SlideShare a Scribd company logo
1 of 41
Ideas How to use the revision cards:
- Colour code the cards to show how
confident you are with the topic
- Ask someone at home to test you
-Test yourself & highlight key words
- Annotate (label) the cards
- Re-write your own definitions
- ‘Look, cover, check’
- Draw a mind map to for some topics
- Expand on key words
- Read through cards
- Cut out cards & stick around a room
1

Extreme
Environments

Hot
Deserts

What are Hot
deserts like?

Features of hot deserts
Hot Deserts have many different features:
- They are all dry and arid
-They may have a sandy, rocky or stony surface.
- They have very little rainfall
-They are often a lot hotter during the day, than at
night
2

Extreme
Environments

Hot
Deserts

Why are these
Deserts so Hot?

Reason 1  Distance of Travel

Parallel rays
of sunshine

Deserts are hot because of their proximity to the equator. Ray B
has to travel further, through the atmosphere, dust & clouds,
therefore not as
much heat reaches
the poles. Whereas
Ray A has a
shorter distance to
travel – meaning
that it retains more
of the heat from
the sun.
3

Extreme
Environments

Hot
Deserts

Why are these
Deserts so Hot?

Reason 2  Angle of Suns rays

Parallel rays
of sunshine

Deserts are hot because of their proximity to the equator. The earth
is curved. This means that the energy from Ray B is spread/
dispersed over a
X
greater area – the
energy is less
intense. This is
shown by ‘X’ on the
picture.
Whereas the energy
Y
from Ray A is
concentrated on a
smaller area. This is
shown by ‘Y’ on the
Diagram.
4

Extreme
Environments

Hot
Deserts

Why do deserts
receive very little
rainfall?

To understand why deserts receive little
rain, we first need to know why rain occurs.
Rain only forms when moist air rises, cools and
condenses. Often this is by:
Convection current – The sun heats the earth, which heats
the air above it. The air becomes less dense, rises & then
condenses. E.g. Tropical Rainforests at the equator
Frontal Rain – Two air masses meet. One is less dense
than the other and is forced over the top of the other one.
Meaning that it rises, cools and then condenses. E.g. UK
Relief Rain. An air mass is forced over an area of high land.
The air rises, cools and condenses. E.g. in Hilly areas
Why do deserts
Hot
Extreme
receive very little
Environments Deserts rainfall?
In deserts, the air does not contain much
moisture & the air is usually falling meaning
that it cannot condense to produce rain.
Reasons why air falls:
Trade Winds - Due to suns heat, air rises at the
equator & falls near to the tropics (Cancer/Capricorn)
Rain Shadow - Air blows across a mountain. The
air then loses all of its moisture on the other side
Coastal Deserts - If the ocean is particularly
cold, then the air around the coast is cooled,
meaning that it will not rise & condense
5
How does wind
Hot
Extreme
affect how dry the
Environments Deserts desert is?
The prevailing (most common) wind direction
also plays a very important role in desert
climates. E.g. The Prevailing wind for the
Sahara desert in Africa
is from the North East.
This wind blows over
land, so is quite ‘dry air’
as it does not pick up
moisture from the sea.
The same is true for
other deserts.
6
7

Rain Shadow

The rain gets forced up
and over the (windward)
side of the mountain. As
the air rises, it cools
condenses. The
and
rain falls over
the mountains.
By the time the
clouds reach the
other (leeward)
side there is no
moisture left in
the air
8

Coastal Desert -Caused by cold Currents

Cold ocean currents affect the climate of the
coastal area. The colder sea cools down the land
Which means that
the air is cool and
not able to rise.
Sea fog can form
on the coast.
Some plants have
adapted so they
are able to use
Cold
the moisture from
Currents
the fog.
9

Rain &
clouds

TRADE WINDS

The sun is most powerful at the
equator. Here, the sun heats the
earth (A) and the air Rises = low
pressure system. As the air
rises, it cools and condenses
forming cloud (B) and rain
(C). This is why tropical
Rainforests have so much
rain. The air then moves
away from the equator.
Before it then falls. The air
then starts to fall at approx
300N (D) & 300S of the
equator (E). As it falls, it
warms up - the air can’t
then produce rain = High
Pressure system
10

Extreme
Environments

Hot
Desert

How have people
reacted to Hot Deserts
(media)

Hot deserts are depicted in a number of ways
through different types of media.
Accounts of historical expeditions The extremes of
deserts may be stressed, & meeting different cultures.
E.g. Across the empty quarter  Thesiger
Through films Lawrence of Arabia & the English
Patient.
Historical Newspaper articles  “Across the sahara
by caterpillar” The Observer Jan 14th 1923, by Major
Gordon Home &The Murder of Major Gordon Laing
Guardian August 2nd 1828
• http://www.youtube.com/watch?v=OxfZHP1HHHg
• http://www.youtube.com/watch?v=OlhLOWTnVoQ
• http://www.youtube.com/watch?v=lLaWj7d6PiE
• http://www.youtube.com/watch?v=t65VrYZ2U9s
11

Extreme
Environments

Hot
Desert

How have people
reacted to Hot Deserts
(media)

Through TV  Bear Grylls, Travel Programmes,
Michael Palin (Sahara and Pole to Pole)
Through Paintings ‘Pear Blossom Highway’
Hockney. ‘St John in the desert’ Veneziano
Each source of information will depict the desert in a
different way. Sometime they will focus on the
hardships of the desert and sometimes they will
focus upon the difficulties. The desert may be
portrayed much more positively - the mystical
quality/romance of the desert may be highlighted.
12

Extreme
Environments

Hot
Deserts

Where are hot deserts
found?

