6 January 1912

German geophysicist Alfred Wegener first presents his theory of continental drift.

Alfred Wegener was a German meteorologist, polar researcher, and geophysicist who proposed the theory of continental drift in the early 20th century. His groundbreaking ideas challenged the prevailing scientific views of his time and laid the foundation for the modern theory of plate tectonics. Wegener’s work was instrumental in shaping our understanding of Earth’s dynamic geology.

Wegener’s theory of continental drift, first presented in 1912, suggested that the continents were not fixed in their positions but rather had drifted over time. He proposed that all continents were once part of a single supercontinent, which he named Pangaea, and that they had gradually drifted apart to their current positions.

Wegener supported his continental drift hypothesis with several lines of evidence:

Fit of the Continents: Wegener noticed that the coastlines of continents such as South America and Africa seemed to fit together like pieces of a jigsaw puzzle. This suggested that these continents were once connected.

Fossil Evidence: Similar fossilized plants and animals were found on continents that are now widely separated by oceans. For example, fossils of the extinct reptile Mesosaurus were found in both South America and Africa, indicating that these continents were once connected.

Rock Formations and Mountain Ranges: Wegener observed similarities in rock formations and mountain ranges across continents, such as the Appalachian Mountains in North America aligning with the Caledonian Mountains in Scotland and Scandinavia. This suggested a geological connection between these regions.

Paleoclimatic Evidence: Wegener also pointed out the presence of glacial deposits and evidence of past climates that were inconsistent with the current positions of the continents. For instance, he argued that coal beds found in Antarctica indicated that the continent was once situated in a much warmer climate.

Despite the compelling evidence, Wegener faced skepticism from the scientific community. One major challenge was the lack of a plausible mechanism explaining how continents could move across the Earth’s surface. Wegener suggested that the continents plowed through the ocean floor, but this idea was not well-received.

It wasn’t until the mid-20th century, with the development of plate tectonics theory, that Wegener’s ideas gained widespread acceptance. Plate tectonics provided a mechanism for the movement of continents by proposing that the Earth’s lithosphere is divided into rigid plates that float on the semi-fluid asthenosphere beneath them. The movement of these plates explained the observed phenomena associated with continental drift.

6 January 1994

American figure skater Nancy Kerrigan is attacked and injured by an assailant hired by her rival Tonya Harding’s ex-husband during the U.S. Figure Skating Championships that they were both taking part in.

6 January 1912

The German geophysicist Alfred Wegener first describes his theory of continental drift.

article is about the development of the continental drift hypothesis before 1958. For the contemporary theory, see plate tectonics. For the Russell Banks novel, see Continental Drift. For the fourth film in the Ice Age franchise, see Ice Age: Continental Drift.

The continental drift of the last 250 million years

Antonio Snider-Pellegrini’s Illustration of the closed and opened Atlantic Ocean.
Continental drift is the theory that the Earth’s continents have moved over geologic time relative to each other, thus appearing to have “drifted” across the ocean bed. The speculation that continents might have ‘drifted’ was first put forward by Abraham Ortelius in 1596. The concept was independently and more fully developed by Alfred Wegener in 1912, but his theory was rejected by many for lack of any motive mechanism. Arthur Holmes later proposed mantle convection for that mechanism. The idea of continental drift has since been subsumed by the theory of plate tectonics, which explains that the continents move by riding on plates of the Earth’s lithosphere.

Abraham Ortelius, Theodor Christoph Lilienthal, Alexander von Humboldt, Antonio Snider-Pellegrini, and others had noted earlier that the shapes of continents on opposite sides of the Atlantic Ocean seem to fit together. W. J. Kious described Ortelius’ thoughts in this way:

Abraham Ortelius in his work Thesaurus Geographicus … suggested that the Americas were “torn away from Europe and Africa … by earthquakes and floods” and went on to say: “The vestiges of the rupture reveal themselves if someone brings forward a map of the world and considers carefully the coasts of the three.”

