Doc Brown's Chemistry - Earth Science Revision Notes

9. More on Plate Tectonics and subduction

Revision KS4 Science IGCSE/O level/GCSE Chemistry Information Study Notes for revising for AQA GCSE Science, Edexcel 360Science/IGCSE Chemistry & OCR 21stC Science, OCR Gateway Science  (revise courses equal to US grades 9-10)

based on a GCSE Geological & Earth Science TASK SHEET * Earth Science Homepage * 5 multi-word fill GCSE worksheets + answers * GCSE Earth Science Quiz: Foundation-easier m/c Quiz and Higher-harder level m/c Quiz

ANSWERS-NOTES 1. The Evolution of the Earth's atmosphere and Carbon Cycle ... 2. The Rock Cycle and types of rock (details 'evolve' through sections 3. to 9.) ... 3. Weathering of Rocks ... 4. Igneous Rocks ... 5. Sedimentary Rocks ... 6. Metamorphic Rocks ... 7. The Structure of the Earth ... 8. Plates and their movement ... 9. Plate Tectonics ... 10. The Moon and Planets

9. More on Plate Tectonics and subduction (using the basic ideas to explain all the effects)

9.1

9(a) When plates move apart: New crust is formed mainly at mid-ocean ridges where magma breaks through a huge fractures in the crust. ((2) in Fig 9.1 above) This is known as sea floor spreading and is happening along oceanic ridges, including the mid-Atlantic ridge. This causes cracks through which more molten magma material from deep below the lithosphere can push through producing new rock. The magma from theses chains of linked undersea volcanoes (or just long gashes of hundreds of kilometres!)  rapidly cools to form basalt type rocks of the new crust spreading out on either side. (see also evidence for this mechanism) Sometimes a long central rift valley forms (4). All in all, what is described below, is the detail of the ultimate rock recycling machine!

9(b) When plates collide [more in 9(c)]: Crust material is removed from the tectonic plates whenever two plates collide head on because one plate descends into the subduction zone to be melted and combined with the mantle material ((1) oceanic-oceanic plates meeting (e.g. Pacific Ring of Fire) and (3) oceanic-continental plates meeting (e.g. Andes Mountains) in Fig 9.1 above). One plate descends into a deep ocean trench, and mud and sand  pour into these trenches and at (3) can end up as bands of metamorphic rock in the 'fold' mountains - see 9(c).

9(c) When continental plate meets oceanic plate the thinner more dense oceanic plate subducts below the continental plate, and partly melts under the thicker but less dense granitic plate. Deep ocean off-shore trenches are formed and parallel mountain chains with volcanoes and earthquake activity too. The geology can be complex and the sediments of the continental crust get crunched up into fold mountains. Metamorphic rocks can be formed due to the heat and pressure in the processes (casing recrystallisation without melting), accompanied by considerable faulting, folding, igneous intrusions and volcanoes. Some of the molten rock cools deep below the surface to form course-grained grained rocks like granite. The magma which rises to the surface cools rapidly to form fined grained rocks like basalt lava.

If continental plates meet (i.e. after all the ocean has been squeezed out!), the massive collision and compression can build up huge mountain ranges like the Himalayas. Even the pre-existing sedimentary rocks, like limestone and sandstone from the seas originally between the plates, can be squashed up and become part of the fold mountain ranges (the top of Mount Everest is limestone!). They can also be heated to give regions of metamorphic rock, more folding and compressional faulting. The whole process goes on for millions of years! and these 'new' mountain ranges replace 'older' ones worn down by weathering and erosion processes.

See below for side-ways passing movement.

• When two plates meet e.g. at (1) or (3) in Fig 9.1 then the rocks are compressed and the tension builds up even if one plate is descending. Eventually a point comes were the strain in the rocks is too much for the structure to maintain and the rock layers move suddenly to relieve the tension. The release of energy is enormous and radiates out as 'shock waves' or seismic waves. These can create fault lines which themselves can be centres of seismic activity. Earthquake have enormous destructive power, not just on land, but undersea they create giant tidal waves called 'tsunami'.
• Earthquake power can be measured on the:
  • Richter Scale based on shock wave acceleration and energy.
    • It is a logarithmic scale, meaning an increase in 1 unit means 10x more powerful.
    • An earthquake of magnitude 7 is 1000x more powerful than one of magnitude 4 on the Richter scale.
  • Mercalli Scale is based on a succession of increasingly 'dramatic' observed events.
    • It was devised before Richter's Scale.
    • What the geologist Richter did was to give Mercalli's scale numerical values based on seismometer vibration measurements. The bigger the vibration amplitude, the more powerful the earthquake.
  • Earthquakes can be detected with an instrument called a seismometer, which detects vibrations in the ground its placed on. It is even sensitive enough to detect the minute vibrations in the earth's crust thousands of miles from the epicentre of an earthquake. From the graph of the amplitude of the wave (vibration) versus time (from a seismograph instrument connected to the seismometer), the energy released by the earthquake wave can be measured and a value assigned to it on the Richter Scale. Also, from the time intervals of the graph, and compiling and processing data from several seismographic stations around the world, it is possible to work out where the earthquake took place as well as its strength.
  • Other uses of seismometers
    • Seismographic data can also be used to analyse the structure of the earth e.g. the density and thickness of the crust, mantle and inner & outer layers of the mantle by analysing the complicated wave patterns of the vibrations of earthquake waves.
    • Seismometers have been used in the past (particularly in the West versus Russia 'Cold War') of the 1950's, 1960's and 1970's to detect and measure the power and geographical locations of underground explosions from the testing of atomic weapons. The task of seismograph technicians continues as other countries have developed nuclear weapons.