Hot deserts are found near to the tropic of Capricorn &
Cancer & Often between 150 - 300 N and South of the Equator
13

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Climate

There is a large Diurnal (daily) range in
temperatures in the desert.
Why are Deserts Hot
During the Day?

Why are Deserts Cold
at Night?

During the day, the
sun heats up the
ground. This is
because there are v.
few clouds to stop
the suns rays.

At night a lot of heat
escapes. This is
because there are v.
few clouds, which
means that the heat
can escape.
14

Extreme
Environments

Hot
Deserts

Why are Deserts Hot
During the Day?
15

Extreme
Environments

Hot
Deserts

Why are Deserts Cold
During the Night?
16

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Climate
You may be asked to
describe what these
graphs show. Refer
to: Highest, Lowest,
trends, anomalies.
Include Data,
months,
increases/decreases
seasons, links
between Rain/Temp
17

Extreme
Environments

Hot
Deserts

What are Hot Deserts
like?  Vegetation

For any vegetation to survive in a desert it must
adapt. The main challenge is the heat & lack of water
1) Xerophytes These plants have made physical adaption's to
survive the desert e.g. Cacti. Some of the features are:
- Spines – These deter predators and help to break up wind –

reducing the amount of transpiration of water moisture
-Shallow roots – these quickly draw up any surface rainwater.
-Deep roots – Reach towards deep underground water stores.
-‘pleated’ body – The cactus can swell up to take in water
-Green body – body takes on role of photosynthesis.
-Small surface area – to reduce transpiration
-Thick waxy body – the make sure no water is lost
18

Extreme
Environments

Hot
Deserts

What are Hot Deserts
like?  Vegetation

For any vegetation to survive in a desert it must
adapt. The main challenge is the heat & lack of water

2a) Ephemerals (plants)
These plants lie dormant for months, or even years in
the desert until it rains.
These plants grow & flower very quickly (within a few
days) before the water gets evaporated or soaked away.
2b) Ephemerals (seeds)
In deserts there are many seeds waiting to be
germinated. When the rains come they will quickly start
to grow into plants, taking advantage of the conditions
19

Extreme
Environments

Hot
Deserts

Xerophytes A sketch to
show key features of a cactus

What are Hot Deserts
like?  Vegetation

Ephemerals Desert
after a ‘rain’ event
20

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Animals

Animals need to adapt in order to survive in desert
environments.
They have to cope with extreme temperatures, lack
of food and lack of water.
To avoid daytime heat, many desert animals are
Nocturnal; they burrow beneath the surface or hide
in the shade during the day, emerging at night to
eat.
Many desert animals do not have to drink at all –
they get all of their water from the moisture in food
21

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Animals

How have camels adapted to life in deserts?
Thick fur & underwool –
warmth at night & insulation
against sun in day

Fat Stored in humps
- energy reserve

Concentrated urine
to retain as much
water as possible

Broad, flat leathery
pads on hooves to
spread out weight
on sand

Two rows of
eyelashes– protects
against sand & sun
Nostrils can be
closed to keep out
sand

Thick leathery
patches on knees to
protect when
resting on hot sand

Long, strong legs – carry
heavy loads & body
further away from sand
22

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Weathering &
Erosion

Weathering is the breaking up of rocks in the
place that they are found. For Example:
a) Physical Weathering. This includes Freeze-Thaw
Weathering (ice expanding in a crack, thaws, then refreezes) and exfoliation (sun heats layers of rock & they
break off like layers of an onion)
Freeze-Thaw
Weathering
Exfoliation /
onion skin
weathering
23

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Weathering &
Erosion

b) Chemical Weathering. This includes Salt Crystallisation
(water evaporates & leaves behind salt, which expands) and
Hydration (water reacts with chemical in the rock)
c) Biological Weathering. This is when plant roots grow into
crack in the rock and force the cracks open.
Erosion is the wearing away and removal of material.
In deserts erosion is mainly caused by the wind. Although
flash flooding can also happen & moves lose material.
Both occur as there is little vegetation hold /bind sand.
Deposition is the laying down of material that has
already been eroded. Material from wind erosion often
deposits is often laid down to form Dunes & flash floods
carry material further down the valley & across flood plains
24

Extreme
Environments

Hot
Deserts

Formation of Zeugen
 Stage 1
When there are alternating
layers of hard & soft rock
there can sometimes be
weaknesses in the joints.
When the temperature
changes and dew occurs
at night, chemical
weathering breaks up the
rock and starts to open up
the joints

What are hot deserts
like?  Physical
features – Zeugen 1
25

Extreme
Environments

Hot
Deserts

Formation of Zeugen
 Stage 2
Once the joints are
opened up, they are then
eroded away further by
the wind (abrasion).
This forms ridges and
hollows. At this stage
the erosion starts to
reach into the soft rock

What are hot deserts
like?  Physical
features – Zeugen 2
26

Extreme
Environments

Hot
Deserts

Formation of Zeugen
 Stage 3
The Zeugen can stand
between 3m – 36m high.
Now that abrasion starts
to erode the softer rock
(which is less resistant),
rock pedestals will often
form

