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geo 8
geo guide
chapter 8.2
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Cards (19)
Ocean currents
1.
Wind
blows from
same
direction for long time
2.
Seawater
starts to
flow
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Ocean currents
Can bring warmer water from
tropics
to
polar
regions
Can carry
cold polar water
to
warmer
zones
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Ocean currents
Influence
average
temperature on
land
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Gulf Stream
Warm ocean current that flows past Norway, bringing
warm
water from
Gulf of Mexico
to west coast of Europe
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The
Earth's
crust is divided into
tectonic plates
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Tectonic plate movement
1. Plates can move
apart
(divergence)
2. Plates can move
towards
each other (convergence)
3. Plates can
slide past
each other (transform movement)
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Divergence
Magma rises up from
mantle
and flows away as
lava
, filling gap between plates and forming new crust
Creates
mid-ocean ridges
with
low-lying areas
in between
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Convergence -
Oceanic
plate and
continental
plate
Heavier
oceanic plate slides under lighter continental plate (
subduction
)
Forms
deep
underwater trenches
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Convergence
- Two oceanic plates
Older,
heavier
plate slides under younger plate
Forms deep
underwater
trenches
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Convergence
- Two continental plates
Forms mountain
ranges
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Transform movement
Plates slide past each other, e.g. San Andreas
Fault
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Types of volcano
Stratovolcano
(composite volcano)
Caldera
volcano
Shield
volcano
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Stratovolcano
Formed by
subduction
Steep
slopes
Made of layers of
lava
and
ash
Thick
,
dense
magma
Explosive
eruptions when pressure is
high
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Stratovolcano eruption
1.
Thick
lava flows down slope
2.
Volcanic
bombs,
ash
, toxic gas and steam fly high into air
3.
Pyroclastic
flow races down slope
4. Danger of deadly mudflows from
melting
ice and
snow
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Caldera volcano
Large
crater
caused by collapse of empty magma chamber after eruption
Often has
crater
lake and new
crater
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Shield volcano
Formed by
plate divergence
Thin
, flowing lava
Flattened
slopes shaped like a
shield
Non-explosive
eruptions
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The Earth has existed for about
4.6 billion
years
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Geological time chart
Divides
Earth's
geological history into different
periods
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Fossils
Petrified imprints of plants and animals preserved in
Earth's
crust, used to determine
geological
period
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