In 1889, Alfred Russel Wallace remarked, “It was formerly a very general belief, even amongst geologists, that the great features of the earth’s surface, no less than the smaller ones, were subject to continual mutations, and that during the course of known geological time the continents and great oceans had, again and again, changed places with each other.”[8] He quotes Charles Lyell as saying, “Continents, therefore, although permanent for whole geological epochs, shift their positions entirely in the course of ages.”[9] and claims that the first to throw doubt on this was James Dwight Dana in 1849.

In his Manual of Geology, Dana wrote, “The continents and oceans had their general outline or form defined in earliest time. This has been proved with respect to North America from the position and distribution of the first beds of the Silurian – those of the Potsdam epoch. … and this will probably prove to the case in Primordial time with the other continents also”. Dana was enormously influential in America – his Manual of Mineralogy is still in print in revised form – and the theory became known as Permanence theory.

This appeared to be confirmed by the exploration of the deep sea beds conducted by the Challenger expedition, 1872-6, which showed that contrary to expectation, land debris brought down by rivers to the ocean is deposited comparatively close to the shore on what is now known as the continental shelf. This suggested that the oceans were a permanent feature of the Earth’s surface, and did not change places with the continents.

Apart from the earlier speculations mentioned in the previous section, the idea that the American continents had once formed a single landmass together with Europe and Asia before assuming their present shapes and positions was speculated by several scientists before Alfred Wegener’s 1912 paper. Although Wegener’s theory was formed independently and was more complete than those of his predecessors, Wegener later credited a number of past authors with similar ideas: Franklin Coxworthy, Roberto Mantovani, William Henry Pickering and Frank Bursley Taylor. In addition, Eduard Suess had proposed a supercontinent Gondwana in 1885 and the Tethys Ocean in 1893, assuming a land-bridge between the present continents submerged in the form of a geosyncline, and John Perry had written an 1895 paper proposing that the earth’s interior was fluid, and disagreeing with Lord Kelvin on the age of the earth.

For example: the similarity of southern continent geological formations had led Roberto Mantovani to conjecture in 1889 and 1909 that all the continents had once been joined into a supercontinent; Wegener noted the similarity of Mantovani’s and his own maps of the former positions of the southern continents. In Mantovani’s conjecture, this continent broke due to volcanic activity caused by thermal expansion, and the new continents drifted away from each other because of further expansion of the rip-zones, where the oceans now lie. This led Mantovani to propose an Expanding Earth theory which has since been shown to be incorrect.

Continental drift without expansion was proposed by Frank Bursley Taylor, who suggested in 1908 that the continents were moved into their present positions by a process of “continental creep”. In a later paper he proposed that this occurred by their being dragged towards the equator by tidal forces during the hypothesized capture of the moon in the Cretaceous, resulting in “general crustal creep” toward the equator. Although his proposed mechanism was wrong, he was the first to realize the insight that one of the effects of continental motion would be the formation of mountains, and attributed the formation of the Himalayas to the collision between the Indian subcontinent with Asia. Wegener said that of all those theories, Taylor’s, although not fully developed, had the most similarities to his own. In the mid-20th century, the theory of continental drift was referred to as the “Taylor-Wegener hypothesis”, although this terminology eventually fell out of common use.

Alfred Wegener first presented his hypothesis to the German Geological Society on 6 January 1912. His hypothesis was that the continents had once formed a single landmass, called Pangaea, before breaking apart and drifting to their present locations.

Wegener was the first to use the phrase “continental drift” and formally publish the hypothesis that the continents had somehow “drifted” apart. Although he presented much evidence for continental drift, he was unable to provide a convincing explanation for the physical processes which might have caused this drift. His suggestion that the continents had been pulled apart by the centrifugal pseudoforce of the Earth’s rotation or by a small component of astronomical precession was rejected, as calculations showed that the force was not sufficient. The Polflucht hypothesis was also studied by Paul Sophus Epstein in 1920 and found to be implausible.

The theory of continental drift was not accepted for many years. One problem was that a plausible driving force was missing. A second problem was that Wegener’s estimate of the velocity of continental motion, 250 cm/year, was implausibly high. It also did not help that Wegener was not a geologist. Other geologists also believed that the evidence that Wegener had provided was not sufficient. It is now accepted that the plates carrying the continents do move across the Earth’s surface, although not as fast as Wegener believed; ironically one of the chief outstanding questions is the one Wegener failed to resolve: what is the nature of the forces propelling the plates?

