What happened to lunar volcanoes

An asteroid impact on the Moon started a fragment of the satellite surface and threw it into space. After a trip of thousands of years, the meteorite fell in northwest Africa, where it was discovered in February 2023. After two years of studies, it has helped cover a hole of one billion years in the lunar geological history. Context. Apollo missions brought 382 kg of lunar rocks to Earth. The analysis of these rocks told us that the moon had had a violent volcanic past, but that its inner fire had turned off about 3,000 million years ago. A much more recent mission, Chang’e 5, brought younger basalts, “barely” 2,000 million years. This still leaves us a huge hole of almost one billion years of lunar history in which we do not know what happened. Did volcanism go out and reactivated? The answer came to us. And it has arrived, as so many times in science, by chance. A lunar rock found in the Norafricano desert in 2023 has turned out to be the piece that was missing in the puzzle. He NWA 16286 Meteorite Analysispresented at the Goldschmidt conference in Prague, suggests that lunar volcanism was a much more continuous process than we thought. The lunar meteorite number 31. The protagonist of this story is a piece of soil of the moon of 311 grams, one of the only 31 lunar basalt meteorites officially identified on our planet. It was not brought by any astronaut or any probe, but reached the earth by its own foot. An asteroid impact on the moon started it from the satellite surface and threw it into space. After a trip of thousands of years, he fell in northwest Africa, where he was discovered in February 2023. Studying the rocks that the moon sends us for free is an incredibly valuable way to explore its geology, because the rocks of the sampling return missions are limited to the immediate areas of the places chosen for the moon landing. Lunar meteorites can be expelled from anywhere from the moon surface. There is a lot of serendipia in this sample. The missing piece. But the true importance of NWA 16286 resides in his age. He Lead isotope analysis He has dated the rock in about 2,350 million years. This makes it the youngest lunar basaltic meteorite ever discovered, and places it within that mysterious hole of one billion years in lunar volcanic history. The samples of NASA and Luna’s Apollo missions of the Soviet Union are between 3,100 and 4,000 million years. Those of the Chinese Chang’e-6 mission (from the hidden face of the moon) They are about 2,830 million years. Chinese mission shows Chang’e-5 (from the visible face of the moon) are about 2,030 million years. NWA 16286 is in the middle. Volcanic activity did not stop. The characteristics of the meteorite suggest that Lunar volcanic activity continued Throughout that time: the moon was not geologically dead. It is a basalt rich in olivine with unusually high levels of potassium. In addition, its “fingerprint” lead isotopic pointed out that it was formed from a source in the lunar mantle with a very high proportion of uranium-plaomo. Potassium and uranium are radioactive elements, as is the thorium. Its disintegration along eons generates a constant amount of heat. The theory, now reinforced by this rock, is that lunar mantle bags enriched in these elements acted as a residual heat engine that maintained parts of the interior of the moon hot enough to produce magma and feed volcanoes much after what was thought. What part of the moon came from? NWA 16286 has a different lithology from any known meteorite. It is believed that it came from a lunar sea so far not sampled. Its texture suggests a two -stage cooling story: a slow, perhaps in a magma camera, followed by an eruption in a lava flow of several tens of meters thick. This rock not only resolves an old mystery, but also serves as a guide. Analyzing their trajectory and composition will help scientists identify the crater of origin on the moon, marking a priority point of interest for future sampling return missions. And so is how a rock found in the desert is telling us where we have to go the next time we visit the moon. Image | SM BELARDO et al. In Xataka | There is a silent career to get the moon waves: dozens of companies have claimed part of their spectrum

In 2021 a volcano spent three days in eruption without anyone finding out. Now it helps us ahead of the silent volcanoes

Knowing how to read the signals that a volcano gives before erupting can make a difference between a scare and a tragedy. Some volcanoes make it easy for experts who know how to read these clues but others erupt without prior notice. Or maybe just we couldn’t decipher your signs. At least until now. A new tool. A team of researchers He has devised A new mechanism to model the behavior of some volcanoes. This tool, its creators stand out, will serve to more effectively monitor the eruptions of some volcanoes reducing the risk associated with these natural phenomena often so violent. Some special usefulness in the case of “silent” volcanoes. “Despite great advances in monitoring, some volcanoes erupt with minimally detectable or even without them precursors, significantly increasing the risk of nearby populations,” pointed in a press release Yuyu Li, co -author of the study. As explained by LI herself, some of these volcanoes are located not only near communities, also near important air traffic routes. Silent volcanoes. For the development of its tool, the team resorted to the Veniaminaf volcano, located in the North American state of Alaska. This is one of the so -called “silent” volcanoes, volcanoes whose eruption is not preceded by the signals that are generally associated with an imminent or close eruption, such as earthquakes or the deformation of the soil in the surroundings of the Magma Chamber. Veniaminof’s is just an example that We can find In this family of silent volcanoes that also includes some closer such as Stromboli in Italy or Popocatepetl in Mexico. Looking inside the volcano. But among all of them, the Veniaminof volcano is perhaps the most paradigmatic. Not because only two of the 13 rashes that have leaded since 1993 have been planned, but because in 2021 he achieved the milestone of erupting without anyone noticing Until three days later. The team responsible for the study analyzed the internal conditions that make it a silent volcano. Factors such as a slow supply of magma and a warm host rock are key in this regard. The monitoring of the volcano was carried out for three summers prior to one of the silent eruptions of the volcano, that of 2018. A model to get ahead of the eruption. The result, a model that conforms to the state of different variables that can condition the probability of the burst of the magma, such as the volume of the reserve, flow conditions of the magna, depth of the reserve or the form that it acquires is. Thus they could estimate what kind of conditions could be linked to a silent eruption and which ones were not. The team found that soil deformation could help prevent some eruptions of the volcano but that the relationship between underground magma and rashes were somewhat more complex than it might seem. The details of the study have been published In an article In the magazine Frontiers in Earth Science. The following steps. Monitoring the numerous silent volcanoes distributed throughout the world will not be an easy task. For now, the resolution gives a clue to what are the volcanoes to monitor more closely: volcanoes with small and warm reserves and slow magma flows, explains the team. In Xataka | In 2021 a volcano spent three days in eruption without anyone finding out. Now it helps us to unmask the silent volcanoes Image | Alaska Volcano Observatory Photo Gallery

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