Tuesday, March 31, 2015
Wednesday, March 25, 2015
Types of Volcanoes
Shapes
and sizes of volcanoes
•Volcanoes vary in shapes and
sizes
due to the characteristics of the lava.
•Viscosity refers to the stickiness
of the lava
•The most common types of volcanoes are:
- Shield
volcanoes;
and
- Strato volcanoes
Danial's video
http://study.com/academy/lesson/types-of-volcanoes-shield-cinder-cones-composite-cones.html#lesson
Watch
this video from Danial and answer :
1.Shield volcano
– Shape and size
2.Strato volcano – shape and size
3.Which is more
explosive?
Individual Task:
1. Complete P59 - Compare between a Strato and shield volcano [4]
2. Draw a strato and shield volcano on top empty space of P59
(Show Miss ST completed work before proceeding to computers)
Computer Task:
1. Mark Answers for P59. Refer to class blog 'Volcanoes ppt' posted on 18 March on Slide 17
2. Complete ALL corrections
3. Hand up resource pack (for PTM tmr)
Monday, March 23, 2015
Wednesday, March 18, 2015
Answers to P54
8 With the aid of a well-labelled diagram, explain the formation of fold mountains at a continental-continental plate boundary. [4]
•2m (diagram) , 0.5m for each point
below
•Two continental plates may collide
with one another, resisting subduction.
•This causes the plates to break
and slide along fractures
in the crusts.
•When continental Eurasian plate converge
with continental Indian plate,
•the crusts are compressed and they fold
upwards or sideways to form fold mountains
P54
Q9
Explain
how the plate movement taking place at a
continental-oceanic plate
boundary may produce fold mountains.
[4]
•When an oceanic plate converges with
a continental plate
•The denser oceanic plate subducts under
the less dense continental plate
•As the continental plate rode over
the oceanic plate, the sediment on the ocean floor buckled and crumpled
•This cause an uplift of the crust
into the fold mountains
Monday, March 9, 2015
Wednesday, March 4, 2015
San Andreas Fault - Transform Boundary Qn
(i) Describe the appearance of the fault and its surrounding landscape. [4]
Appearance
• Long/linear
• Narrow
• Deep valley
• Fault line offsets to the right
• Presence of river within the fault
Surrounding landscape
• Hills are dissected
• Surrounding lands are highland
• Presence of some vegetation max4@1 mark
(ii) Explain how an earthquake may occur at this type of plate boundary. [4]
• The 2 plates are sliding past each other in opposite direction.
• There is a lot of friction and the movement is not smooth.
• Stress build up
• Over time, shock is suddenly released resulting in earthquakes.
Appearance
• Long/linear
• Narrow
• Deep valley
• Fault line offsets to the right
• Presence of river within the fault
Surrounding landscape
• Hills are dissected
• Surrounding lands are highland
• Presence of some vegetation max4@1 mark
(ii) Explain how an earthquake may occur at this type of plate boundary. [4]
• The 2 plates are sliding past each other in opposite direction.
• There is a lot of friction and the movement is not smooth.
• Stress build up
• Over time, shock is suddenly released resulting in earthquakes.
Monday, March 2, 2015
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