What are hot deserts
like?  Physical
features – Zeugen 3
27

Extreme
Environments

Hot
Deserts

What are hot deserts
like? Physical Features
 Rock Pedestal

Rock Pedestal–These are sometimes called mushroom
rocks as they are often ‘top heavy’. Over time, the wind
(which carries particles of sand) wears away the rock. This
type of erosion is called abrasion. A rock pedestal erodes
more in places than others. This is because softer (less
Example of a Rock Pedestal Classic mushroom resistant) rock
shape at he top
erodes more quickly
More resistant rock than harder (more
worn away slowly
resistant) rock and
because much of
Less resistant rock
worn away quickly
the erosion takes
Most erosion within place within the first
first metre of ground
metre of the ground
as wind lifts material
28

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Physical
features – Yardang

Yardang: Formation

Key

Yardangs often form in alternate vertical bands
of hard and soft rocks. The weaker rocks are less
resistant and erode Stage 1 – flat surface
more quickly. The
harder rocks are
more resistant and Stage 2–Differential erosion due to abrasion
left as ridges.
Hard, Resistant Rock

Softer, less resistant rock
29

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Physical
features – Yardang

Yardang: Formation Stage 3 – Ridges become more pronounced
Yardangs are long and
thin in appearance. The
ridges become more
pronounced. Can be up
Cross section view
to 15m high
They also often occur
parallel to the prevailing
(most common) wind
direction, this is when
most erosion will occur.
Diagram is plan view
30

Extreme
Environments

Hot
Deserts

What are hot deserts
like?  Physical
features – Wadi

A Wadi is a steep sided, deep, flat floored (dry) valley in
a desert. Usually they do not have any water in them.
There may be a few desert plants in the Wadi.
The material in the wadi is
often loose. Therefore,
when there is a flash
flood, lots of material in
the wadi is transported
(moved) & then deposited
(dropped) further down
the valley.

Steep
Sides

Loose
Material

Flat
bottom

Some
plants
31

Extreme
Environments

Hot
Deserts

What are hot deserts
like? Physical features
Barchan Dunes

There are lots of different types of Sand Dune. They will
differ according to the strength/direction of the wind, amount
of vegetation, amount and type of sand. As the sand is loose,
many types of sand dunes will migrate (move), due to the
wind. Sand dunes mostly form when there is an obstacle –
the sand builds around the obstacle – e.g. vegetation.
Sand
deposited

Prevailing
Wind

150

Cross
section
32

Extreme
Environments

Hot
Deserts

What are hot deserts
like? Physical features
Barchan Dunes

A Barchan Dune has a particular shape. It is a crescent
shape with ‘horns’ pointing downwind. The upwind slope is
approx 340 & the downwind slope is approx 150. Barchan
dunes occur where there’s a limited supply of sand, therefore
they may by up to 100m
apart. They form around
an obstruction. The
obstruction causes the
wind to lose speed &
then deposits, which
causes a greater
obstruction & more
material is deposited.
They will move over time
33

Extreme
Environments

Hot
Deserts

How do people use
hot deserts?
Oil and Gas

General  Beneath the Sahara are layers of
sedimentary rock. Oil and gas is trapped
beneath after is was formed from the remains
of microscopic organisms millions of years ago.

Oilfield
drilling
rig

Positives  Exporting oil and gas can make
a lot of money for countries.

Negatives  The money isn’t distributed
equally in the country & companies are often
owned by overseas companies.
It is very expensive to find oil and gas. Many of the larger, easy to
find oil wells have now been used up. Transport oil and gas
through pipelines is very expensive. Oil & gas are non-renewable
resources – one day they’ll run out & burning these releases CO 2.
34

Extreme
Environments

Hot
Deserts

How do people use
hot deserts?
Tourism

Tourism Many people find deserts to be
fascinating and like the idea of visiting a
desert. There are many tour companies
that offer desert holidays, catering for
different experiences – e.g. self drive,
buggies, Bedouin tents/camel treks.
Positives People are able to find out about different cultures.
Some money from tourism will go to locals.
Negatives Some areas may have delicate environments which
could be damaged by tourism. Some tours companies are foreign
owned, meaning that not all money goes to the locals.
35

Extreme
Environments

Hot
Deserts

How do people use
hot deserts?
Agriculture

In deserts, there is lots of flat, cheap land
which makes it ideal for agriculture. Of
course, water is needed for crops to grow.
This can either come from irrigation
channels which take water from rivers, or
from well which takes water from underground aquifers (water holding rocks).
Positives – allows greater areas of desert
to be used. Creates employment.
Negatives – River levels affects, aquifers
will run out of water. Lots of chemicals are
needed to feed the plants, as desert
sand/soil has v few nutrients.

Desert

Agriculture

Irrigation channel
Water pumped
up from aquifer
36

Extreme
Environments

Hot
Deserts

How do people use
Hot Deserts?

