independent learning. progress checker learning activities: 1.read the lesson materials before...
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Independent Learning
Progress Checker
Learning Activities:
1.Read the lesson materials before attending the lessons.2.Attended the lessons3.Fully participated and engaged in lessons.4.Used deep processing strategies.5.Practised retrieval and application of info6.Self-assessed level of understanding and made notes or read additional material to clarify understanding or extend learning.Each Week:
1.YES or NO if learning activity completed or not.2.0 – 5 to show how much you feel you have learnt for that week. 3.Maintain your file as evidence of the learning activities, including notes, answers to set questions, independent learning tasks and any additional reading
Take Charge of Your Learning
YES
YES
YES
YES
YES
YES
4
By using this sheet every week!
Plate Tectonics
Learning Outcomes:
By the end of the lesson you should be able to...
1.Name and label the major relief features of the Earth on a world map and cross-sections through the Earth’s surface
2.Name the different types of plate boundary that exist on a map of the major relief features of the Earth and indicate the direction of plate movement.
Major Relief Features of the Earth
Ocean Basins•Mid-oceanic ridges•Ocean trenches•Rift valleys•Volcanic island chains•Mountain belts (volcanic island arcs)
Continents•Mountain belts (non-volcanic)•Mountain belts (continental volcanic arcs)
Plate Boundaries•Constructive
•Destructive
•Conservative
Major Relief Features of the Earth
Major Relief Features of the Earth
Cross-section 1
Cross-section 3
Cross-section 2
A B A
A
B
B
MOROceanic trench
Continental volcanic
arc
Constructive plate boundary
Destructive plate boundary
Cross-section 1Cross-section 1
A B
Oceanic trench
Island arc volcano
Destructive plate boundary
Cross-section 2
Cross-section 2
A
B
Cross-section 3
Cross-section 3
A
B
Destructive plate boundary
Mountain belt (non-volcanic)
Learning Outcomes:
By the end of the lesson you should be able to...
1.Define the characteristics of the upper layers of Earth involved in plate tectonics.
2.Explain the importance of the asthenosphere in plate tectonic theory.
3.Outline the theory of plate tectonics.
Plate Tectonic Theory
Constructive plate margins
Destructive plate margins
Conservative plate margins
Plate Tectonic Theory
Learning Outcomes:
By the end of the lesson you should be able to...
1.Describe the relationship between seismicity, volcanicity and plate boundaries.
2.Explain the distribution of earthquakes and volcanoes.
Learning Outcomes:
By the end of the next two lessons you should be able to...
1.Describe the location of the Earth’s major tectonic features.2.Explain the formation of the Earth’s major tectonic features.
Ocean Basins•Mid-oceanic ridges•Ocean trenches•Rift valleys•Volcanic island chains•Mountain belts (volcanic island arcs)•Earthquakes
Continents•Mountain belts (non-volcanic)•Mountain belts (continental volcanic arcs)•Earthquakes
Learning Outcomes:
By the end of the next two lessons you should be able to...
1.Describe the location of the Earth’s major tectonic features.2.Explain the formation of the Earth’s major tectonic features.
1 2 3 4 5
MegMattyCameronGeorge
ShannonJackJoshDaniel
EllisJordonJamesDanny
LiamJakeCaleb
MelissaDamianEddie
1. Constructive Plate Margin2. Destructive Plate Margin (continental-
oceanic)3. Destructive Plate Margin (oceanic-oceanic)4. Conservative Plate Margin5. Intraplate (hot spots)
Groups:
Plate Tectonic Theory
Shallow focus earthquakes 0 – 70km
Intermediate focus earthquakes 70 – 300km
Deep focus earthquakes 300 – 700km
Benioff ZoneInclined zone where earthquakes occur
Constructive Plate Margin
Destructive Plate Margin
Shallow focus earthquakes 0 – 70km
Constructive Plate Margins
Transform fault
Mid-Oceanic ridge
Rift valleyBasaltic, shield volcano
Strong, solid, brittle layer
Weak, mobile, semi-molten layer (<1% molten)
•Low angled (< 10°)
•Non-explosive (effusive)
Volcanic tremor (rising magma)
1
2
3
Tectonic tremor (transform fault)Tectonic tremor (normal faults)
Evidence for Plate Tectonics
Mid-Atlantic Ridge
Constructive Plate Margins
Peridotite BasalticPartial melting
Peridotite (Ultra-basic)
Basic magma
Intermediate magma
Acidic magma
- Basaltic
- Andesitic
- Rhyolitic
Basalt
DoleriteGabbro
Constructive Plate Margins
Destructive Plate Margins
Mt Pinatubo, Philippines Andesitic, cone-shaped volcano, explosive
Benioff Zone
Oceanic Trench
Partial melting of basaltic oceanic crust
Volcanic Island ArcSubduction
of denser oceanic crust
Deep focus earthquakes
Shallow focus earthquakes
Destructive Plate Margins
Conservative Plate Margins
6 cm/year 2 cm/year
San Andreas Fault
Hot Spots
Plate Tectonic Theory1. Evidence for Earth’s internal heat energy:
• volcanoes
• hot springs
• deep mines
2. Causes for Earth’s internal heat energy:
• radioactive decay in the mantle & crust
• iron crystallisation in core
• residual heat from Earth formation
3. How is heat transferred from Earth interior?:
• conduction
• convection
4. What is the theory of plate tectonics?:
• The upper part of the mantle and overlying crust form the rigid lithosphere.• The lithosphere is split up into 7 large and many smaller sections known as lithospheric plates.