Richter Scale	Mercalli Scale
< 3.5	only detected by seismometers, very sensitive people
3.5-4.2	feels like a heavy truck passing
4.3-4.8	felt by people walking, most sleepers wakened
4.9-5.4	objects swing and overturn causing damage, trees sway
5.5-6.1	walls crack, general alarm
6.2-6.9	buildings damaged, chimneys fall
7.0-7.3	ground cracks, buildings collapse, pipes break
7.4-8.0	most buildings and bridges  collapsed, major services out; landslides
> 8.1	total destruction, objects thrown in air, ground moves in violently in waves

• When plates move apart where no magma breaks through, land between 'slips' down 'fault' lines and this causes seismic activity, see (4) in Fig 9.1. Also at mid-ocean ridges, the new crust movement can trigger earthquakes, see (2) in Fig 9.1
•  
• The plates can pass each other sideways and the 'grinding action' causes tension to build up in the rocks either side of the fault line. Occasionally, and unpredictably the stored tension energy is released causing earthquake activity. An example of this is infamous San Andreas fault in California USA. Note: When plates pass sideways there is no loss or gain of plate material and usually little volcanic activity but there are plenty of minor earthquakes and every so often 'the big one' - ask the people of LA!
  • There is good evidence of side-ways movement in Scotland on the SE to NE 'line' along the Great Glen of northern Scotland, though thankfully, there is no seismic activity to worry about!
•  
• Most earthquakes happen many km below the Earth's surface and it is difficult to monitor and evaluate all the factors that might help to predict when an earthquake might happen e.g. temperature, earth tremors, gas emissions etc. So, unfortunately tragedies continue to happen, even though scientists do their best, despite the uncertainties of the situation, to make accurate predictions.

9(e) Volcanoes tend to form where plates meet ((1) (e.g. Pacific Ring of Fire) and (3) (e.g. the east Pacific ocean trench and the Andes Mountains on the South American plate) in Fig 9.1). The crust and mantle are disturbed in the subduction zone and extra heat is generated from compression and friction. Some of the upper mantle becomes much more fluid, 'gassy' and less dense. This results in hot magma working its way upwards to break through as a volcano. The explosive force of volcanoes is usually due to the rapid release of high pressure gas trapped in the magma. This can throw out huge quantities of magma, rocks and volcanic ash to form surrounding deposits which can be studied by volcanologists to research the history of a volcanoes eruptions.

9(f) Fig 9.2 Folds and Faults caused by tectonic activity - plate movement

an anticline near Mizen Head, West Cork, Ireland

Fig 9.2

• Folding shows the compression of layers due to plate tectonic movement as plates meet head on! Along the various layers of rock a curve down is called a syncline, a curve in an upwards is called an anticline.
• Sometimes large sections of rock layers are tilted at extreme angles by the tectonic forces.
• Fault lines are huge 'cracks' down through layers of rocks. They are caused by earthquake activity and for subsequence earthquakes, the rock movement is often along these fault lines.
• In the diagram the sequence might be interpreted as follows from 10 up to 1:
  • layers from 10 up to 4 laid down in that order with 10 first
  • the folding occurs later, since newer layers of sedimentary rock would tend to be laid on top and fill up the fold.
  • the faulting occurred after the folding because all the folds are uniformly displaced
  • the left folds have been displaced downwards with respect to the middle section (or middle folds upwards with respect to left folds)
  • the more right linear sections may have been moved upwards with respect to the middle section or the middle section has slipped down.
  • layers 3, 2 and 1 could be the most recent sedimentary rock layers laid down later on top of the eroded layers 4-6 (by weather or glaciations) and have not been subjected to major tectonic forces since there is no evidence of folding or faulting.
• Folding and faulting can give information on the magnitude and direction of the tectonic forces involved.

9(g) A rift valley is formed on continental crust when two plates move away from each other and the land in between falls as shown in (4). This is exemplified by the Great Rift Valley of Africa but it can also be filled with sea water e.g. the Red Sea between the African Continent and the Arabic states.

9(h) In Fig 9.1 above the loss of plate at (1) and (3) is matched by the creation of new crust at (2)!

9(i) In situation (2) new crust is formed but at (1) and (3) crust is being moved. So all new rocks have their start at (1) and eventually end up, in whatever rock form, by returning to the mantle at (1) or (3). Hence all mineral material is eventually recycled in the 'big picture' shown in Fig 9.3 below

Fig 9.3

and Fig 9.1 above. Most of these 'answer notes' are looking at the details of all the primary and secondary processes involved. Note in Fig 9.1 above the arrow ==> on the right could match up with the ==> on the left i.e. its a 'balanced' global cycle both internally and externally! Any mountain ranges not subducted still get worn away by weathering and erosion, so everything gets recycled in the end!

Fig 9.4 A simpler approach to the "THE ROCK CYCLE" to show the relationship between the three types of rocks - the "3rd Big Picture View"

Fig 9.4

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