The Bedouin The Bedouin are pastoral (raise
Lighting a
fire
animals) nomads (they move around from place to
place. They overcome problems in the following ways:
Water – They plan routes from water source to
another. Also, use other indicators such as lines of
plants and insects to find hidden underground water.
Transport – Bedouins traditionally use camels as
transport as they are able to carry large loads.
Clothing - They traditionally wear woollen, loose fitting clothes, from
their animals. These insulate against the heat of the day & provide
warmth at night. Covering their bodies means that the amount of
sweating is reduced, therefore reducing dehydration.
Shelter–They need to be able to carry their shelter with them & pack
up quickly. Their tents are made from Goat hair cloth as it is warm &
waterproof. They are long/narrow allowing breeze to blow
37

Extreme
Environments

Hot
Deserts

Desertification
This is the process by which land turns
into desert. After a ‘dry period’ land will
often recover. Desertification is when
the land is so damaged that it can’t
recover.
The damage can be caused by
physical (Natural) processes, or by
Human (due to people) processes
One of the areas at risk of
desertification is the Sahel, in Africa. It
is on the southern edge of the Sahara.
It is an area where some farming
occurs & is mainly grassland

What Challenged do
hot deserts pose?
Desertification 1
Extreme
Environments
38

Hot
Deserts

What Challenged do
hot deserts pose?
Desertification 2

Desertification - Physical Causes:
Less Rainfall – Overall, there has been a reduction in the
amount of rain for the Sahel over the last few years
Less Reliable Rainfall – Also, the rain is less reliable – it may
be many years before its rains properly in an area
Higher Temps–This increases the amount of moisture/water
lots through evaporation & transpiration (water from plants)
Desertification - Human Causes:
Irrigation–water for growing crops is quickly evaporated, salt in
the water is left on the ground=unsuitable for future farming
 Over grazing – Herds of animals eat lots of vegetation. Too
many animals means that the vegetation cannot recover
Over farming – Soil can’t recover from lots of farming. It loses
it nutrients and loss of vegetation means that it blows away.
More people - Many people in the Sahel use firewood. More
people means too much may be collected-plants cannot recover.
39

Extreme
Environments

Hot
Deserts

What Challenged do
hot deserts pose?

Some of the other challenges that Hot Deserts Pose:
Drought – This is caused by lack of water of a long
period of times causes drought - Crops may fail.
Famine – This is caused by drought. Large numbers
of people are not able to access food/water.
Cultures – Over time, cultures change. The Bedouin
for example, find it more and more difficult to maintain
their traditional way of life. Many cultures have dies out.
This is sometimes due to desertification, they are not
enough resources to support the Bedouin.

More Related Content

What's hot

Glacial landforms AS Level Geography
Glacial landforms AS Level GeographyGlacial landforms AS Level Geography
Glacial landforms AS Level Geography
Katie-Ann Sheehan
 
Coastal Processes And Landforms
Coastal Processes And LandformsCoastal Processes And Landforms
Coastal Processes And Landforms
Malia Damit
 
Coastal Landforms
Coastal  LandformsCoastal  Landforms
Coastal Landforms
whiskeyhj
 

What's hot (20)

Glaciers
GlaciersGlaciers
Glaciers
 
Glaciers
GlaciersGlaciers
Glaciers
 
Glacial landforms AS Level Geography
Glacial landforms AS Level GeographyGlacial landforms AS Level Geography
Glacial landforms AS Level Geography
 
Coastal Processes And Landforms
Coastal Processes And LandformsCoastal Processes And Landforms
Coastal Processes And Landforms
 
King's model-Geomorhology Chapter
King's model-Geomorhology ChapterKing's model-Geomorhology Chapter
King's model-Geomorhology Chapter
 
Theory of isostacy
Theory of isostacyTheory of isostacy
Theory of isostacy
 
Arid Aeolian Landform
Arid Aeolian LandformArid Aeolian Landform
Arid Aeolian Landform
 
GEOGRAPHY YEAR 10: RIVER LANDFORMS
GEOGRAPHY YEAR 10: RIVER LANDFORMSGEOGRAPHY YEAR 10: RIVER LANDFORMS
GEOGRAPHY YEAR 10: RIVER LANDFORMS
 
Erosional & depositional glacial landforms
Erosional & depositional glacial landformsErosional & depositional glacial landforms
Erosional & depositional glacial landforms
 
JET STREAMS.pptx
JET STREAMS.pptxJET STREAMS.pptx
JET STREAMS.pptx
 
Fundmetal concepts of geomorphology
Fundmetal concepts of geomorphologyFundmetal concepts of geomorphology
Fundmetal concepts of geomorphology
 
Mass Movement
Mass MovementMass Movement
Mass Movement
 
Types of Rainfall
Types of RainfallTypes of Rainfall
Types of Rainfall
 
Coastal Landforms
Coastal  LandformsCoastal  Landforms
Coastal Landforms
 
Air masses and its types
Air masses and its typesAir masses and its types
Air masses and its types
 
What are periglacial processes?
What are periglacial processes?What are periglacial processes?
What are periglacial processes?
 
Types of Rivers
Types of RiversTypes of Rivers
Types of Rivers
 
Geomorpholgy: NATURE AND SCOPE
Geomorpholgy: NATURE AND SCOPEGeomorpholgy: NATURE AND SCOPE
Geomorpholgy: NATURE AND SCOPE
 
Fundamental concepts of geomorphology
Fundamental concepts of geomorphologyFundamental concepts of geomorphology
Fundamental concepts of geomorphology
 
Periglacial landforms-processes, formation
Periglacial landforms-processes, formationPeriglacial landforms-processes, formation
Periglacial landforms-processes, formation
 

Similar to Deserts

Resource 6 Introuding Water Matters
Resource 6    Introuding Water MattersResource 6    Introuding Water Matters
Resource 6 Introuding Water Matters
teacherlizz
 
ELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptx
ELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptxELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptx
ELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptx
BryanBangiban1
 
How do ecosystems compare
How do ecosystems compareHow do ecosystems compare
How do ecosystems compare
bassantnour
 

Similar to Deserts (20)