• These plates are underlain by a semi-mobile zone in the upper mantle known as the asthenosphere.
• Convection currents in the mantle cause the plates to move over the asthenosphere, either moving apart, together or against each other.
Earth’s Major Features and Plate Tectonics
Destructive Plate Margin
Constructive Plate Margin
MOR
Basaltic Magma
Decompression Melting
Oceanic Crust
Lithosphere
Asthenosphere
Subd
ucting
Sla
b
Hyd
ration
Mel
ting
Asthenosphere
Lithosphere
Andesitic Magma
Continental Crust
Continental Volcano Oceanic Trench
Ben
ioff Z
one
Learning Outcomes:
By the end of the lesson you should be able to...
1.Outline how palaeomagnetism can be used to plot plate movements over time.2.Plan a response to an exam essay question.
1 2 3 4 5
AbigailDan WNathan
HannahAyazKieran
LukeAmandaDan H
VickiJackBob
GraceSamDavid
A. Magnetic InclinationB. Apparent Polar Wandering CurvesC. Magnetic Anomalies in the Oceanic
Crust
Learning Outcomes:
By the end of the lesson you should be able to...
1.Outline how palaeomagnetism can be used to plot plate movements over time.2.Plan a response to an exam essay question.
Learning Outcomes:
By the end of the lesson you should be able to...
1.Outline how palaeomagnetism can be used to plot plate movements over time.2.Plan a response to an exam essay question.
Outline how palaeomagnetism can be used to plot plate movements over time. (25 marks)
Monday 1st October
Put these 8 images in order
to explain palaeomagnetis
m.
• Iron minerals in basalt e.g. magnetite
• Rotate & align with magnetic field
• Remain in this position after magma cools – remnant magnetism
• Magnetic reversals
• New magnetite minerals magma iron aligns in different direction
Palaeomagnetism
• Liquid basalt
• Basalt cools below Curie point (< 570° C for magnetite)
• Earth’s magnetic field
• Magnetic anomalies at constructive plate margins
• Apparent polar wandering curves• Magnetic inclination gives latitude of erupted basalt
Evidence for Plate Tectonics
Magnetic Anomalies at MOR
Magnetic Anomalies at MOR
Calculate the rate the oceanic crust is moving away from the MOR. Your answer should be in mm/year.
60km
Earth’s magnetic field
Orientation of magnetic iron minerals in lavas formed at different latitudes
Earth’s Magnetic Field
Latitude Magnetic Angle
0° 0°
30° 50°
60° 70°
90° 90°
Magnetic Anomalies
Earth’s Magnetic Field & Plate Tectonics
Sediment
Basaltic pillow lavas & dolerite dykes
Gabbro
Eruption Type
Composition(Acid/Basic)
Viscosity (High/Low)
Temperature
Main Products
Plate Location
Effusive
Explosive
Heat flow(mW/m²)
50 60 70 120
180
70 40 20 40 50 60 75 295
100
70 60
Km 0 10 18 20 23 30 40 45 50 60 70 85 90 93 95 100
• Mid-oceanic ridges
• Oceanic trench
• Oceanic lithosphere
• Continental lithosphere
• Subducting plate
• Benioff zone
• Oceanic crust
• Continental crust
• Asthenosphere
• Moho
• Partial melting (twice)
• Basaltic magma
• Andesitic magma
• Gabbro
• Dolerite dykes
• Basaltic pillow lavas
• Sediment
• Shield volcano
• Cone-shaped volcano
• Slab pull/ridge push
Evidence for Plate Tectonics
Evidence for Plate Tectonics
Evidence for Plate Tectonics
Depth (km) Geotherm (°C) Melting point of Peridotite (°C)
0 15 1200
50 1250 1350
200 1450 1600
500 1900 2100
1000 2500 3000
2000 3250 3600
3000 4000 3850
4000 4250 4050
5000 4250 4200
6000 4250 4500
Temperature Variation within Earth’s Interior
Temperature Variation within Earth’s Interior
Depth (km)
Temperature (°C)
Inner Core
(solid)
Outer Core
(liquid)
Asthenosphere (semi-solid)
Mesosphere (solid)
Temperature Variation within Earth’s Interior
GeothermMelting curve
Depth (km)
Temperature (°C)
Inner Core
(solid)
Outer Core
(liquid)
Lithosphere (solid)
Asthenosphere (semi-solid)
Mesosphere (solid)
Where does this heat come from?
• Radiogenic heat
• Primordial heat
• What?
• Why?
• Where?
• Who?
• When?
• How?
• Which?
Plate Tectonic Theory
Plate Tectonic Theory
Plate Tectonic Theory
Plate Tectonic Theory