Tag: asteroids

  • Can we spot every incoming asteroid before they hit Earth?

    Can we spot every incoming asteroid before they hit Earth?

    [ad_1]

    Asteroid 2024 RW1 seen over the Philippines

    Allan Madelar/Facebook

    The surprise discovery of asteroid 2024 RW1, mere hours before it hit Earth harmlessly this week, may have you wondering whether we are at risk of larger space rocks coming out of nowhere and wreaking devastation. Thankfully, our ability to track asteroids is on the rise, even if we can’t catch them all.

    “We believe we know more than 90 per cent of the asteroids that are about one kilometre in size, where one kilometre is considered, not a planet killer, but something that would destroy a whole region or a whole continent,” says Ian Carnelli at…

    [ad_2]

    Source link

  • Asteroid CAQTDL2 is about to hit Earth – but don’t worry, it is only small

    Asteroid CAQTDL2 is about to hit Earth – but don’t worry, it is only small

    [ad_1]

    The predicted path of asteroid CAQTDL2 over the Philippines

    Catalina Sky Survey/ESA

    Astronomers have just discovered that an asteroid is about to strike Earth at thousands of kilometres per hour, impacting just east of the Philippines and most likely in the sea. Thankfully, the relatively small object poses no harm and will burn up in the atmosphere in a fireball.

    The asteroid, which is estimated to be roughly 1 metre across, was spotted earlier today by the NASA-funded Catalina Sky Survey and given the designation CAQTDL2. It is due to strike Earth at around 1645 GMT, or 1745 London…

    [ad_2]

    Source link

  • 2024 RW1: A small asteroid hit Earth and burned up over the Philippines

    2024 RW1: A small asteroid hit Earth and burned up over the Philippines

    [ad_1]

    The predicted path of asteroid CAQTDL2 over the Philippines

    Catalina Sky Survey/ESA

    An asteroid hit Earth and burned up in the atmosphere just east of the Philippines. It was discovered by astronomers only hours before it streaked across the sky in a bright fireball, but went unseen by many on the ground as the view was obscured by cloudy weather produced by Typhoon Enteng.

    The asteroid, which is estimated to be roughly 1 metre across, was spotted earlier today by the NASA-funded Catalina Sky Survey and initially given the designation CAQTDL2, before being named 2024 RW1.

    As predicted, the asteroid struck Earth around 1645 GMT, or 1745 London time, 1245 New York time and 0045 local time just east of the northernmost island of the Philippine archipelago. It was expected to hit at a speed of 17.6 kilometres per second, or 63,360 kilometres per hour, which Alan Fitzsimmons at Queen’s University Belfast in the UK says is about average for such objects. “Don’t be fooled by Hollywood movies where you can see the thing coming screaming through the sky and you’ve got time to run out the house, get the cat, jump in the car and drive somewhere. You don’t have the time to do that,” he says.

    The asteroid CAQTDL2 is visible moving across the sky within the purple circle

    Catalina Sky Survey

    Fortunately, there was no need for an evacuation: NASA’s Planetary Defense Coordination Office posted on social media that the asteroid “safely impacted Earth’s atmosphere”.

    “An object this small can’t do any damage on the ground. We’re protected from them by the Earth’s atmosphere,” says Fitzsimmons. A video shared on social media shot from the province of Cagayan at the northern tip of the Philippines shows a flickering green fireball appear behind the clouds, followed by an orange tail, which disappeared just seconds later.

    Fitzsimmons says that two or three objects this size strike Earth every year and that we are increasingly able to spot them early, with the first incoming asteroid being detected by astronomers before landing in 2008. 2024 RW1 is the ninth accurately predicted asteroid strike on Earth.

    “The really positive aspect about this is that the survey telescopes are now good enough to spot these things coming in and give us a bit of warning,” he says. “Put another way, if this object had been much larger and so perhaps pose a threat to people on the ground, then it would be much brighter, and we’d have projected it much further out. So this actually is a really nice demonstration that the current survey systems are doing a very good job. We’re probably averaging about one small asteroid detected before it hits the atmosphere every year now, and the survey systems are only getting better.”

    Not only is Earth developing and improving its early warning system, but in 2022 NASA’s Double Asteroid Redirection Test (DART) spacecraft proved that we have a chance of saving the planet from a catastrophic impact of a larger object. DART crashed into the 160-metre-wide moonlet Dimorphos and slowed it slightly, demonstrating that, in theory, we could avert such a disaster. Next month, the European Space Agency is due to launch its Hera mission to study the results of the impact up close, and further improve our understanding of planetary defence.