Deserts
DesertsDeserts
Deserts
 
Desert Biomes
Desert BiomesDesert Biomes
Desert Biomes
 
Climate SG Key
Climate SG KeyClimate SG Key
Climate SG Key
 
Sub tropical deserts
Sub tropical deserts Sub tropical deserts
Sub tropical deserts
 
The great epic
The great epicThe great epic
The great epic
 
E learning geography project by Julian Sammut, 3.02
E learning geography project by Julian Sammut, 3.02E learning geography project by Julian Sammut, 3.02
E learning geography project by Julian Sammut, 3.02
 
Blue planet General science for education.pptx
Blue planet General science for education.pptxBlue planet General science for education.pptx
Blue planet General science for education.pptx
 
Antartica by judy flores
Antartica by judy floresAntartica by judy flores
Antartica by judy flores
 
Resource 6 Introuding Water Matters
Resource 6    Introuding Water MattersResource 6    Introuding Water Matters
Resource 6 Introuding Water Matters
 
Desert
DesertDesert
Desert
 
Climate
ClimateClimate
Climate
 
Climate
ClimateClimate
Climate
 
ELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptx
ELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptxELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptx
ELEMENTS OF WEATHER CLIMATE quarter 4 week 3 DAY 1-DAY 4.pptx
 
How do ecosystems compare
How do ecosystems compareHow do ecosystems compare
How do ecosystems compare
 
Chapter 2
Chapter 2Chapter 2
Chapter 2
 
Deserts
DesertsDeserts
Deserts
 
Lesson 15-2 of biology book
Lesson 15-2 of biology bookLesson 15-2 of biology book
Lesson 15-2 of biology book
 
Desert biome
Desert biomeDesert biome
Desert biome
 
Secondary Three Geography: Elements-temperature
Secondary Three Geography: Elements-temperatureSecondary Three Geography: Elements-temperature
Secondary Three Geography: Elements-temperature
 
Deserts
DesertsDeserts
Deserts
 

Recently uploaded

Making and Justifying Mathematical Decisions.pdf
Making and Justifying Mathematical Decisions.pdfMaking and Justifying Mathematical Decisions.pdf
Making and Justifying Mathematical Decisions.pdf
Chris Hunter
 
Seal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptxSeal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptx
negromaestrong
 
Gardella_Mateo_IntellectualProperty.pdf.
Gardella_Mateo_IntellectualProperty.pdf.Gardella_Mateo_IntellectualProperty.pdf.
Gardella_Mateo_IntellectualProperty.pdf.
MateoGardella
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
kauryashika82
 

Recently uploaded (20)

Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impact
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The Basics
 
ICT Role in 21st Century Education & its Challenges.pptx
ICT Role in 21st Century Education & its Challenges.pptxICT Role in 21st Century Education & its Challenges.pptx
ICT Role in 21st Century Education & its Challenges.pptx
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and Mode
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot Graph
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptx
 
Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17
 
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
 
Making and Justifying Mathematical Decisions.pdf
Making and Justifying Mathematical Decisions.pdfMaking and Justifying Mathematical Decisions.pdf
Making and Justifying Mathematical Decisions.pdf
 
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
 
Basic Civil Engineering first year Notes- Chapter 4 Building.pptx
Basic Civil Engineering first year Notes- Chapter 4 Building.pptxBasic Civil Engineering first year Notes- Chapter 4 Building.pptx
Basic Civil Engineering first year Notes- Chapter 4 Building.pptx
 
Mehran University Newsletter Vol-X, Issue-I, 2024
Mehran University Newsletter Vol-X, Issue-I, 2024Mehran University Newsletter Vol-X, Issue-I, 2024
Mehran University Newsletter Vol-X, Issue-I, 2024
 
Seal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptxSeal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptx
 
Gardella_Mateo_IntellectualProperty.pdf.
Gardella_Mateo_IntellectualProperty.pdf.Gardella_Mateo_IntellectualProperty.pdf.
Gardella_Mateo_IntellectualProperty.pdf.
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
 
Class 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdfClass 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdf
 
APM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across SectorsAPM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across Sectors
 
SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...
SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...
SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...
 
Advance Mobile Application Development class 07
Advance Mobile Application Development class 07Advance Mobile Application Development class 07
Advance Mobile Application Development class 07
 
psychiatric nursing HISTORY COLLECTION .docx
psychiatric  nursing HISTORY  COLLECTION  .docxpsychiatric  nursing HISTORY  COLLECTION  .docx
psychiatric nursing HISTORY COLLECTION .docx
 

