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UK rural and urban environments checklist

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UK rural and urban environments checklist

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DME Development in India Resource Booklet

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DME Development in India Resource Booklet

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SAMS (example exam papers for your spec )

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SAMS (example exam papers for your spec )

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https://www.bbc.co.uk/programmes/p00xf8dh

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https://www.bbc.com/education/guides/zt3xdmn/revision/6

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https://www.bbc.com/education/guides/zc7hwxs/revision

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https://www.bbc.com/education/guides/z3y9frd/revision/1

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https://www.bbc.com/education/guides/zcn6k7h/revision

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Only look at pages 4-6
https://www.bbc.com/education/guides/zctymnb/revision/4

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Global climate, tropical storms and drought KO

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Global climate, tropical storms and drought KO

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The rainforest consists of several layers. Each layer has plants and animals which are adapted to the conditions found there. In the ground layer, soil is poor and any nutrients are quickly recycled. The next layer is made up of shrubs and plants which can tolerate low light levels. The lush undercanopy consists of smaller trees which compete for the light and space. Epiphytes are found in the undercanopy. The canopy is a continuous layer of tall trees. Many animals live here. Occasionally trees push through the canopy to become emergents.

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Rainforest structure - layering - GCSE Geography - BBC Bitesize

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The rainforest consists of several layers. Each layer has plants and animals which are adapted to the conditions found there. In the ground layer, soil is poor and any nutrients are quickly recycled. The next layer is made up of shrubs and plants which can tolerate low light levels.

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Posters to get completed and get stuck on your wall. Try and get these done on A3 size paper

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2016 NIC

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2016 Rural tourism

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2015 DME Coasts

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Savanna biome 2015 (also covers desertification)

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2015 Water supply

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2015 Shopping

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2014 MNC

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Rural Urban migration

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Practice question2

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Practice questions 3

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Practice questions 4

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Amended from resource shared by another teacher - with w

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Lots of graph / map / numeracy questions

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Lots of graph / map / numeracy questions

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The strongest tropical storms are called hurricanes , or tropical cyclones . The different names all mean the same thing, but are used in different parts of the world. If these huge storms start in the Atlantic off the west coast of Africa, they are called hurricanes.

In an average year over a dozen hurricanes form over the Atlantic Ocean and head westwards towards the Caribbean, the east coast of Central America and the southern USA (Florida in particular). Hurricanes may last as long as a month and although they travel very slowly - usually at about 24 km/h (15 mph) - wind speeds can reach over 120 km/h (75 mph).

How hurricanes form

Hurricanes need a lot of heat to form and a sea surface temperature of at least 26°C, which is why they usually occur over tropical seas. They also need to be between 5 and 20° north or south of the Equator. It works like this:

When this warm and wet air rises, it condenses to form towering clouds, heavy rainfall. It also creates a low pressure zone near the surface of the water.

Rising warm air causes the pressure to decrease at higher altitudes. Warm air is under a higher pressure than cold air, so moves towards the 'space' occupied by the colder, lower pressure, air. So the low pressure 'sucks in' air from the warm surroundings, which then also rises. A continuous upflow of warm and wet air continues to create clouds and rain.

Air that surrounds the low pressure zone at the centre flows in a spiral at very high speeds - anti-clockwise in the northern hemisphere - at speeds of around 120 km/h (75 mph).

Air is ejected at the top of the storm - which can be 15km high - and falls to the outside of the storm, out and over the top, away from the eye of the storm. As this happens, it reduces the mass of air over the 'eye of the storm' - causing the wind speed to increase further. Some ejected air also cools and dries, and sinks through the eye of the storm, adding to the low pressure at the centre.

The faster the winds blow, the lower the air pressure in the centre, and so the cycle continues. The hurricane grows stronger and stronger.

Seen from above, hurricanes are huge circular bodies of thick cloud around 450 km (300 miles) wide. The cloud brings heavy rain, thunder and lightning.

In the centre is the eye of the hurricane, about 45 km across (30 miles) across. Often there will be no clouds in the eye. Seen from below it will seem calmer, with a circle of blue sky above. The eye is formed because this is the only part of the hurricane where cold air is descending.

In the northern hemisphere, the prevailing easterly tropical winds tend to steer hurricanes toward land - although their course is unpredictable. As hurricanes move inshore, their power gradually reduces because their energy comes from sucking up moist sea air.

