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Earthquake
A sudden
movement
or trembling of
Earth's
crust
Earthquakes occur
1. Plates
collide
or slide past one another
2.
Pressure
builds
up
3. One of the plates
slips
4.
Pressure
is eased
5. A huge amount of
energy
is suddenly released
Earthquake
Plates suddenly move along the fault line
The
focus
is the point deep underground where the
earthquake
occurs
Shock waves
or
tremors
spread out from the focus, causing Earth's surface to shake (or quake) for a period
The tremors are usually strongest at the epicentre, the area on the
surface
directly above the
focus
Most
tremors
last from a few seconds to up to a minute
Seismograph
Instrument that detects and measures tremors from an
earthquake
Pen on the tip of the seismometer records the tremors on a
rotating drum
to produce a
seismogram
The seismograph can detect
tremors
too
small
for a person to be aware of
Tsunami
A huge wave or series of waves, can be as high as
60
metres, usually a result of an underwater earthquake or
volcanic
eruption
How a tsunami is formed
1.
Ocean
floor at a
plate
boundary rises or falls suddenly
2.
Displaces
the water above it
3. Starts the
rolling waves
that grow to become a tsunami
Rock
is the
hardest
material that forms earth's crust.
All rocks are
solid
, occur naturally, and are made up of one or more
minerals
that have been compressed and cemented together.
Rocks differ from eachother in their:
Mineral
content
Colour
Hardness
Texture
3 types of rocks:
Igneous
Sedimentary
Metamorphic
Igneous rocks
Rocks formed as a result of
volcanic
activity
Formation of igneous rocks
1.
Volcanic
material cools down and
solidifies
2. Material that cooled inside the crust forms
intrusive
rocks
3. Material that cooled on the surface forms
extrusive
rocks
Sedimentary
rocks are formed from remains of other rocks, plant life, and
animal
life.
Remains are
compressed
and cemented together to make
sedimentary
rocks.
Rocks that allow
water
to pass through it are called
permeable.
Limestone
is the most common rock in
Ireland
Metamorphic rocks are formed when existing igneous or sedimentary rocks come into contact with great
heat
and
pressure.
Volcanic
activity takes place along the boundaries of plates.
Volcanic activity results in
mid-ocean ridges
or
volcanic cones.
A mid ocean ridge is an
underwater mountain range
formed when
two plates separate.
Geothermal
energy is made by hot water or
steam
Volcanic mountains are formed when
molten magma
erupts through a hole in the crust called a
vent.
Magma is called
lava
once it's over the surface
Erosion
:
wearing
away material from the surface
Transportation:
removing material the river has eroded.
Deposition
: dropping material the river was
transporting
Hydraulic
action: force of water breaking off material from banks and beds of
river.
Attrition
: material is worn down, smoother, and rounded by stones
bouncing
off eachother.
Solution:
acids
in the water dissolve some
rocks
Rivers
deposit their load when they lose energy, speed, volume decreases, or it flows into a lake or sea
Meander
: curve in a
river
Oxbow lake
: when the river gets too close and ends up cutting off the river
channel
making a U shaped lake.
Features of a river
Source
Course
Tributary
Confluence
Mouth
Estuary
Drainage basin
Watershed
Source
The point where a river
begins
Course
The route taken by a
river
as it flows into the
sea
Tributary
A small
river
or stream that joins a
larger
one
Confluence
The place where two
rivers
meet
Mouth
The place where a
river
enters the
sea
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