Deserts

  • 1. Ideas How to use the revision cards: - Colour code the cards to show how confident you are with the topic - Ask someone at home to test you -Test yourself & highlight key words - Annotate (label) the cards - Re-write your own definitions - ‘Look, cover, check’ - Draw a mind map to for some topics - Expand on key words - Read through cards - Cut out cards & stick around a room
  • 2. 1 Extreme Environments Hot Deserts What are Hot deserts like? Features of hot deserts Hot Deserts have many different features: - They are all dry and arid -They may have a sandy, rocky or stony surface. - They have very little rainfall -They are often a lot hotter during the day, than at night
  • 3. 2 Extreme Environments Hot Deserts Why are these Deserts so Hot? Reason 1  Distance of Travel Parallel rays of sunshine Deserts are hot because of their proximity to the equator. Ray B has to travel further, through the atmosphere, dust & clouds, therefore not as much heat reaches the poles. Whereas Ray A has a shorter distance to travel – meaning that it retains more of the heat from the sun.
  • 4. 3 Extreme Environments Hot Deserts Why are these Deserts so Hot? Reason 2  Angle of Suns rays Parallel rays of sunshine Deserts are hot because of their proximity to the equator. The earth is curved. This means that the energy from Ray B is spread/ dispersed over a X greater area – the energy is less intense. This is shown by ‘X’ on the picture. Whereas the energy Y from Ray A is concentrated on a smaller area. This is shown by ‘Y’ on the Diagram.
  • 5. 4 Extreme Environments Hot Deserts Why do deserts receive very little rainfall? To understand why deserts receive little rain, we first need to know why rain occurs. Rain only forms when moist air rises, cools and condenses. Often this is by: Convection current – The sun heats the earth, which heats the air above it. The air becomes less dense, rises & then condenses. E.g. Tropical Rainforests at the equator Frontal Rain – Two air masses meet. One is less dense than the other and is forced over the top of the other one. Meaning that it rises, cools and then condenses. E.g. UK Relief Rain. An air mass is forced over an area of high land. The air rises, cools and condenses. E.g. in Hilly areas
  • 6. Why do deserts Hot Extreme receive very little Environments Deserts rainfall? In deserts, the air does not contain much moisture & the air is usually falling meaning that it cannot condense to produce rain. Reasons why air falls: Trade Winds - Due to suns heat, air rises at the equator & falls near to the tropics (Cancer/Capricorn) Rain Shadow - Air blows across a mountain. The air then loses all of its moisture on the other side Coastal Deserts - If the ocean is particularly cold, then the air around the coast is cooled, meaning that it will not rise & condense 5
  • 7. How does wind Hot Extreme affect how dry the Environments Deserts desert is? The prevailing (most common) wind direction also plays a very important role in desert climates. E.g. The Prevailing wind for the Sahara desert in Africa is from the North East. This wind blows over land, so is quite ‘dry air’ as it does not pick up moisture from the sea. The same is true for other deserts. 6
  • 8. 7 Rain Shadow The rain gets forced up and over the (windward) side of the mountain. As the air rises, it cools condenses. The and rain falls over the mountains. By the time the clouds reach the other (leeward) side there is no moisture left in the air
  • 9. 8 Coastal Desert -Caused by cold Currents Cold ocean currents affect the climate of the coastal area. The colder sea cools down the land Which means that the air is cool and not able to rise. Sea fog can form on the coast. Some plants have adapted so they are able to use Cold the moisture from Currents the fog.
  • 10. 9 Rain & clouds TRADE WINDS The sun is most powerful at the equator. Here, the sun heats the earth (A) and the air Rises = low pressure system. As the air rises, it cools and condenses forming cloud (B) and rain (C). This is why tropical Rainforests have so much rain. The air then moves away from the equator. Before it then falls. The air then starts to fall at approx 300N (D) & 300S of the equator (E). As it falls, it warms up - the air can’t then produce rain = High Pressure system
  • 11. 10 Extreme Environments Hot Desert How have people reacted to Hot Deserts (media) Hot deserts are depicted in a number of ways through different types of media. Accounts of historical expeditions The extremes of deserts may be stressed, & meeting different cultures. E.g. Across the empty quarter  Thesiger Through films Lawrence of Arabia & the English Patient. Historical Newspaper articles  “Across the sahara by caterpillar” The Observer Jan 14th 1923, by Major Gordon Home &The Murder of Major Gordon Laing Guardian August 2nd 1828
  • 12. • http://www.youtube.com/watch?v=OxfZHP1HHHg • http://www.youtube.com/watch?v=OlhLOWTnVoQ • http://www.youtube.com/watch?v=lLaWj7d6PiE • http://www.youtube.com/watch?v=t65VrYZ2U9s
  • 13. 11 Extreme Environments Hot Desert How have people reacted to Hot Deserts (media) Through TV  Bear Grylls, Travel Programmes, Michael Palin (Sahara and Pole to Pole) Through Paintings ‘Pear Blossom Highway’ Hockney. ‘St John in the desert’ Veneziano Each source of information will depict the desert in a different way. Sometime they will focus on the hardships of the desert and sometimes they will focus upon the difficulties. The desert may be portrayed much more positively - the mystical quality/romance of the desert may be highlighted.
  • 14. 12 Extreme Environments Hot Deserts Where are hot deserts found? Hot deserts are found near to the tropic of Capricorn & Cancer & Often between 150 - 300 N and South of the Equator
  • 15. 13 Extreme Environments Hot Deserts What are hot deserts like?  Climate There is a large Diurnal (daily) range in temperatures in the desert. Why are Deserts Hot During the Day? Why are Deserts Cold at Night? During the day, the sun heats up the ground. This is because there are v. few clouds to stop the suns rays. At night a lot of heat escapes. This is because there are v. few clouds, which means that the heat can escape.
  • 18. 16 Extreme Environments Hot Deserts What are hot deserts like?  Climate You may be asked to describe what these graphs show. Refer to: Highest, Lowest, trends, anomalies. Include Data, months, increases/decreases seasons, links between Rain/Temp
