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Ocean Mapping

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                                                     Ocean Mapping It's crazy to think that we don't have a complete picture of the planet," a researcher involved in a project to map the world's oceans by 2030 told Live Science. Humans have explored an incredible variety of strange and harsh environments - from the frozen surface of Antarctica to the unforgiving surface of the moon. But there may be one place right under our noses that holds a complete mystery: the bottom of the ocean. Most of the deep sea has not been seen by human eyes or perhaps mapped as it should be, and in fact the great fathers of the sea have not been found. So how many tons of ocean have we explored? It depends on how you define "find yourself". The first step of exploration is mapping — truly plotting out the shape of the seafloor, Vicki Ferrini, a geoscientist at Columbia University, knowledgeable Live Science. And as of mid-2023, we've got first-class mapped approximately 1

Chandrayaan-4: The next step in ISRO's lunar exploration

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                        Chandrayaan-4: The next step in ISRO's lunar exploration ISRO and JAXA are planning a joint lunar mission called the Lunar Pole Exploration Mission (LUPEX), also called the Chandrayaan-4 mission after the successful Chandrayaan-3 mission. Chandrayaan-4 Mission In order to release the Lunar Polar Exploration Mission (LUPEX), also called the Chandryaan-4 Mission, the Indian Space Research Organization (ISRO) and the Japan Aerospace Exploration Agency (JAXA) have teamed collectively. In 2026, the Indian Space Agency (ISRO) and Japanese Space Entity (JAXA) aim to launch the Chandryaan-4 Mission after the a hit touchdown of the Chandrayaan-three moon challenge, with this project India attained astounding accomplishment inside the Space Program.   The discovery of water at the moon could drastically affect space exploration inside the destiny and offer a critical resource for maintaining human presence on Earth’s lunar neighbour. The LUPEX is prepared to set n

Researchers accurate overestimates with ‘hot model’ climate predictions of rising temperatures in China

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  Researchers accurate overestimates with ‘hot model’ climate predictions of rising temperatures in China Changes in temperature sensitivity and temperature extremes in the vicinity of extreme hot climates have been widely observed. A subset of CMIP6 climate models, called "warm models," projected more warming due to greenhouse gases. The mean and extreme warming over China related to global surface air temperature (GSAT) warming. Credit: Geophysical Research Letters (2023). However, researchers at the Institute of Atmospheric Physics (IAP) of the Chinese Academy of Sciences (CAS) and the Pacific Northwest National Lab in the U.S. They found that the "warmer" climate model was overstating the warming of China. They propose a new way to fix this problem, can change the climate and mitigation strategies. They advanced an effective emergency prevention device in steps. First, they adjusted projections of destiny warming using latest worldwide warming. Next, they adjust

Scientists endorse awesome-vibrant mild sources powered by means of quasiparticles

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  Scientists endorse awesome-vibrant mild sources powered by means of quasiparticles Scientists studied the unique properties of quasiparticles in plasmas by running advanced computer simulations on supercomputers available through the European High-Performance Computing Joint Undertaking. They propose using quasiparticles to create light sources as powerful as the most advanced ones in existence today, but much smaller.  A global team of scientists is rethinking the primary concepts of radiation physics with the purpose of creating remarkable-brilliant light assets. In a new have a look at published in Nature Photonics, researchers from the Instituto Superior Técnico (IST) in Portugal, the University of Rochester, the University of California, Los Angeles, and Laboratoire d'Optique Appliquée in France proposed methods to use quasiparticles to create light assets as effective because the most superior ones in lifestyles nowadays, but an awful lot smaller. Quasiparticles are shaped

Abundant evidence of the Earth's core moving has been found at Baffin Island

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       Abundant evidence of the Earth's core moving has been found at Baffin Island A joint team of scientists from the Woods Hole Oceanographic Institution and the California Institute of Technology observed evidence of high levels of helium-three in rocks on Baffin Island—potential evidence that the Earth's core is leaking. In their paper published in the journal Nature, the organization describes their observations of helium-3 and helium-4 in the Canadian Arctic Archipelago. Early researchers saw helium-3 elements in lava flows on Baffin Island, suggesting a possible leak from the Earth's core. This is due to the fact that it is an old isotope - it changed conditions over time as the Earth formed and was trapped in the core. But due to its nature, helium-3 that makes its way to the ground quickly escapes into the atmosphere and disappears into space. Thus, helium-three is rare. If it is found on the surface, the percentage is high enough that it has made its way out of t

The discovery of lithium in a US volcano may be the largest deposit ever discovered

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The discovery of lithium in a US volcano may be the largest deposit ever discovered World-class lithium reserves along the Nevada-Oregon border could meet growing demand for the metal, according to a new study. It is estimated that 20 to 40 million tons of lithium ore are contained in volcanic craters that erupted about 16 million years ago. This compares with the lithium deposits beneath Bolivia’s thin salt deposits, formerly considered the world’s largest reserves. But Native Americans, to whom the area is sacred and believe it was the site of an 1865 massacre, are competing for a mining site Anauk Borst, a geologist at KU Leuven University and the Royal Museum of Central Africa in Tervuren, Belgium, says: 'If you consider their surface lithium reserves, this is a very, very , significant lithium deposit on price, security of supply , and geopolitics.' Further analysis of the site indicates that the craters of the volcano, an unusual clay composed of the mineral illite, conta