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Hurricanes - Tropical storms - GCSE Geography Revision - BBC Bitesize

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The strongest tropical storms are called hurricanes , or tropical cyclones . The different names all mean the same thing, but are used in different parts of the world. If these huge storms start in the Atlantic off the west coast of Africa, they are called hurricanes.

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Flooding occurs when a river bursts its banks and overflows onto the surrounding land. There are many factors which can cause a flood - often the natural landscape can influence flooding and human interactions can increase the risk.

Causes of flooding

Prolonged rainfall - if it rains for a long time, the land around a river can become (it's holding as much water or moisture as can be absorbed). If there is more rainfall it cannot be soaked up, so it runs along the surface this is known as .

Heavy rainfall - if there is heavy rainfall there is less chance of it being soaked up by the soil ( ) so it runs off into the river. The faster the water reaches the river, the more likely it will flood. Water travelling over the surface (surface runoff) will reach a river quicker than water travelling through the ground ( through flow and groundwater flow).

- a steep valley is more likely to flood than a flatter valley because the rainfall will run off into the river more quickly.

- allow water to pass through pores and cracks, whereas do not. If a valley is made up of impermeable rocks, there is a higher chance of flooding as there is an increase in surface run-off.

Vegetation - trees and plants absorb water, this is known as . Lots of vegetation reduces flood risk. Sometimes people cut down trees ( ). This will increase the flood risk, as the water will not be intercepted and more will flow into the river.

Urban land use - when an area surrounding a river is built on, it increases the amount of tarmac and concrete, which are impermeable surfaces. Drains and sewers take water directly and quickly to the river which increases the flood risk.

Effects of flooding

Floods can cause damage to homes and possessions as well as disruption to communications. However, flooding can also have positive impacts. Flooding deposits fine (alluvium) onto the floodplain, making it very fertile and excellent for farming.

(LICs) are usually affected more than (HICs) by the impacts of flooding. LICs often do not have the resources to prevent flooding or deal with its aftermath. More people rely on agriculture in LICs and fertile floodplains are attractive places to live and so have high population densities.

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Flood risk - the causes of flooding - River flooding - causes and management - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Flooding occurs when a river bursts its banks and overflows onto the surrounding land. There are many factors which can cause a flood - often the natural landscape can influence flooding and human interactions can increase the risk.

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is the process that wears away the river bed and banks. Erosion also breaks up the rocks that are carried by the river.

There are four types of erosion:

Hydraulic action - This is the sheer power of the water as it smashes against the river banks. Air becomes trapped in the cracks in the rock of the river bank and bed, and causes the rock to break apart.

- When pebbles grind along the river bank and bed in a sand-papering effect.

- When rocks that the river is carrying knock against each other. They break apart to become smaller and more rounded.

- When the water dissolves certain types of rock, eg limestone.

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Different processes of erosion - River processes - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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is the process that wears away the river bed and banks. Erosion also breaks up the rocks that are carried by the river. There are four types of erosion: Hydraulic action - This is the sheer power of the water as it smashes against the river banks.

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Hard engineering strategies - advantages and disadvantages - Managing coastal hazards - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Learn about and revise managing coastal hazards and hard and soft engineering strategies with GCSE Bitesize Geography (Eduqas).

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The process of can create different landforms along the coastline.

Headlands and bays

along the coastline do not erode at the same pace. A cliff is a steep rock face. When a stretch of coastline is formed from different types of rock, headlands and bays can form.

Bands of soft rock such as clay and sand are weaker therefore can be eroded quickly. This process forms . A bay is an inlet of the sea where the land curves inwards, usually with a beach. Hard rock such as chalk is more resistant to the processes of erosion. When the softer rock is eroded inwards, the hard rock sticks out into the sea, forming a .

Erosional features such as and cliffs can be found on headlands, since they are more open to the waves. Bays are more sheltered with which deposit sediment to form a beach.

Cliffs and wave-cut platforms

Cliffs are shaped through erosion and . Soft rock erodes quickly and forms gentle sloping cliffs, whereas hard rock is more resistant and forms steep cliffs. A wave-cut platform is a wide gently-sloping rocky surface found at the foot of a cliff.

A wave-cut platform is formed when the following occurs:

The sea attacks the base of the cliff between the high and low water mark.

As the notch increases in size, the cliff becomes unstable and collapses, leading to the retreat of the cliff face.

The backwash carries away the eroded material, leaving a wave-cut platform.

