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Types of Employment
Employment
Unemployment
Employment
People are in work, receive a regular
wage
, and pay
tax
to the government
Unemployment
People are not in
work
, do not receive a wage, and do not pay
tax
Sectors of Industry
Primary
Secondary
Tertiary
Quaternary
Primary industry
Creating raw materials such as farming, mining, and forestry
Secondary industry
Manufacturing goods
from
raw materials
Tertiary
industry
Providing
services
Quaternary industry
High-tech research and design
Primary industry was around
70
% in 1800-1900, falling to
20%
by 2000
Secondary
industry
was around 30% in 1800-1900,
falling
to 20% by 2000
Tertiary
industry
was around 10% in 1800-1900,
rising
to 50% by 2000
Quaternary industry was emerging up to
10%
by
2000
Globalisation has led to the world becoming more interconnected through
trade
and
cultural exchange
Improvements in transportation, such as larger containers, have
decreased
the cost of transporting goods between countries, accelerating
globalisation
Organisations like the World Trade Organization have promoted freedom of
trade
Calculating percentage change
1. Work out
difference
between the
two
numbers
2.
Divide
this number by
original
number
3.
Multiply
by
100
Factors affecting population density
Physical geography
Economic
factors
Political
factors
Social
factors
The
Demographic Transition
Model is a
simplification
of the more complex changes in population over time
An
aging
population has a higher average age, caused by
lowered
birth rates and rising life expectancy
Migration
The
movement
of people from one place to another, either
temporarily
or permanently
Layers of the Earth
Crust
Mantle
Outer core
Inner core
Crust
The
thin
, outer solid rock layer of the Earth,
0-60km
thick
Mantle
The largest section of the Earth, approximately
2900km
thick, made of
semi-molten
rock
Outer core
The liquid layer surrounding the inner core, made of iron and nickel,
extremely hot
Inner core
The solid, innermost layer of the Earth, made of iron and
nickel
, with temperatures up to 6,500°C
Types of plate boundaries
Constructive
(apart)
Destructive
(together)
Conservative
(slide past)
Types of volcanoes
Active
Dormant
Extinct
Focus
Source of the
Earthquake
Epicentre
Point on earth's surface directly above the
focus
Seismic Waves
Fast waves of
energy
generated, travel rapidly from the focus of the
earthquake
Fault Lines
Breaks or
fractures
in the earth's
crust
Volcano eruption
1.
Lava
erupts to the earth's surface
2.
Lava
cools and hardens
3.
Layers
of lava build up to form a volcano
4.
Melting
of the oceanic plate releases gases
5.
Increased
pressure forces the magma to
rise
to the earth's surface
Volcano
Magma from the
mantle
passes through the earth's crust and reaches the
surface
Lava flow
Molten
rock flows across the surface of the earth at speeds of up to
700
mph
Temperature
between 700°C and 1200°C
Cools
and
solidifies
into igneous rock
Lahars
Mud
and
debris
flows down the side of the volcano
Speeds between
20-40
mph
Can cover distances of over
50
miles from the crater
Pyroclastic flow
Speed
avalanches
of hot rock, ash and gas that move down the side of a
volcano
Temperatures up to
1600°C
Speeds up to
150
mph
Volcanic ash
Small fragments of rock and volcanic gas
Ejected
over
5
miles into the air
Volcanic bombs
Large
pieces of rock sometimes the same size as
cars
Thrown out of the
volcano
Fall
to the ground quickly at greater speed than
ash
Volcano prediction
1. Monitoring
volcanoes
2.
Taking
readings from various devices and technology
3. Determine changes in the volcano to
predict
eruption
Volcano planning
1. Drawing up
evacuation
plans
2. Using
hazard
maps to prevent building in
high
risk areas
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