The Solar System
consists of a star (the
Sun) and stuff orbiting
it
Planets
Mercury
Venus
Earth
Mars
Jupiter
Saturn
Uranus
Neptune
Mercury, Venus,
Earth and Mars
are called INNER
PLANETS
Jupiter, Saturn, Uranus and Neptune are called OUTER PLANETS
Eight planets
Pluto is not a
planet anymore
Orbit in almost circular paths
Elipses
The asteroid planet
comes between the
inner and outer planets
Asteroids and comets are made from stuff that was left over from the Solar System's formation
Asteroids are lumps of rubble an rock
Comets are balls of rock, dust and ice
Orbit the sun in very long elipses
The sun is at the end of the elipses
When a comet
approaches the sun, the
ice melts leaving a tail of
gas and debris
The Solar System is about
5 thousand million years
old
Formed over long periods of
time from big clouds of dust and
gas
1) A cloud started to get squeezed
slightly
Nearby exploding star
2) Particles got closer together
and gravity caused the cloud to
collapse on itself
At the centre of the
collapse a protostar was
formed
3) Fusion started when
the temperature got
high enough
Hydrogen particles
joined together to
make helium
Gives out a lot of heat and
light which created a star
(the Sun)
4) Around the sun, hydrogen,
helium and other heavier elements
clumped together to make planets
Sun and planets are similar ages
We know the Solar System is at least 4500 million years old
This is because the
oldest rocks on Earth are
meteorites that crashed
into the Earth about 4500
million years ago
Stars and Planets are very different
Stars are huge, very hot and
give out lots of light
Planets are a lot smaller
and reflect sunlight
Our Solar System is in the Milky Way Galaxy
There are about
100,000,000,000 in the galaxy
They create spiral arms leading
out from the centre
The Sun is about halfway along one of the arms
The distance between each star in the solar system is millions
of times greater than the distance between the planets in the
Solar System
The Universe is made up of millions of galaxies
You can measure distances in the
Universe by using light years
This is the distance that light travels through a
vacuum in one year
You need to know relative sizes and
distances of different stuff in space
And some ages
Earth - 5000 years
Sun - 5000 years
Universe - 14,000 years
Lesson 2:
Looking into
Space
We can tell a lot about a star by
studying the electromagnetic
radiation
The colour of a star is a good guide
to working out its surface
temperature
There are various
methods to work out
how far away a star is
1) For 'nearby'
stars you can use a
parallax
Astronomers
take pictures of
the sky six
months apart
This is when the
Earth is at opposite
sides of its orbit
A parallax is when
something appears to
move when you look at it
from different places
The apparent movement of the
star between the two photos
Stars further away appear to move less
2) You can also measure its brightness
Unfortunately a star that looks very bright
from Earth could either be
a) Quite close to Earth but not
actually that bright
b) Or a long way away and very bright
Astronomers know how
much radiation certain
types of star actually emit,
though, so by examining
the brightness, they can
tell how far from Earth it is
The Atmosphere and Light Pollution cause
some problems though
The atmosphere absorbs a lot of light before
it can reach us
Light pollution makes it hard to see dim objects
Light pollution is light thrown upwards
from street lamps, etc.
This is why scientists put the Hubble telescope into space -
where you can't get these problems
We see stars and galaxies as they
were in the past
Electromagnetic radiation travels very fast
The Sun is about 150 million km away from
Earth so the radiation from the Sun reaches
us 8 minutes after it has left the Sun
This means we see the
Sun as it was 8 minutes
ago
The nearest star to our star is about
4.2 light years away from us
This means the light takes 4.2 years to reach us
We see the star as it was 4.2 years ago
For other stars, the effect is more extreme
The North Star is about 430 light years away, whihc means we see it
as it was during the time of William Shakespeare
Lesson 3:
The Life of
the Universe
When a galaxy is moving away
from us, the wavelength of the light
changes and becomes redder
This is called red shift
By measuring how much the light has been
red-shifted you can work out how quickly it
is moving away
The greater the red shift, the faster it is moving away
From observations of different red shifts of
different galaxies we know that the more
distant the galaxy the faster it moves away
from us
This proves that the Universe is expanding
Th Big Bang Theory
All the galaxies seem to be moving apart from a single point
According to the theory, all the matter and
energy in the Universe must have been
compressed in a very small space
It then exploded and expanded and the expansion is still going on
The age of the Universe can be estimated from the current rate of expansion
They think the Big Bang happened about 14 thousand million years ago
It is difficult to estimate because it is
hard to tell how much the expansion
has slowed down
The Universe's ultimate fate depends on
how fast it's expanding and the total mass
there is in it
To calculate the speed of
expansion, large distances
need to be measured
Because of the size of the
Universe it is hard to accurately
measure the distances involved
Also need to observe the motion
of objects accurately
Only assumptions can be made
Pollution gets in the way
Difficult to measure mass
because most of it appears to be
invisible
Doesn't glow like a star
The amount of dark matter in
the Universe has not been
measured
Scientists aren't exactly sure what it is
The dark matter will dictate the
future of the Universe
All the mass is attracted together by gravity
The more mass there is, the greater the pull and the
greater the slowing down of the Universe's expansion
If there is enough mass compared to how fast the
galaxies are moving the Universe will eventually stop
expanding
This will cause it to contract
The Big Crunch
If there's not enough mass in
the Universe to stop the
expansion, it could expand
forever
Universe becoming more
and more spread out into
eternity
Lesson 4: The
Changing
Earth
The Earth has been
changing for thousands of
millions of years
Rocks provide a record of changes to the Earth
Erosion
The slow wearing away of
soil/rock by water flow or
wind.