The process repeats. The cliff continues to retreat.

Caves, arches, stacks and stumps

Caves, arches, stacks and stumps are erosional features that are commonly found on a .

are formed in the headland through the erosional processes of hydraulic action and abrasion.

As the waves continue to grind away at the crack, it begins to open up to form a .

The cave becomes larger and eventually breaks through the headland to form an .

The base of the arch continually becomes wider through further erosion, until its roof becomes too heavy and collapses into the sea. This leaves a (an isolated column of rock).

The stack is undercut at the base until it collapses to form a .

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Erosional landforms - Coastal landforms - erosion and deposition - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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The process of can create different landforms along the coastline. along the coastline do not erode at the same pace. A cliff is a steep rock face. When a stretch of coastline is formed from different types of rock, headlands and bays can form.

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BBC Bitesize Weather (Depressions and anticyclones)

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BBC Bitesize Weather (Depressions and anticyclones)

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is the day-to-day conditions of the atmosphere at a particular place. It includes temperature, precipitation, cloud cover and wind speed. is the average weather conditions of a place taken over a long period of time, typically 30 years.

The UK has a temperate climate . In general, this means that Britain gets cool, wet winters and warm, wet summers. It rarely features the extremes of heat or cold, drought or wind that are common in other climates. The conditions are also very changeable.

The first climate graph is for London, in the south-east of the UK. This region is characterised by a warm and dry climate in the summer and a cold and dry climate in the winter.

Not all parts of the UK have the same climate. The second climate graph is from Cumbria in the mountainous north-west of England. Notice that temperatures are generally cooler and there is more rainfall throughout the year.

The general pattern of the climate across the UK has four distinct regions:

the south-east - cold winters, warm and dry summers

the south-west - mild and very wet winters, warm and wet summers

the north-west - mild winter, cool summers and heavy rain all year

the north-east - cold winter, cool summers and steady rain all year

How has the climate changed over time?

The climate is continually changing. There is evidence, for example from fossils, which shows that during certain periods, the world was much warmer than it is now, and there was little ice on the North Pole. There is also evidence to suggest that at other times the ice cover was much greater than it is today. Since the 1950s, there has been evidence of a steep climb in global temperature compared to the past. This trend is linked to climate change.

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Climate and weather in the UK - Weather and climate in the UK - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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is the day-to-day conditions of the atmosphere at a particular place. It includes temperature, precipitation, cloud cover and wind speed. is the average weather conditions of a place taken over a long period of time, typically 30 years. The UK has a temperate climate .

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Droughts occur when there is abnormally low rainfall for an extended period of time. This means that a desert would not be considered in drought unless it had less rainfall than normal, for a long period of time. Droughts can last from weeks to months and even years.

Why are some areas more vulnerable to droughts?

Droughts can occur all over the world, however there is a link between drought and some climate patterns:

A lack of water vapour in the atmosphere means there is less and more chance of drought. High-pressure systems reduce evaporation and moisture in the atmosphere.

El Niño - as the surface temperature of the Pacific Ocean around the central South American coast , storm patterns are disrupted. This phenomenon is thought to create droughts in Indonesia and Australia.

La Niña - as the surface temperature of the Pacific Ocean around the central South American coast , storms are again disrupted and North and South America are prone to droughts.

Causes of droughts

There are three main types of drought:

Meteorological drought - when the amount of precipitation received in a specific area is less than the average.

Hydrological drought - when reduced precipitation impacts on water supply, eg there is decreased streamflow, soil moisture, reservoir and lake levels, and groundwater.

Agricultural drought - when the above two types of drought impact on agricultural activities, eg reduced soil moisture or reservoir levels required for .

Droughts can also be caused by human activities, for example:

Agriculture - using large amounts of water to irrigate crops removes water from lakes, rivers and groundwater. Some crops require more water than others, eg cotton.

Dam building - large dams can be built across a river to produce electricity and store water in a reservoir. This can reduce river water flowing downstream and cause drought below the dam.

Deforestation - removing trees can reduce the amount of water stored in the soil as rain tends to fall and wash off the land as . This leaves the ground vulnerable to erosion and which can lead to drought.

Climate change - it is predicted that climate change will cause some places around the world to get hotter, which will increase evaporation and some areas to receive less rainfall - both increasing the risk of drought.

