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geo 8
geo guide
chapter 8.2
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Ocean currents
1.
Wind
blows from
same
direction for long time
2.
Seawater
starts to
flow
Ocean currents
Can bring warmer water from
tropics
to
polar
regions
Can carry
cold polar water
to
warmer
zones
Ocean currents
Influence
average
temperature on
land
Gulf Stream
Warm ocean current that flows past Norway, bringing
warm
water from
Gulf of Mexico
to west coast of Europe
The
Earth's
crust is divided into
tectonic plates
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)
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
Convergence -
Oceanic
plate and
continental
plate
Heavier
oceanic plate slides under lighter continental plate (
subduction
)
Forms
deep
underwater trenches
Convergence
- Two oceanic plates
Older,
heavier
plate slides under younger plate
Forms deep
underwater
trenches
Convergence
- Two continental plates
Forms mountain
ranges
Transform movement
Plates slide past each other, e.g. San Andreas
Fault
Types of volcano
Stratovolcano
(composite volcano)
Caldera
volcano
Shield
volcano
Stratovolcano
Formed by
subduction
Steep
slopes
Made of layers of
lava
and
ash
Thick
,
dense
magma
Explosive
eruptions when pressure is
high
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
Caldera volcano
Large
crater
caused by collapse of empty magma chamber after eruption
Often has
crater
lake and new
crater
Shield volcano
Formed by
plate divergence
Thin
, flowing lava
Flattened
slopes shaped like a
shield
Non-explosive
eruptions
The Earth has existed for about
4.6 billion
years
Geological time chart
Divides
Earth's
geological history into different
periods
Fossils
Petrified imprints of plants and animals preserved in
Earth's
crust, used to determine
geological
period