    Topics:



    [ad_2]

    Source link

  • Huge asteroid impact may have knocked over Jupiter’s largest moon

    Huge asteroid impact may have knocked over Jupiter’s largest moon

    [ad_1]

    The solar system’s largest moon, Ganymede, alongside Jupiter in a picture taken by NASA’s Cassini spacecraft

    NASA/JPL/University of Arizona

    A massive collision billions of years ago may have dramatically reoriented Ganymede, Jupiter’s largest moon.

    Naoyuki Hirata at Kobe University, Japan, and his colleagues studied Ganymede’s extensive furrow system, a series of concentric troughs believed to be remnants of the largest impact structure in the outer solar system.

    The centre of the furrow system aligns closely with Ganymede’s tidal axis – the imaginary line running to Jupiter from the centre of the moon’s side that always faces its planet. This led the researchers to suggest that the impact that formed the furrows caused a significant redistribution of mass that reoriented the moon.

    Through simulations, the researchers determined that the impactor responsible probably had a diameter of about 150 kilometres ­– significantly larger than the one that caused the extinction of the dinosaurs on Earth, which is estimated to have had a diameter of about 10 kilometres.

    Andrew Dombard at the University of Illinois Chicago says that if an asteroid like that hit Earth, “it would be a global sterilising event, a bad day”.

    Upon impact, this asteroid would have breached Ganymede’s icy crust into the liquid oceans below, creating a transient crater and hurling vast amounts of material across the moon’s surface.

    As this settled, it would have formed a thick blanket of ejecta around the impact site, creating a region where gravity is stronger due to the extra mass. Over time, this anomaly would cause Ganymede to reorient, aligning the impact site with its tidal axis, the simulation showed.

    Furrows on Ganymede are thought to be remnants of an ancient impact structure

    NASA/JPL/Brown University

    Hirata’s team compared this process with an event on Pluto, where a large impact created a basin called Sputnik Planitia, leading to a reorientation of the dwarf planet.

    However, although it is likely that the Ganymede impact significantly affected the moon’s early history, estimating the size of the object that hit it is complicated because we lack good data on the gravity and topography of this frigid world, says Hirata.

    Dombard says the model used in the paper doesn’t account for some of the complexities of Ganymede’s unique icy structure. “I think it is very good for establishing that this process could occur, but I don’t necessarily trust the numbers,” he says.

    Topics:

    [ad_2]

    Source link

  • Dinosaur-killing Chicxulub asteroid formed in Solar System’s outer reaches

    Dinosaur-killing Chicxulub asteroid formed in Solar System’s outer reaches

    [ad_1]

    Artist impression of a large asteroid hitting Earth.

    The impact from the Chicxulub asteroid (illustration) caused a mass extinction 66 million years ago.Credit: Illustration by Mark Garlick

    The object that smashed into Earth and kick-started the extinction that wiped out almost all dinosaurs 66 million years ago was an asteroid that originally formed beyond the orbit of Jupiter, according to geochemical evidence from the impact site in Chicxulub, Mexico.

    The findings, published on 15 August in Science1, suggest that the mass extinction was the result of a train of events that began during the birth of the Solar System. Scientists had long suspected that the Chicxulub impactor, as it is known, was an asteroid from the outer Solar System, and these observations bolster the case.

    The Cretaceous/Palaeogene (K/Pg) extinction was the fifth in a series of mass extinctions that have occurred during the past 540 million years or so: the period in which animals have spread around Earth. The event wiped out more than 60% of species, including all non-avian dinosaurs.

    Since 1980, evidence has accumulated that the extinction was caused by a city-sized object hitting Earth. Such an impact would have thrown huge volumes of sulfur, dust and soot into the air, partially blocking out the Sun and causing temperatures to plummet. A layer of iridium metal, which is rare on Earth but more common in asteroids, was deposited all over the planet around the time the extinction began. And in the 1990s, scientists described2 the impact site, a huge buried crater near Chicxulub on Mexico’s Yucatán Peninsula.

    “We wanted to identify the origin of this impactor,” says Mario Fischer-Gödde, an isotope geochemist at the University of Cologne in Germany. To find out what the object was and where it came from, he and his colleagues obtained samples of K/Pg rocks from three sites, and compared them with rocks from eight other impact sites from the past 3.5 billion years.

    Ruthenium signature

    The team focused on isotopes of ruthenium metal. Ruthenium is extremely rare in Earth rocks, says Fischer-Gödde, so samples of it from an impact site offer “the pure signature” of the impactor. There are seven stable isotopes of ruthenium, and celestial bodies have characteristic blends of them.