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Characteristics and causes of droughts - Droughts - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Droughts occur when there is abnormally low rainfall for an extended period of time. This means that a desert would not be considered in drought unless it had less rainfall than normal, for a long period of time. Droughts can last from weeks to months and even years.

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Rural - urban links - GCSE Geography Revision - Eduqas - BBC Bitesize

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GCSE Geography Rural - urban links learning resources for adults, children, parents and teachers.

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BBC Bite size maths / numeracy / statistics

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BBC Bite size maths / numeracy / statistics

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Measures of data - Numerical and statistical skills - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Learn and revise numerical and statistical skills, including various measures of data and calculations, with GCSE Bitesize Geography (Eduqas).

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Fieldwork involves the collection of information or data. Quantitative data usually consists of factual information that can be counted and used in fieldwork. Qualitative data is more opinion-based, but is still useful for geographical investigations.

Data collection sheets

Data can either be:

primary - information that you collect yourself, eg tallies, measurements and photographs

secondary - information that someone else has previously collected and made available, eg on the internet

The design of primary data collection sheets is important. Simple methods of noting down information leads to clear and accurate data. Informed conclusions can then be drawn.

Sampling

It's important to collect enough data to give a good picture of events. Any data collected should not be biased , for example, some younger people might think that skate parks improve their city, but some older people might prefer gyms or cafes, so ask a mixture of different ages to gain a balanced view.

Sampling techniques help to avoid bias:

Random sampling - selecting a person to interview or site to measure, at random. Random sampling is unbiased as particular people or places are not specifically selected.

Systematic sampling - collecting data in an ordered or regular way, eg every 5 metres or every fifth person.

Stratified sampling - dividing sampling into groups, eg three sites from each section of coastline, or five people from each age range. It is possible to combine stratified sampling with random or systematic sampling:

stratified random sampling - random samples are taken from within certain categories

stratified systematic sampling - regular samples are taken from within certain categories

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Fieldwork - data collection and sampling techniques - Collecting data - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Fieldwork involves the collection of information or data. Quantitative data usually consists of factual information that can be counted and used in fieldwork. Qualitative data is more opinion-based, but is still useful for geographical investigations.

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Physical maps

Physical maps show natural features such as mountains, lowlands, major rivers, seas, oceans and like deserts and rainforests on a global scale. On a national scale, physical maps show and drainage features, such as rivers.

Some maps show physical features that are experienced rather than seen. Examples of this are average temperature and rainfall maps.

Human and political maps

Political maps show country boundaries and major cities. Human maps show features that people have created. Examples of these are population distribution , flows, and layout.

Some maps show human features that are experienced rather than seen. Examples of this are , or even measures of world happiness.

Often, maps should have a arrow to show which way is north. North is at the top of the globe and south is at the bottom. East is to the right and west is to the left. Compass points in between these four are shown as combinations, eg the point in between north and east is called north-east. If the point is slightly closer to the east, it is called east-north-east.

Latitude and longitude

As the Earth is a sphere, lines of latitude and longitude are measured using degrees of a circle.

Lines of run from east to west . The is a line of latitude that lies at 0°. Lines above this are shown as °N (north) and lines below this are shown as °S (south).

Lines of run from north to south. The or in London is a line of longitude at 0°. Lines to the right of this are shown as °E (east) and lines to the left of this are shown as °W (west).

Latitude is shown first and longitude is shown second, eg Manchester in the UK is at 53.5°N, 2.2°W.

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Types of atlas maps - Cartographic skills - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Physical maps show natural features such as mountains, lowlands, major rivers, seas, oceans and like deserts and rainforests on a global scale. On a national scale, physical maps show and drainage features, such as rivers. Some maps show physical features that are experienced rather than seen.

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Fieldwork in geography is all about following an enquiry . A geographical enquiry is an active, questioning approach to learning.

Types of enquiry

An enquiry is based on a question that you set out to answer. A hypothesis is very similar, though it is a statement rather than a question that you set out to prove or disprove. Both can be either physical or human in nature:

physical enquiries will look at natural landscapes, eg rivers or coasts

human enquiries will look at environments that are created by people, eg cities or tourist resorts

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Formulating an enquiry - Introduction to fieldwork - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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1 2 3 4 5 6 Page 1of 6 Fieldwork in geography is all about following an enquiry . A geographical enquiry is an active, questioning approach to learning. An enquiry is based on a question that you set out to answer.