Cliffs worn away by the sea
The Grand Canyon
Making new rock
When lava from volcanoes
sets, it forms new rock
Fossils
Rocks built up around
dead animals and plants
The oldest rocks found on Earth so
far are about 4 thousand million
years old
The rock cycle
1) Particles eroded from existing rock get
washed into the sea and settle as sediment
These sediments are crushed
together to make sedimentary rocks
2) These can get pushed to the surface or they can
descend into the heat and pressure inside the Earth
If they descend, the structure of
the rock can completely change as
it gets heated and crushed
Sometimes the rock actually melts and
will solidify into new rock on the Earth's
surface
3) When any of these rocks are pushed up
to the surface, the cycle starts again
They gradually get worn down
and carried off to the sea again
and so on
The rock cycle needs dome very powerful forces to push rock up
or down as described - but there's very good evidence that this is
what happens.
For example, some rock formations show rock that's been squeezed so hard it's just folded
Lesson 5:
Wegener's Theory
of Continental
Drift
Past beliefs
For years, fossils of very similar plants
and animals had been found on
continents at opposite ends of the
Atlantic Ocean
People thought this was because the continents had been linked by
land-bridges which had sunk or been covered in water as the Earth
cooled
Why the coastlines of South America and Africa
matched so well was also unknown
People also didn't understand why fossils of sea
creatures had been found in the Alps
Alfred Wegener hypothesised that
Africa and South America had
previously been one continent which
had then split
He found evidence to back up his hypothesis
There were matching layers in
the rocks on different
continents
There were similar fossils in both South America and
South Africa
His theory of continental drift supposed that
300 million years ago there had been just one
supercontintent which he called Pangaea
According to Wegener, Pangaea broke into smaller
chunks which are our continents which are still slowly
drifting apart
A lot of people opposed his theory because it
opposed things said in the land-bridge theory
These were things like mountains being
formed as continents crashed into one
another
Scientist's reactions were hostile
Wegener's explanation of how the
drifting was happening wasn't
convincing enough because the
movement wasn't detectable
Wegener suggested that tidal
movement or the Earth's rotation
could cause the drifting
Geologists showed this was impossible
It also didn't help that Wegener was a meteorologist not a 'proper' geologist,
which was frowned upon
New evidence
In the 1950's, scientists discovered the
Mid-Atlantic ridge, which runs the whole length of
the Atlantic
The found evidence that magma rises up through
the sea floor, solidifies and forms underwater
mountains that are roughly symmetrical
This suggested that the sea floor
spread by a few centimetres per year
Evidence that the continents are moving
apart came from the magnetic orientation
of the rocks
As liquid magma erupts out of the gap, iron particles
align themselves with the Earth's magnetic field and
as it cools, they set in position
Every half a million years, the
Earth's magnetic orientation
swaps direction and the rocks
on either side of the ridge has
bands of alternate magenetic
polarity, syymetrical about the
ridge
This was convincing evidence of how the sea floor was
created and how the continents were moved apart
Lesson 6:
The Structure
of the Earth
The Earth is almost spherical and has layers
The Crust
We live on it
20 km thick
Continental crust
Forms the land
Oceanic crust
Under oceans
The Mantle
Properties of solid
Flows slowly
The Outer Core
Hot
Radioactive decay
Heat and decay cause mantle to flow in convection currents