    In particular, looking at ruthenium isotopes can help researchers to distinguish between asteroids that formed in the outer Solar System — beyond the orbit of Jupiter — and those with an origin in the inner Solar System. When the Solar System was forming from a molecular cloud around 4.5 billion years ago, temperatures in the inner region were too high for volatile chemicals such as water to condense. As a result, asteroids produced there had low levels of volatiles, and became rich in silicate minerals. Asteroids that formed further out became ‘carbonaceous’, containing lots of carbon and volatile chemicals. Ruthenium isotopes were unevenly distributed in the cloud, and this heterogeneity is preserved in asteroids.

    Fischer-Gödde’s team found that the ruthenium isotopes in the Chicxulub impactor were a good match for a carbonaceous asteroid from the outer Solar System, and did not match siliceous asteroids from the inner Solar System.

    Previous studies have also suggested that the impactor was a carbonaceous asteroid, says Sean Gulick, a geophysicist at the University of Texas at Austin. But the latest work “is a really elegant way to get at some of these same answers and get several of the same answers using one methodology”, he adds.

    Not a comet

    The ruthenium isotopes also provide evidence against another hypothesis: that the Chicxulub impactor was a comet rather than an asteroid. “The idea it was a comet goes back far into the literature,” says William Bottke, a planetary scientist at the Southwest Research Institute in Boulder, Colorado. The hypothesis was revived in a controversial 2021 study3, which argued that the impactor was part of a long-period comet that had broken up under the Sun’s gravitational pull.

    But Fischer-Gödde says the ruthenium-isotope data do not match a comet. Gulick agrees. He adds that geochemical evidence from the Chicxulub impact site has never been consistent with a comet, and the latest study “does a really good job of kind of nailing that home”.

    Bottke adds that the comet hypothesis also “runs into difficulty” when you consider the dynamics of the Solar System. “Sizeable carbonaceous asteroids are much more probable to hit the Earth than comets,” he says. In a 2021 study, he and his colleagues argued that the impactor probably came from the main asteroid belt, between Mars and Jupiter.

    Most of the other impactors that Fischer-Gödde’s team studied seem to have formed in the inner Solar System, according to their ruthenium isotopes. The only exceptions were the oldest ones, from between 3.2 billion and 3.5 billion years ago, which look more like the Chicxulub impactor. It could be that “something interesting was happening in the asteroid belt at that time, such as a large asteroid break-up in a good place to deliver objects to Earth”, says Bottke.

    [ad_2]

    Source link

  • A contact binary satellite of the asteroid (152830) Dinkinesh

    [ad_1]

    Observations

    The analysis presented here is based on panchromatic (350–850 nm) images taken with Lucy’s LOng Range Reconnaissance Imager, hereafter L’LORRI, which is a 20.8-cm, f/13 telescope feeding a 1,024 × 1,024-pixel CCD focal plane35. L’LORRI has a field of view of 0.29° and a pixel size of 5 µrad. It was primarily used in three distinct observation campaigns during the encounter. (1) Optical navigation reconstruction images were designed to precisely determine the trajectory of Lucy. They were taken daily during the period of ±4 days of encounter (tCA = −4 to +4 days) and every 15 min from tCA = −2 h to +2 h. (2) High-resolution close-approach images were taken every 15 s from tCA = −10 min to +9 min, then with 1-min cadence until +55 min. (3) Post-encounter light-curve photometry was acquired from tCA = +4 h to +95 h. Three exposures were taken at a cadence of 1 h. At this time, the Dinkinesh–Selam system was unresolved. To minimize data volume, these data were taken in L’LORRI’s so-called 4 × 4 mode, which bins the data by 4 × 4 pixels during the CCD readout.

    Light-curve analysis

    The orbital period of Selam and the rotational period of Dinkinesh can be determined using the post-encounter light-curve photometry described above in the ‘Observations’ section. Instrumental magnitudes of the system were extracted from the images using a 1.5-pixel-radius aperture. The small aperture served to exclude contamination from nearby stars. The formal errors from the extraction were scaled upward by a factor of 1.545 to adjust the reduced χ2 to be 1 before determining the final uncertainties on the fitted results. There were 267 images analysed.

    The data were compensated for the changing distance as well as correcting to a constant solar phase angle using a phase coefficient of 0.06 mag per °. The phase angle varied from 60.52° at the start to 59.67° at the end. The observing direction changed little over the 3.5 days and these corrections remove these slight changes, leaving only a record of the global photometric properties of the system. The resulting light curve is shown in Extended Data Fig. 1 in units of relative flux.

