"...as to merit respectful and sympathetic interest from every geologist. Some striking arguments in his favor have been advanced, and it would be foolhardy indeed to reject any concept that offers a possible key to the solution of profound problems in the Earth's history.” - Chester R. Longwell, "Some Thoughts on the Evidence for Continental Drift," 1944
Wegener and his supporters did all they could do to find evidence to support continental drift. But without a mechanism the idea would not be accepted. What was needed was the development of technologies that would allow scientists to find more evidence for the idea and help them describe a mechanism. But first, they would find still more evidence that the continents had moved.
The next breakthrough in the development of the theory of plate tectonics came two decades after Wegener’s death. Magnetite crystals are shaped like a tiny bar magnet. As basalt lava cools, the magnetite crystals line up in the magnetic field like tiny magnets. When the lava is completely cooled, the crystals point in the direction of magnetic north pole at the time they form. How do you expect this would help scientists see whether continents had moved or not?
Magnetite crystals.
As a Wegener supporter, (and someone who is omniscient), you have just learned of a new tool that may help you. A magnetometer is a device capable of measuring the magnetic field intensity. This allows you to look at the magnetic properties of rocks in many locations. First, you’re going to look at rocks on land. Which rocks should you seek out for study?
Geologists noted important things about the magnetic polarity of different aged rocks on the same continent:
Earth’s current north magnetic pole is in northern Canada.
In other words, although the magnetite crystals were pointing to the magnetic north pole, the location of the pole seemed to wander. Scientists were amazed to find that the north magnetic pole changed location over time (Figure below).
The location of the north magnetic north pole 80 million years before present (mybp), then 60, 40, 20, and now.
Can you figure out the three possible explanations for this? They are:
How do you figure out which of those three possibilities is correct? You decide to look at magnetic rocks on different continents. Geologists noted that for rocks of the same age but on different continents, the little magnets pointed to different magnetic north poles.
Now look again at the three possible explanations. Only one can be correct. If the continents had remained fixed while the north magnetic pole moved, there must have been two separate north poles. Since there is only one north pole today, what is the best explanation? The only reasonable explanation is that the magnetic north pole has remained fixed but that the continents have moved.
How does this help you to provide evidence for continental drift? To test the idea that the pole remained fixed but the continents moved, geologists fitted the continents together as Wegener had done. It worked! There has only been one magnetic north pole and the continents have drifted (Figure below). They named the phenomenon of the magnetic pole that seemed to move but actually did not apparent polar wander.
On the left: The apparent north pole for Europe and North America if the continents were always in their current locations. The two paths merge into one if the continents are allowed to drift.
This evidence for continental drift gave geologists renewed interest in understanding how continents could move about on the planet’s surface.
NOTES / HIGHLIGHTS
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| Image | Reference | Attributions |
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| Credit: Courtesy of the National Oceanic and Atmospheric Administration Source: http://www.moc.noaa.gov/tj/visitor/photo-las2.html License: Public Domain | ||
| Credit: Parent Géry Source: https://commons.wikimedia.org/wiki/File:Magn%25C3%25A9tite_(Bolivie).jpg License: CC0 | ||
| Credit: Courtesy of the National Oceanic and Atmospheric Administration Source: http://apod.nasa.gov/apod/ap040919.html License: Public Domain | ||
| Credit: Sam McCabe Source: CK-12 Foundation License: CC BY-NC 3.0 | ||
| Credit: Christopher AuYeung Source: CK-12 Foundation License: CC BY-NC 3.0 |
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