The British geologist Arthur Holmes championed the theory of continental drift at a time when it was deeply unfashionable. He proposed in 1931 that the Earth’s mantle contained convection cells which dissipated radioactive heat and moved the crust at the surface. His Principles of Physical Geology, ending with a chapter on continental drift, was published in 1944.

Geological maps of the time showed huge land bridges spanning the Atlantic and Indian oceans to account for the similarities of fauna and flora and the divisions of the Asian continent in the Permian era but failing to account for glaciation in India, Australia and South Africa.

Geophysicist Jack Oliver is credited with providing seismologic evidence supporting plate tectonics which encompassed and superseded continental drift with the article “Seismology and the New Global Tectonics”, published in 1968, using data collected from seismologic stations, including those he set up in the South Pacific.

It is now known that there are two kinds of crust: continental crust and oceanic crust. Continental crust is inherently lighter and its composition is different from oceanic crust, but both kinds reside above a much deeper “plastic” mantle. Oceanic crust is created at spreading centers, and this, along with subduction, drives the system of plates in a chaotic manner, resulting in continuous orogeny and areas of isostatic imbalance. The theory of plate tectonics explains all this, including the movement of the continents, better than Wegener’s theory.

6 January 2001

The US Congress certifies George W Bush winner of 2000 presidential elections.

On this day in 2001, more than five weeks after balloting ended, Vice President Al Gore, the 2000 Democratic presidential nominee, presided over a joint session of Congress that certified George W. Bush of Texas, the Republican nominee, as the winner. The disputed outcome in Florida caused the delay. It was resolved when the U.S. Supreme Court ruled, 5-4, on Dec. 12 to halt a statewide manual recount of the ballots ordered, in a 4-3 vote, by the Florida Supreme Court.

Bush’s margin of victory at that point was less than one half of one percent. The high court’s ruling gave him Florida’s 25 electoral votes. That, in turn, gave him 271 votes to Gore’s 266 — one more than the 270 required to be declared the winner. It paved the way for Bush to take the oath of office on Jan. 20, 2001, thereby becoming the nation’s 43rd president.

Although Gore finished second in the electoral vote, he received 543,895 more popular votes than Bush. This marked the fourth election in U.S. history in which the winner failed to get a plurality of the popular vote. The others were the elections of 1824, 1876 and 1888.

Gore failed to win the popular vote in his home state, Tennessee, which both he and his father had represented in the Senate, making him the first major-party presidential candidate to have lost his home state since Democrat George McGovern lost South Dakota in 1972.

Furthermore, Gore lost West Virginia, a state that had voted Republican only once in the previous six presidential elections. He also lost Arkansas, the home state of two-term President Bill Clinton, after having largely shunned Clinton’s help during his own presidential campaign. A victory in any one of those three states would have given Gore enough electoral votes to win the presidency without Florida.

Bush lost Connecticut, the state of his birth. He was also the first Republican to win the presidency without winning Vermont or Illinois, the second Republican to win the presidency without winning California — James A. Garfield in 1880 was the first — and the only victorious Republican to fail to receive any electoral votes from California.

6 January 1721

The Committee of Inquiry on the South Sea Bubble publishes its findings.

The South Sea Bubble of 1720 was one of the first but by no means the last or the worst of capitalism’s great bubbles. As with all the others, it made some rich and impoverished many. In a single year, obsessive trading in the stocks of Britain’s South Sea Company increased the price from just over £100 to almost £1,000 per share. Before 1720 was out, the price had plunged to well below its starting-point.

The South Sea Company, founded to consolidate and reduce state debt and to have a monopoly trade in the South Seas – the Spanish-controlled territory of Latin America had managed to disguise the fact that it could not turn a profit on either venture. The former because the dividend returns promised to investors outstripped the interest the Crown was prepared to pay. The latter because, for most of the life of the South Sea Company, Britain was at war with Spain and – consequently – the chances that Spain would grant extensive trade rights within its own sphere of influence to a British company were, shall we say, remote. The bubble brought share trading into disrepute. Traders and investors alike were seen as venal and corrupt, seeking something for nothing – the solid something reflected in the bubble’s shimmering surface.