The True Story Behind "Fool's Gold"-Pyrite

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             The True Story Behind "Fool's Gold"-Pyrite “Fool’s Gold” is technically referred to as pyrite or iron sulfide (FeS2) and is one of the maximum not unusual sulfide minerals. Sulfide minerals are a set of inorganic compounds containing sulfur and one or more elements. Minerals are defined through the manner of their chemistry and crystalline shape. Minerals which have the equal chemical composition however distinct crystal systems are known as polymorphs. Pyrite and marcasite, for instance, are polymorphs due to the fact they'll be both iron sulfide, but each has a amazing structure. Minerals also can have the identical crystalline structure however specific elemental compositions, but it’s the crystal shape that determines the mineral’s bodily traits. In addition to pyrite, commonplace sulfides are chalcopyrite (copper iron sulfide), pentlandite (nickel iron sulfide), and galena (lead sulfide). The sulfide beauty additionally consists of the selenides, the

How the Greenland ice sheet can nevertheless be stored

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                   How the Greenland ice sheet can nevertheless be stored Greenland is the world's second largest landmass covered by ice; only Antarctica is bigger. The Greenland ice sheet is greatly affected by the effects of climate change. If the ice melts completely it could cause a sea level rise of more than seven meters - a disaster for coastal areas around the world and for those who live there. Time series of ice volume and spatial extents of the GrIS for warming scenarios without mitigation. a, Sketch of applied warming and cooling scenarios in this study. The warming period lasts for 100 years, followed by varying cooling phases. The black line corresponds to scenarios without mitigation as shown in this figure. b, Evolution of total GrIS ice volume simulated by PISM-dEBM, without reversal of the temperature anomalies (black line in panel a), for different temperature anomalies between ΔTJJA = 0 °C and 7.0 °C above present. The warming period lasts for 100 years until y

New styles in sun's layers should assist scientists remedy sun mystery

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                    New styles in sun's layers should assist scientists remedy sun mystery Astronomers are one step in the direction of expertise in one of the maximum enduring solar mysteries, having captured extraordinary facts from the sun's magnetic subject. Small-scale magnetic structures of the ‘quiet sun’ at high resolution His groundbreaking data accrued from the US National Science Foundation's (NSF) Daniel K Inouye Solar Telescope (DKIST) in Hawaii—the most effective sun telescope in the international—has provided the most exact representations thus far of the magnetic discipline of the so-referred to as 'quiet' floor of the sun.   An international team of scientists, which include researchers from the University of Sheffield, believe the facts have implications for the way we model power transfer among the layers of the solar system. The research has been posted in Astrophysical Journal Letters. This may assist give an explanation for one of the biggest c

Earth's plate tectonics these days underwent a fundamental trade-A New Proof

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  Earth's plate tectonics these days underwent a fundamental trade-A New Proof Sampling of a primordial mantle reservoir by mantle plume as evidenced by Ti and Sr isotopic records of the modern OIBs from the Iceland, Samoa and Caroline hotspots. Data of the OIB samples from Cape Verde and Azores in ref. 3 are shown as white circles. The N-MORB and E-MORB samples from refs. 3,4 are shown, for which the N-MORB samples without available Sr isotope data have been assumed to have 87Sr/86Sr = 0.7025. The dotted pink trajectories describe the effects from mixing in increments of 0.2% the ancient marine sediments or continental crust material with δ49Ti = +0.200‰ (refs. 5,6) and 87Sr/86Sr = 0.740 (ref. 47) into a modern depleted MORB mantle source with 87Sr/86Sr = 0.7025 (ref. 63) and δ49Ti = +0.001‰ (refs. 3,4) or into a mantle source with 87Sr/86Sr = 0.7035 and a primordial mantle δ49Ti of +0.052‰. Addition of recycled melting residues would lead to lower δ49Ti values in N-MORBs and some

Rediscovery of Pontus: Geologists discover the remains of a long-lost tectonic plate 1/4 the size of the Pacific Ocean!

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  Rediscovery of Pontus: Geologists discover the remains of a long-lost tectonic plate 1/4 the size of the Pacific Ocean! In Earth’s lengthy history of over 4.5 billion years, there are numerous threads that we’re yet to entangle. One such ginormous thread has recently been undone, adding a new bankruptcy to our planet’s geological records.    Scientists have successfully exposed another lengthy-lost secret of our planet: a huge tectonic plate that becomes as soon as one-quarter the dimensions of the Pacific Ocean! Suzanna van de Lagemaat, a geologist from Utrecht University, reconstructed a huge and previously unknown tectonic plate named Pontus at the same time as exploring the planet's maximum complex plate tectonic place — the place across the Philippines. This discovery was made viable by way of piecing together fragments of antique tectonic plates, located deep in Earth's mantle, throughout the mountain levels in Japan, Borneo, the Philippines, New Guinea and New Zealan

Why don’t rocks burn?

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                                              Why don’t rocks burn? While many rocks don’t burn, a number of them do. It depends on what the rocks are made from – and that’s associated with how they were shaped.   There are three important rock sorts: igneous, sedimentary and metamorphic. These rocks are products of minerals that each one has one-of-a-kind characteristics. Some will soften into magma or lava – splendid-hot, liquid rock – whilst they're uncovered to heat. Others will catch fire. Rocks can appear alike, but one rock isn't like some other.    Rocks that burn after they get heated up are combusting. This way, elements in the rocks are reacting with oxygen within the air to supply warmth and light, in the form of flames. The factors sulphur, carbon and hydrogen effortlessly react with oxygen. Rocks that contain those elements are flammable. Without those elements inside them, rocks that are exposed to sufficient heat will melt as opposed to catching fire.