  • 19. 17 Extreme Environments Hot Deserts What are Hot Deserts like?  Vegetation For any vegetation to survive in a desert it must adapt. The main challenge is the heat & lack of water 1) Xerophytes These plants have made physical adaption's to survive the desert e.g. Cacti. Some of the features are: - Spines – These deter predators and help to break up wind – reducing the amount of transpiration of water moisture -Shallow roots – these quickly draw up any surface rainwater. -Deep roots – Reach towards deep underground water stores. -‘pleated’ body – The cactus can swell up to take in water -Green body – body takes on role of photosynthesis. -Small surface area – to reduce transpiration -Thick waxy body – the make sure no water is lost
  • 20. 18 Extreme Environments Hot Deserts What are Hot Deserts like?  Vegetation For any vegetation to survive in a desert it must adapt. The main challenge is the heat & lack of water 2a) Ephemerals (plants) These plants lie dormant for months, or even years in the desert until it rains. These plants grow & flower very quickly (within a few days) before the water gets evaporated or soaked away. 2b) Ephemerals (seeds) In deserts there are many seeds waiting to be germinated. When the rains come they will quickly start to grow into plants, taking advantage of the conditions
  • 21. 19 Extreme Environments Hot Deserts Xerophytes A sketch to show key features of a cactus What are Hot Deserts like?  Vegetation Ephemerals Desert after a ‘rain’ event
  • 22. 20 Extreme Environments Hot Deserts What are hot deserts like?  Animals Animals need to adapt in order to survive in desert environments. They have to cope with extreme temperatures, lack of food and lack of water. To avoid daytime heat, many desert animals are Nocturnal; they burrow beneath the surface or hide in the shade during the day, emerging at night to eat. Many desert animals do not have to drink at all – they get all of their water from the moisture in food
  • 23. 21 Extreme Environments Hot Deserts What are hot deserts like?  Animals How have camels adapted to life in deserts? Thick fur & underwool – warmth at night & insulation against sun in day Fat Stored in humps - energy reserve Concentrated urine to retain as much water as possible Broad, flat leathery pads on hooves to spread out weight on sand Two rows of eyelashes– protects against sand & sun Nostrils can be closed to keep out sand Thick leathery patches on knees to protect when resting on hot sand Long, strong legs – carry heavy loads & body further away from sand
  • 24. 22 Extreme Environments Hot Deserts What are hot deserts like?  Weathering & Erosion Weathering is the breaking up of rocks in the place that they are found. For Example: a) Physical Weathering. This includes Freeze-Thaw Weathering (ice expanding in a crack, thaws, then refreezes) and exfoliation (sun heats layers of rock & they break off like layers of an onion) Freeze-Thaw Weathering Exfoliation / onion skin weathering
  • 25. 23 Extreme Environments Hot Deserts What are hot deserts like?  Weathering & Erosion b) Chemical Weathering. This includes Salt Crystallisation (water evaporates & leaves behind salt, which expands) and Hydration (water reacts with chemical in the rock) c) Biological Weathering. This is when plant roots grow into crack in the rock and force the cracks open. Erosion is the wearing away and removal of material. In deserts erosion is mainly caused by the wind. Although flash flooding can also happen & moves lose material. Both occur as there is little vegetation hold /bind sand. Deposition is the laying down of material that has already been eroded. Material from wind erosion often deposits is often laid down to form Dunes & flash floods carry material further down the valley & across flood plains
  • 26. 24 Extreme Environments Hot Deserts Formation of Zeugen  Stage 1 When there are alternating layers of hard & soft rock there can sometimes be weaknesses in the joints. When the temperature changes and dew occurs at night, chemical weathering breaks up the rock and starts to open up the joints What are hot deserts like?  Physical features – Zeugen 1
  • 27. 25 Extreme Environments Hot Deserts Formation of Zeugen  Stage 2 Once the joints are opened up, they are then eroded away further by the wind (abrasion). This forms ridges and hollows. At this stage the erosion starts to reach into the soft rock What are hot deserts like?  Physical features – Zeugen 2
  • 28. 26 Extreme Environments Hot Deserts Formation of Zeugen  Stage 3 The Zeugen can stand between 3m – 36m high. Now that abrasion starts to erode the softer rock (which is less resistant), rock pedestals will often form What are hot deserts like?  Physical features – Zeugen 3
  • 29. 27 Extreme Environments Hot Deserts What are hot deserts like? Physical Features  Rock Pedestal Rock Pedestal–These are sometimes called mushroom rocks as they are often ‘top heavy’. Over time, the wind (which carries particles of sand) wears away the rock. This type of erosion is called abrasion. A rock pedestal erodes more in places than others. This is because softer (less Example of a Rock Pedestal Classic mushroom resistant) rock shape at he top erodes more quickly More resistant rock than harder (more worn away slowly resistant) rock and because much of Less resistant rock worn away quickly the erosion takes Most erosion within place within the first first metre of ground metre of the ground as wind lifts material
  • 30. 28 Extreme Environments Hot Deserts What are hot deserts like?  Physical features – Yardang Yardang: Formation Key Yardangs often form in alternate vertical bands of hard and soft rocks. The weaker rocks are less resistant and erode Stage 1 – flat surface more quickly. The harder rocks are more resistant and Stage 2–Differential erosion due to abrasion left as ridges. Hard, Resistant Rock Softer, less resistant rock
  • 31. 29 Extreme Environments Hot Deserts What are hot deserts like?  Physical features – Yardang Yardang: Formation Stage 3 – Ridges become more pronounced Yardangs are long and thin in appearance. The ridges become more pronounced. Can be up Cross section view to 15m high They also often occur parallel to the prevailing (most common) wind direction, this is when most erosion will occur. Diagram is plan view
