The volcanic activity is related to the heat flow, explains Leone, though the degree of volcanic activity could be varied in the simulation and influenced by the strength of the impact. The model's calculations closely match previous calculations and mineralogical explorations. After a billion years, the heat flow was only one-tenth its initial value, which was too low to maintain even the volcanism. The model also demonstrates why it ceased: a sharp decrease in heat flow from the core into the mantle and the crust in the first 400 million years after the impact. The date calculated by the model corresponds to around 4.1 billion years ago, a figure previously proven by other scientists. Lastly, the model developed by the ETH researchers confirmed the date on which the magnetic field on Mars ceased to exist. One condition, however, is that the celestial body impacting Mars consist of 80 per cent iron when the researchers simulated the impact with a celestial body made of pure silicate rock, the resulting image did not correspond to the reality of the dichotomy. And he goes on to explain that the model - depending on the composition of the impact body chosen - is a virtually perfect representation of the size and shape of the hemispheres. Their simulation was also able to reproduce the different topographies of the two hemispheres in an extremely realistic manner, says Leone. According to the researcher, no other model has been able to portray or explain this distribution before. "Our model is an almost identical depiction of the actual distribution of volcanic identity," asserts Leone. The volcanoes on Mars are very unevenly distributed: they are common and widespread on the southern hemisphere, but are rare and limited to only a few small regions in the northern hemisphere. This theory did not convince Leone: "Our scenarios more closely reflect a range of observations about Mars than the theory of a northern hemisphere impact," states Leone. In 2008 a different team revived this idea and published it once again in Nature. They postulated that a large celestial object struck the Martian north pole. The most important theory about the origin of the Mars dichotomy was formulated by two American researchers in 1984 in an article in the journal Nature. Volcanic activity and topography modelled under realistic conditionsĮarlier theories posited the opposite, namely that there must have been a gigantic impact or many smaller strikes against the northern hemisphere. In the model, the researchers found that activity on Mars died down after around three billion years, after which time the Red Planet experienced neither volcanic activity nor a magnetic field - this is consistent with observations and measurements. Mantle plumes are magma columns that transport liquid material from the mantle to the surface. Around the equator in particular, numerous mantle plumes were generated as a consequence of the impact, which migrated to the south pole where they ended. But the simulation also found that it triggered strong volcanic activity lasting three billion years. When the celestial object impacted, it added more mass to Mars, particularly iron. And, just like the popular dessert, hiding beneath the surface was a liquid interior. Mars' crust must have been very thin at that time, like the hard, caramelised surface of a crème brûlée. The event is estimated to have occurred around 4 to 15 million years after the Red Planet was formed. In their simulation, the researchers assumed that the celestial body consisted to a large degree of iron, had a radius of at least 1,600 kilometres, and crashed into Mars at a speed of five kilometres per second. Volcanic activity over three billion years The molten rock eventually solidified into the mountainous highlands that today comprise the southern hemisphere of Mars. The celestial body that struck Mars must have been at least one-tenth the mass of Mars to be able to unleash enough energy to create this magma ocean. Their simulation shows that this impact generated so much energy that it created a magma ocean, which would have extended across what is today's southern hemisphere. Using a computer model, the scientists have concluded that a large celestial object must have smashed into the Martian south pole in the early history of the Solar System. Leone is the lead author of a paper recently published in the journal Geophysical Research Letters. ETH Zurich geophysicists under Giovanni Leone are now providing a new explanation. Although theories and assumptions about the origin of this so-called and often-discussed Mars dichotomy abound, there are very few definitive answers. Non-volcanic, flat lowlands characterise the northern hemisphere, while highlands punctuated by countless volcanoes extend across the southern hemisphere. The two hemispheres of Mars are more different from any other planet in our solar system.
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