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1.4 Rock becomes sediment
1.4 Rock becomes sediment
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Aardrijkskunde
Middelbare school
vmbo t, mavo, havo, vwo
Leerjaar 2
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Lesson duration is:
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Items in this lesson
1.4 Rock becomes sediment
Part 1
Slide 1 - Slide
Learning goals
- You can recognise the upper, midle and lower courses of rivers from photos.
- You understand how sedimentary rock is formed.
- You can explain how sandbanks, dunes and deltas are formed
Slide 2 - Slide
Upper course
Middle course
Lower course
Slide 3 - Slide
The Upper course
Slide 4 - Slide
Upper course
Slide 5 - Slide
Upper course
Slide 6 - Slide
Upper course
Upper course:
- weathering material (sediments) ends up in glaciers and rivers.
=
sediments
that have been loosened by weathering.
(rock that is formed by the deposit of material by water, wind or ice.)
- height difference large
- stream speed high
- deep valleys scoured
- a lot of erosion
Slide 7 - Slide
The Middle course
Slide 8 - Slide
Middle course
Slide 9 - Slide
Middle course
Slide 10 - Slide
Middle course
Middle course:
- height differences smaller
- river flows less quickly
- power of water decreases
- less erosion
- sedimentation of medium-sized pieces
Slide 11 - Slide
The Lower course
Slide 12 - Slide
Lower course
Slide 13 - Slide
Lower course
Slide 14 - Slide
Lower course
Lower course:
- little to no relief
- flat area
- river flows slowly
- sedimentation of small particles
Slide 15 - Slide
Make exercise
2 and 3
Slide 16 - Slide
1.4 Rock becomes sediment
Part 2
Slide 17 - Slide
Learning goals
- You can recognise the upper, middle and lower courses of rivers from photos.
- You understand how sedimentary rock is formed.
- You can explain how sandbanks, dunes and deltas are formed
Slide 18 - Slide
What are the characteristics of upper, middle and lower course.
Slide 19 - Slide
The origins of a grain of sand
Slide 20 - Slide
The heaviest material sinks first and the lightest material is deposited furthest from the river.
Slide 21 - Slide
Slide 22 - Slide
Slide 23 - Slide
Delta
How do you recognize a delta?
-A piece of land that extends into the sea.
-The river branches into several channels.
-It has a shape of a triangle.
Slide 24 - Slide
Rivers flow into the sea in different ways:
Delta: coast that is being formed when more material is deposited at the mouth of a river than is discharged into the sea by the current.
Estuary: wide river estuary, often in the shape of a funnel (trechter), which has been scoured by ebb and flow currents
Slide 25 - Slide
The formation of dunes
Slide 26 - Slide
Sandbank:
a deposit of sand forming a shallow area in the sea or a river. Beaches form on these.
Dunes
: a mound of sand formed by the wind, usually along the beach.
Slide 27 - Slide
Some of the sand that ends up in the sea ultimately forms the dunes.
Slide 28 - Slide
Slide 29 - Slide
Go to page 40-43
Make ex: 1, 4 and 5
Slide 30 - Slide
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