The surface of our planet varies greatly in altitude. In fact about ¾ are covered by seawater, whose average level has been conventionally chosen as a reference for the surface elevations. The statistical analysis of the elevations of the earth’s surface shows us something interesting: the highest percentage of the elevations is around two particular values that are the average level of the ocean floor (about -3790) and the average level of the emerged lands (about 840 m).
On the relative graph of the percentage distribution of the areas with respect to the altitudes, called “hypsographic curve”, it can be noted that the portions of surface that reach the minimum altitudes (about -11000 m of the Mariana Trench) and the maximum ones (8850 m of Mount Everest) are a very small fraction of the total.
In a nutshell, the mountain ranges are almost an exception, as are the oceanic trenches, on the surface of the Earth. They appear in so-called belts, which are considerably more developed in one direction than in the other. But what is it that keeps them standing at such exceptional altitudes compared to most of the land above ground?



A friend of mine once shared me a link to a press release from the webpage of the Italian edition of Scientific American. The source was the National Institute of Nuclear Physics (INFN). The headline: “Geoneutrinos confirm that we are resting on a mantle of uranium and thorium.” I imagine any geologist would frown a bit at this statement. Why? Because the mantle is not made of uranium and thorium. Plus, this research had not found out that the mantle is composed of uranium and thorium. The research confirmed that most of the Earth’s internal heat comes from the decay of radioactive elements widespread not only in the crust (as already well known) but also in the mantle. Geoneutrinos are subatomic particles, a byproduct of radioactive decay (while neutrinos come form stars for fairly similar reasons).