1.4 Rock becomes sediment




1.4 Rock becomes sediment



Part 1
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Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolvmbo t, mavo, havo, vwoLeerjaar 2

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1.4 Rock becomes sediment



Part 1

Slide 1 - Tekstslide

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 - Tekstslide

Upper course
Middle course
Lower course

Slide 3 - Tekstslide

The Upper course

Slide 4 - Tekstslide

Upper course

Slide 5 - Tekstslide

Upper course

Slide 6 - Tekstslide

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 - Tekstslide

The Middle course

Slide 8 - Tekstslide

Middle course

Slide 9 - Tekstslide

Middle course

Slide 10 - Tekstslide

Middle course
Middle course:
- height differences smaller
- river flows less quickly
- power of water decreases
- less erosion
- sedimentation of medium-sized pieces

Slide 11 - Tekstslide

The Lower course

Slide 12 - Tekstslide

Lower course

Slide 13 - Tekstslide

Lower course

Slide 14 - Tekstslide

Lower course
Lower course:
- little to no relief
- flat area
- river flows slowly
- sedimentation of small particles

Slide 15 - Tekstslide

Make exercise
2 and 3

Slide 16 - Tekstslide




1.4 Rock becomes sediment



Part 2

Slide 17 - Tekstslide

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 - Tekstslide

What are the characteristics of upper, middle and lower course.

Slide 19 - Tekstslide

The origins of a grain of sand

Slide 20 - Tekstslide

The heaviest material sinks first and the lightest material is deposited furthest from the river.

Slide 21 - Tekstslide

Slide 22 - Tekstslide

Slide 23 - Tekstslide

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 - Tekstslide

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 - Tekstslide

The formation of dunes

Slide 26 - Tekstslide

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 - Tekstslide

Some of the sand that ends up in the sea ultimately forms the dunes.

Slide 28 - Tekstslide

Slide 29 - Tekstslide

Go to page 40-43
Make ex: 1, 4 and 5

Slide 30 - Tekstslide