

pts

); at

con

verg

ent m

argi

ns (w

her

e an

oce

anic

pla

te

div

es b

enea

th a

no

ther

pla

te; m

agm

a fo

rms

in t

he

con

tin

enta

l pla

te a

bov

e th

e d

ivin

g o

cean

ic p

late

), an

d le

ss c

om

mo

nly

as

hot s

pots

(w

her

e m

agm

a m

elts

th

rou

gh

a p

late

, su

ch a

s H

awai

`i).