  • 32. 30 Extreme Environments Hot Deserts What are hot deserts like?  Physical features – Wadi A Wadi is a steep sided, deep, flat floored (dry) valley in a desert. Usually they do not have any water in them. There may be a few desert plants in the Wadi. The material in the wadi is often loose. Therefore, when there is a flash flood, lots of material in the wadi is transported (moved) & then deposited (dropped) further down the valley. Steep Sides Loose Material Flat bottom Some plants
  • 33. 31 Extreme Environments Hot Deserts What are hot deserts like? Physical features Barchan Dunes There are lots of different types of Sand Dune. They will differ according to the strength/direction of the wind, amount of vegetation, amount and type of sand. As the sand is loose, many types of sand dunes will migrate (move), due to the wind. Sand dunes mostly form when there is an obstacle – the sand builds around the obstacle – e.g. vegetation. Sand deposited Prevailing Wind 150 Cross section
  • 34. 32 Extreme Environments Hot Deserts What are hot deserts like? Physical features Barchan Dunes A Barchan Dune has a particular shape. It is a crescent shape with ‘horns’ pointing downwind. The upwind slope is approx 340 & the downwind slope is approx 150. Barchan dunes occur where there’s a limited supply of sand, therefore they may by up to 100m apart. They form around an obstruction. The obstruction causes the wind to lose speed & then deposits, which causes a greater obstruction & more material is deposited. They will move over time
  • 35. 33 Extreme Environments Hot Deserts How do people use hot deserts? Oil and Gas General  Beneath the Sahara are layers of sedimentary rock. Oil and gas is trapped beneath after is was formed from the remains of microscopic organisms millions of years ago. Oilfield drilling rig Positives  Exporting oil and gas can make a lot of money for countries. Negatives  The money isn’t distributed equally in the country & companies are often owned by overseas companies. It is very expensive to find oil and gas. Many of the larger, easy to find oil wells have now been used up. Transport oil and gas through pipelines is very expensive. Oil & gas are non-renewable resources – one day they’ll run out & burning these releases CO 2.
  • 36. 34 Extreme Environments Hot Deserts How do people use hot deserts? Tourism Tourism Many people find deserts to be fascinating and like the idea of visiting a desert. There are many tour companies that offer desert holidays, catering for different experiences – e.g. self drive, buggies, Bedouin tents/camel treks. Positives People are able to find out about different cultures. Some money from tourism will go to locals. Negatives Some areas may have delicate environments which could be damaged by tourism. Some tours companies are foreign owned, meaning that not all money goes to the locals.
  • 37. 35 Extreme Environments Hot Deserts How do people use hot deserts? Agriculture In deserts, there is lots of flat, cheap land which makes it ideal for agriculture. Of course, water is needed for crops to grow. This can either come from irrigation channels which take water from rivers, or from well which takes water from underground aquifers (water holding rocks). Positives – allows greater areas of desert to be used. Creates employment. Negatives – River levels affects, aquifers will run out of water. Lots of chemicals are needed to feed the plants, as desert sand/soil has v few nutrients. Desert Agriculture Irrigation channel Water pumped up from aquifer
  • 38. 36 Extreme Environments Hot Deserts How do people use Hot Deserts? The Bedouin The Bedouin are pastoral (raise Lighting a fire animals) nomads (they move around from place to place. They overcome problems in the following ways: Water – They plan routes from water source to another. Also, use other indicators such as lines of plants and insects to find hidden underground water. Transport – Bedouins traditionally use camels as transport as they are able to carry large loads. Clothing - They traditionally wear woollen, loose fitting clothes, from their animals. These insulate against the heat of the day & provide warmth at night. Covering their bodies means that the amount of sweating is reduced, therefore reducing dehydration. Shelter–They need to be able to carry their shelter with them & pack up quickly. Their tents are made from Goat hair cloth as it is warm & waterproof. They are long/narrow allowing breeze to blow
  • 39. 37 Extreme Environments Hot Deserts Desertification This is the process by which land turns into desert. After a ‘dry period’ land will often recover. Desertification is when the land is so damaged that it can’t recover. The damage can be caused by physical (Natural) processes, or by Human (due to people) processes One of the areas at risk of desertification is the Sahel, in Africa. It is on the southern edge of the Sahara. It is an area where some farming occurs & is mainly grassland What Challenged do hot deserts pose? Desertification 1
  • 40. Extreme Environments 38 Hot Deserts What Challenged do hot deserts pose? Desertification 2 Desertification - Physical Causes: Less Rainfall – Overall, there has been a reduction in the amount of rain for the Sahel over the last few years Less Reliable Rainfall – Also, the rain is less reliable – it may be many years before its rains properly in an area Higher Temps–This increases the amount of moisture/water lots through evaporation & transpiration (water from plants) Desertification - Human Causes: Irrigation–water for growing crops is quickly evaporated, salt in the water is left on the ground=unsuitable for future farming  Over grazing – Herds of animals eat lots of vegetation. Too many animals means that the vegetation cannot recover Over farming – Soil can’t recover from lots of farming. It loses it nutrients and loss of vegetation means that it blows away. More people - Many people in the Sahel use firewood. More people means too much may be collected-plants cannot recover.
  • 41. 39 Extreme Environments Hot Deserts What Challenged do hot deserts pose? Some of the other challenges that Hot Deserts Pose: Drought – This is caused by lack of water of a long period of times causes drought - Crops may fail. Famine – This is caused by drought. Large numbers of people are not able to access food/water. Cultures – Over time, cultures change. The Bedouin for example, find it more and more difficult to maintain their traditional way of life. Many cultures have dies out. This is sometimes due to desertification, they are not enough resources to support the Bedouin.