CH5.1-2 recap

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Slide 1: Slide
GeographyMiddelbare schoolhavo, vwoLeerjaar 2

This lesson contains 40 slides, with interactive quizzes, text slides and 1 video.

time-iconLesson duration is: 60 min

Items in this lesson

Welcome
Learning goals
Recap
Questions
Learning

Slide 1 - Slide

Learning goals
− You know which forms of weathering there are.
− You understand how ice, plant roots and changes in temperature cause weathering.
− You know the types of weathered material are and how they differ in size.
− You understand how the transport of weathered material can cause erosion.

Slide 2 - Slide

Learning goals

− You know in which ways weathered material can be moved.
− You understand why a river is better at sorting weathered material than a glacier, and the wind can do it even better.
− You understand why there is much sediment at the end of a glacier.

Slide 3 - Slide

Weathering is the break down of hard rock. The two types are ...... and ........ weathering
A
physical - eroded
B
physical - mechanical
C
chemical - non chemical
D
mechanical - chemical

Slide 4 - Quiz

Circumstances in which chemical weathering occurs
A
hot and humid climate
B
large temperature amplitude
C
hot and dry climate
D
Extremely cold winters

Slide 5 - Quiz

Circumstances in which mechanical weathering may occur.
A
Mediterranean climate
B
Hot and humid climate
C
Extreme temperature differences
D
A moderate maritime climate

Slide 6 - Quiz

Middle reaches
Higher reaches 
Lower reaches 
Sand 
Clay
Rocks
Gravel
Erosion
Weathering
Sedimentation

Slide 7 - Drag question

what is the difference between a U-valley and V-valley?

Slide 8 - Mind map

Sleep het juiste begrip naar de juiste afbeelding
Chemical weathering
Oxidation
Temperature fluctuations 
Mechanical weathering: Frost
Mechanical weathering

Slide 9 - Drag question

Weathered material
The river brings material from the higher reaches to the middle and lower reaches. 
This material decreases in size the further you go.

Boulders, rocks, gravel, sand, clay. 

Slide 10 - Slide

Erosion
Rivers grind away the landscape. The weathered material in rivers bumbs into the sides and scrapes the sides away, like sandpaper does.

Slide 11 - Slide

Erosion
Erosion
Erosion
Sedimentation
Sedimentation
Sedimentation

Slide 12 - Drag question

Slide 13 - Video

Explain in your own words the difference between Erosion and weathering

Slide 14 - Open question

Erosion
Weathering

Slide 15 - Drag question

Weathering
Erosion
Sedimentation

Slide 16 - Drag question

Erosion can happen without weathering
A
yes
B
no

Slide 17 - Quiz

Weathering can happen without erosion
A
yes
B
no

Slide 18 - Quiz

Weathering due to water freezing in the cracks of the stone is called
A
biological weathering
B
frost weathering
C
chemical weathering
D
weathering due to the temperature of stone

Slide 19 - Quiz

Make the correct combinations:
Erosion
Transportation
Deposition
The glacier makes a U-shaped valley
The glacier brought rocks from Scandinavia to The Netherlands
The glacier picks up rocks
The glacier melts and leaves rocks behind
Rocks in the glacier scrapes away rocks below the glacier
The glacier moves and there are rocks inside the glacier

Slide 20 - Drag question

The water flow is the fastest in
A
the upper course
B
the middle course
C
the lower course

Slide 21 - Quiz

Sedimentation of sand is happening in the
A
upper course
B
middle course
C
lower course

Slide 22 - Quiz

Erosion because of a glacier forms a
A
U-valley
B
V-valley
C
Meanders

Slide 23 - Quiz

Slide 24 - Slide

Slide 25 - Slide

Slide 26 - Slide

Slide 27 - Slide

Slide 28 - Slide

Mechenical weathering
chemical weathering
Cold climates
warm climates
Lots of precipitation needed
some precipitation is enough
Closer to the poles
closer to the equator

Slide 29 - Drag question

Erosion
Weathering

Slide 30 - Drag question

Chemical weathering
Mechanical weathering

Slide 31 - Drag question

This picture is taken in Canada. Explain how this landscape is formed. Use the words 'erosion' and 'weathering'.

Slide 32 - Open question

2 hoofdsoorten verwering.
Elke hoofdsoort kent weer verschillende voorbeelden.
Chemische verwering

Het gesteente valt uit elkaar doordat de chemische structuur verandert.

Waardoor: 
- Oplossen van gesteenten in zuur (grond/regen)water
Fysische verwering
(mechanische verwering)

Het gesteente valt uit elkaar, maar behoudt de zelfde structuur.

Waardoor:
- grote temperatuurverschillen,
- vorst
- wortels van planten
- plotseling drukverschil

Slide 33 - Slide

Erosion
Weathering
Sedimentation

Slide 34 - Drag question

Weathering and mountains
In combination with erosion
Young mountain
Old mountain
Example
Alps
Jura
Height
High
Low
Top
Pointy
Flat
Hills
High
Flat

Slide 35 - Slide


A
Young Mountain
B
Old mountain

Slide 36 - Quiz


A
Erosion
B
Sedimentation
C
Weathering

Slide 37 - Quiz


A
Erosion
B
Weathering
C
Sedimentation

Slide 38 - Quiz


A
Erosion
B
Sedimentation
C
Weathering

Slide 39 - Quiz


A
Erosion
B
Sedimentation
C
Weathering

Slide 40 - Quiz