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Lesson 3 The Rhine
Lesson 3
Erosion
1 / 26
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Slide 1:
Tekstslide
Aardrijkskunde
Middelbare school
havo, vwo
Leerjaar 2
In deze les zitten
26 slides
, met
tekstslides
.
Lesduur is:
80 min
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Lesson 3
Erosion
Slide 1 - Tekstslide
Goals
Students can explain what erosion is and how it affects nature.
Students can explain how weathering material is transported and by what transport agents.
Students can explain the landscape cycle in their own words.
Students know what different types of relief there are.
Students can explain what young and old mountains are and how we can recognise these.
Slide 2 - Tekstslide
2N:
Read lesson 2 completely.
Mark all the important sentences
Make exercises 1a, 2b, 3a, 3c, 3d, 4, 5
2H & 2G:
Read lesson 2 completely.
Mark all the important sentences
Make exercises 1, 2a, 2b & 3a, 3c & 3d, 4a, 5 & 6a.
Slide 3 - Tekstslide
Recap
Students know how the alps are formed.
Students know what weathering is.
Students know different types of weathering and can explain the difference.
Slide 4 - Tekstslide
Slide 5 - Tekstslide
Rocks are being moved
Weathered material is carried away by rivers, glaciers and by the wind. In the process,
erosion
occurs.
Three transporters:
Water
Ice
Wind
Slide 6 - Tekstslide
Erosion
= When a
transport agent
carries stones along with it and wears away the rock or landscape.
The big difference between weathering and erosion is that erosion always involves a transport agent.
Slide 7 - Tekstslide
Valleys
If this erosion continues for millions of years it can create valleys.
A
river valley
has a V-shape and a
glacial valley
has a U-shape.
Slide 8 - Tekstslide
?
?
Slide 9 - Tekstslide
Glacial valley
River valley
Slide 10 - Tekstslide
Weathering and erosion
Weathering and erosion cause the solid rock to continue to disintegrate.
Put the following soil types in the correct order from coarse to fine:
Clay
Sand
Gravel
Rocks
Slide 11 - Tekstslide
Erosion at a glacier site
When a new layer of snow falls each year and doesn’t melt away, the snow will accumulate. -->
firn basins
The weight of all the
firn
causes the glacier to slowly flow down from the firn basin (glacier ice is plastic/bendable),
scraping across the bottom and along the sides
--> Erosion
Slide 12 - Tekstslide
Slide 13 - Tekstslide
Landscape cycle
Slide 14 - Tekstslide
Slide 15 - Tekstslide
Get to work!
Read lesson 3 up to 'Relief'
Mark all the important sentences
2N: Make exercises 1, 3, 4 & 5
2H/2G: Make exercises 1, 4 & 5
Slide 16 - Tekstslide
Relief
Variations in height =
relief
Lowlands
= 0-200 meter
Hill country
= 200-500 meter
Low mountain range
= 500-1500 meter
High mountain range
= 1500 meter and higher
Slide 17 - Tekstslide
What relief are these mountains?
Slide 18 - Tekstslide
Mountain ranges
Mountains crumble and wear away through
weathering and erosion.
We have young and old mountain ranges.
Mountains with a lot of relief and high, sharp peaks -->
young mountain ranges
Mountains with little relief and low, round tops -->
old mountain ranges
Slide 19 - Tekstslide
Young or old mountain?
Slide 20 - Tekstslide
Young or old mountain?
Slide 21 - Tekstslide
Young or old mountain?
Slide 22 - Tekstslide
Young or old mountain?
Slide 23 - Tekstslide
Young or old mountain?
Slide 24 - Tekstslide
Get to work!
Read lesson 3 completely
Mark all the important sentences
2N: Make exercises 1, 2, 3, 4, 5 & 6
2H/2G: Make exercises 1, 2a, 2b, 2c, 4, 5 & 6
Slide 25 - Tekstslide
Goals
Students can explain what erosion is and how it affects nature.
Students can explain how weathering material is transported and by what transport agents.
Students can explain the landscape cycle in their own words.
Students know what different types of relief there are.
Students can explain what young and old mountains are and how we can recognise these.
Slide 26 - Tekstslide
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