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ESO Y4B · Biology and Geology
The dynamic Earth · The dynamics of the geosphere

Plate tectonics

At the beginning of the 20th century, the almost perfect fit between the coasts of South America and Africa led Alfred Wegener to propose that the continents had once been joined together. Today that fit, together with evidence that Wegener could not provide, is explained by a single model: plate tectonics.

Before you start, make sure you know: The structure of the geosphere (1st ESO)
Before you start, make sure you know: The lithosphere and its materials (1st ESO)

From continental drift to plate tectonics

If you mark on a world map the epicentres of earthquakes and the active volcanoes of the last decade, you will see that they are not scattered at random, but form continuous lines that enclose huge, almost quiet areas. Why is our planet's geological activity concentrated at the edges of large blocks?

Map of the South Atlantic with South America in its present position and rotated until it fits the coast of Africa, where Mesosaurus fossils form a continuous strip on both sides. South America present position fit of Wegener Africa ocean Atlantic South America in its present position fit with Africa (Wegener) same fossils (Mesosaurus) on both sides movement
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Explain what a lithospheric plate is and name three plates: one containing Europe, an American one, and one that is almost entirely oceanic.

Explain what a lithospheric plate is and name three plates: one containing Europe, an American one, and one that is almost entirely oceanic.

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State whether the following statement is true or false and justify your answer: "Continents move because the lithospheric plates on which they rest move."

State whether the following statement is true or false and justify your answer: "Continents move because the lithospheric plates on which they rest move."

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The forces that move the plates

High-precision GPS stations measure that every year the distance between Madrid and New York increases by about $2{,}5\ \text{cm}$. What internal mechanism is capable of pushing masses of rock covering millions of square kilometres across the planet?

Animation of the diagram of the driving forces of the lithospheric plates: two convection currents circulate beneath the plates, plate 1 and plate 2 move apart at the ridge leaving a widening strip of magma, and plate 2 sinks and slides beneath plate 3 at the subduction zone; then everything returns to the start. plate 2 plate 1 plate 3
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State and briefly describe two forces that contribute to the movement of lithospheric plates.

State and briefly describe two forces that contribute to the movement of lithospheric plates.

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Palaeomagnetic and satellite measurements confirm that the Mid-Atlantic Ridge generates new oceanic lithosphere at a total spreading rate of about $2,5\ \text{cm/year}$,…

Palaeomagnetic and satellite measurements confirm that the Mid-Atlantic Ridge generates new oceanic lithosphere at a total spreading rate of about $2,5\ \text{cm/year}$, which has enabled the widening of the Atlantic Ocean since the breakup of Pangaea.

  1. a) A student proposes the following deduction: "Since ocean ridges worldwide continuously generate crust, the volume and surface area of the Earth must have grown steadily over the last $200$ million years". Refute their hypothesis by explaining what process compensates for the creation of lithosphere and at what type of plate boundaries it takes place.
  2. b) If the current distance between the coasts of West Africa and North America at that latitude is about $4\ 500\ \text{km}$, estimate how many million years ago the Atlantic Ocean began to open in that region, assuming that spreading rate remained constant.
  3. c) Predict and justify how the age of the rocks and the thickness of marine sediments will vary as you move from the ridge axis towards the African continental margin.
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The three types of plate boundary

In Iceland the ground splits open along large fissures from which fluid lava pours, while in the Andes gigantic stratovolcanoes rise above deep ocean trenches, and in California two blocks grind sideways past each other without any volcanism. Why does contact between plates produce such different landscapes and geological hazards?

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The diagram shows the three types of margins that can exist between two lithospheric plates. State which type of plate margin (divergent, convergent or transform)…

The diagram shows the three types of margins that can exist between two lithospheric plates. State which type of plate margin (divergent, convergent or transform) corresponds to each number and explain what happens to the plates in each case.

1 2 3
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In subduction zones, one plate slides beneath another. Describe two geological phenomena associated with these zones and give a real example of a subduction zone.

In subduction zones, one plate slides beneath another. Describe two geological phenomena associated with these zones and give a real example of a subduction zone.

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At the highest elevations of Mount Everest (above $8\ 000\ \text{m}$ in altitude), there are limestone strata containing abundant Mesozoic marine fossils. At the same…

At the highest elevations of Mount Everest (above $8\ 000\ \text{m}$ in altitude), there are limestone strata containing abundant Mesozoic marine fossils. At the same time, despite the violence of earthquakes in the Himalayas, no active surface volcanism is recorded, unlike what happens in the Andes mountain range.

  1. a) Justify in terms of density and buoyancy why the subduction of continental lithosphere does not occur in the collision between the Indian and Eurasian plates, explaining what crustal deformation phenomenon replaces subduction.
  2. b) Explain the sequence of tectonic events that allows ancient marine sediments from the Tethys Ocean to be found today at the highest peak on the planet.
  3. c) Argue why there are dozens of active volcanoes in the Andes and none in the Himalayas, relating the presence or absence of arc magmatism to the thermal and melting fate of the colliding plate.
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The evidence for seafloor spreading

World map with the plate boundaries coloured according to type and three examples marked: the Mid-Atlantic Ridge (divergent), the Mariana Trench (convergent) and the San Andreas Fault (transform). Ridge Mid- Atlantic Trench Mariana Trench San Andreas Fault Divergent (ridge) Convergent (trench) Transform Plate boundaries: P. Bird (2003) Example from the text
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An oceanographic vessel records the magnetic anomalies of the seafloor along a transect perpendicular to an ocean ridge. The data reveal that the last global magnetic…

An oceanographic vessel records the magnetic anomalies of the seafloor along a transect perpendicular to an ocean ridge. The data reveal that the last global magnetic reversal (which occurred $780\ 000$ years ago) is found in basaltic stripes located $15,6\ \text{km}$ to the east and $15,6\ \text{km}$ to the west of the central rift.

  1. a) Justify how the symmetry of the magnetic stripes originates from the cooling of magma and explain why this pattern constituted definitive proof of seafloor spreading.
  2. b) Calculate the total spreading rate of this seafloor (in $\text{cm/year}$).
  3. c) If at a different ridge the same anomaly from $780\ 000$ years ago is located $62,4\ \text{km}$ from the rift, interpret what differences exist between both margins regarding the rate of crust generation and tectonic dynamism.
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Summary

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