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factors, eg a lack of rainfall make it difficult to grow sufficient food

factors, eg some countries have low levels of education, poor water quality or a lack of doctors

political factors, eg war or a corrupt government would hinder development

natural resources, eg some countries have an abundance of raw materials such as timber or oil

trade, eg (LICs) often rely on the export of low value primary products

Patterns of world trade

Trade involves the sale and purchase of goods, services or information:

are goods purchased from abroad and brought into a country

are goods purchased by other countries and sent to them

the is the difference between the money earned from exports and that spent on imports

Usually, (HICs) export valuable such as electronics and cars and import cheaper such as sugar and tea. In low-income countries the opposite is true. This means that low-income countries earn little and spend more, giving them a negative balance of trade. The countries are forced to borrow money to pay for imports and can go into debt.

The price of primary products fluctuates on the world market. Prices are set in HICs and producers in LICs lose out when the price drops. LICs are very dependent on the world-trade system yet they have little control over how it operates.

HICs control world trade through trade tariffs, subsidies and trade quotas:

are taxes imposed on imports. This can make imports more expensive than goods manufactured in the home country.

are limits on the amount of goods imported. This stops some countries exporting their goods to richer countries.

are a government policy to encourage the export of goods through direct payments, low-cost loans, tax relief or government-financed international advertising (which artificially make HIC goods more marketable).

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Factors influencing development and patterns of world trade - Globalisation - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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factors, eg a lack of rainfall make it difficult to grow sufficient food factors, eg some countries have low levels of education, poor water quality or a lack of doctors political factors, eg war or a corrupt government would hinder development natural resources, eg some countries have an abundance of

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Graphs are a useful way to show numerical data. There are a variety of graphs that can help highlight patterns and be used to reach conclusions. Choosing the right graph is very important.

Line graphs

A line graph could be used to show the changes in a country's employment structure over time. This graph shows that in the post-industrial era approximately 11% of employed people work in primary industries, 31% in secondary industries, 54% in tertiary industries and 4% work in quaternary industries. Note how the total adds up to 100%.

Bar charts show grouped data as rectangular bars, eg the number of visiting a resort each month. Divided bar charts split up each rectangular bar to break the information down further. A divided bar chart could be used to show the age breakdown of tourists visiting a resort.

are bar charts that show how many people of different ages are living in a place or country. Population pyramids show the bars arranged sideways, rather than upwards. The x-axis shows the number of people, the shows their ages. The bars on the left show the number of males and the bars on the right show the number of females.

Bar charts and line graphs can be combined. Climate graphs are an example of this. The x-axis shows the months of the year and there are two y-axes to show average temperature and total rainfall. The temperature is shown as a line and the rainfall as bars.

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Line graphs, bar charts, population pyramids and histograms - Graphical skills - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Graphs are a useful way to show numerical data. There are a variety of graphs that can help highlight patterns and be used to reach conclusions. Choosing the right graph is very important. A line graph could be used to show the changes in a country's employment structure over time.

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Global patterns of development - Globalisation - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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Learn about and revise globalisation and global patterns of development with GCSE Bitesize Geography (Eduqas).

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When the wind blows over the sea, it creates waves. The size and energy of the wave depends on certain factors:

There are two different types of waves - and . They can affect the coastline in different ways. When a wave reaches the shore, the water that rushes up the beach is known as the . The water that flows back towards the sea is known as the . The energy of the swash and backwash determine the type of wave.

Destructive waves

The characteristics of a destructive wave are:

occurs in stormy conditions, with strong winds

the strong backwash removes sediment from the beach

waves that are steep and close together

tall waves with short wave length

they arrive quickly and have a high frequency - a lot of them come in a short period of time

Constructive waves

The characteristics of a constructive wave are:

small waves, with low wave height and long wave length

occurs in calm conditions, without much wind

the strong swash brings sediments to build up the beach

the backwash is not strong enough to remove the sediment

waves that are low and further apart

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Wave types - constructive and destructive - Coastal processes - Eduqas - GCSE Geography Revision - Eduqas - BBC Bitesize

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When the wind blows over the sea, it creates waves. The size and energy of the wave depends on certain factors: There are two different types of waves - and . They can affect the coastline in different ways. When a wave reaches the shore, the water that rushes up the beach is known as the .

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Remember its in southern hemisphere!

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Rural depopulation 2012 exam

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2012 exam NB Starts with climate graph

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WJEC 2012 unit 2

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Coasts Exam practice from 2013 WJEC exam