    We analysed the light curve with an iterative process designed to separate the contributions to the total flux from Dinkinesh and Selam. As the first step, a model was constructed that consisted of a Fourier series expansion of the light curve combined with a period for each object. The reference time for the rotational phase was arbitrarily set to the time of the first data point for both objects. The mean flux of Dinkinesh was a free parameter in the model. Also, we iteratively varied the Selam/Dinkinesh mean flux ratio. This ratio is constrained by the close-approach resolved images (Fig. 1d, for example), which show that the ratio of the visible areas of the two objects is 0.25. The two objects are also seen to have similar surface brightness, and so the unresolved flux ratio is also 0.25. This ratio was assumed to be at minimum light for both objects because Selam is viewed edge-on. An iterative correction was applied after separating the light curves to correct from the minimum to the mean flux and the final mean flux ratio was set at 0.33 (corresponding to a magnitude difference of 1.3).

    The model parameters were determined in a series of iterative steps. The first pass fit set a reasonable mean flux for Dinkinesh and the Fourier terms were disabled. At this point, only Selam was free to be adjusted to fit the data. The data were scanned in period. At each step, a best-fit Fourier series was computed and the χ2 was recorded. The lowest χ2 period gave a preliminary value of 51.76 h for Selam. This model was subtracted from the light-curve data and a similar scan was performed on the Dinkinesh-only data. The Dinkinesh scan returned two interesting minima in χ2 at periods of roughly 3.7 and 4.3 h. Note that all periods assume that the light curve is double-peaked.

    Given the two preliminary periods, the data were then fitted with the full model from the two objects and all free parameters were optimized simultaneously with an amoeba χ2 minimization (ref. 36 Chapter 10.4). Using the amoeba fit as the starting point with the a posteriori correction to the uncertainties, a second Markov chain Monte Carlo fit (see ref. 37) was run for the model. There were 18 data points that were excluded because of unreasonably large residuals (see the discussion below). The final fitted light curves revealed amplitudes of 0.82 mag for Selam and 0.25 mag for Dinkinesh.

    The Selam rotation period was determined to be 52.44 ± 0.14 h from this fit, but it is also attributed to its orbital period about Dinkinesh because it is probably tidally locked, as shown by the presence of mutual events. The resulting phased light curves are shown in Fig. 2.

    The variation in flux for the two objects coincidentally are about the same. Dinkinesh is much larger, which implies that it has a smaller relative variation in its flux. The light curve of Selam is well fit by two Fourier terms that capture the slightly asymmetric maximum and slightly broadened minima. The light curve of Dinkinesh is considerably more complicated; both the minima and maxima are asymmetric but there are also clearly higher-order variations seen. In this case, a four-term Fourier fit was required and even this does not fully capture all of the detail in the curve. For instance, one of the minima is sharper than can be followed with a four-term fit. The rotation period of Dinkinesh was determined to be 3.7387 ± 0.0013 h (the 4.3-h period discussed above was determined to be an alias).

    The outliers that were flagged during the light-curve fitting, which are shown in red in the figures, are also of interest because they occur at a coherent rotation phase following a similar time after the two light-curve minima for Selam. A reasonable explanation for these low points is a mutual event between the two bodies. These could, in general, be from the bodies occulting each other from the perspective of the spacecraft or from casting shadows on one another. Fortunately, the timing of these minima allows us to determine which.

    Looking at the photometry as a function of time, the low points appear at a regular interval at half the rotation period of Selam. Geometric constraints from the absolute timing indicate that the events are shadow transits of each other and not physical obscuration along the line of sight (occultations). Furthermore, the timing clearly indicates that the orbital motion of Selam is retrograde, as is true for the rotation of Dinkinesh as well. The first and third dips seen in time are inferior shadowing events, whereas the middle dip is a superior event. In the phased plot, the two inferior events overlay each other and trace out a more complete light curve of an event. The superior event has fewer measurements and shows an incomplete profile of the dip that misses the maximum eclipse point that must be in the middle between the two sets of points.

    Shape

    The digital shape model used for this study (see Fig. 3) was generated by applying classical stereophotogrammetry techniques (ref. 38 and references therein) to L’LORRI imagery. A total of 48 images with a best ground-sampling distance ranging from about 10 m per pixel to 2.2 m per pixel were chosen from the high-resolution close-approach images described in the ‘Observations’ section. These were used to establish a network of 3,000 control points, which served as an input for the bundle adjustment process. Further, thanks to the very good noise and sensitivity performance of the L’LORRI imager, and to its comparatively large field of view, we could identify about 20 catalogue field stars in the Dinkinesh fields throughout the encounter. These star positions were used in the determination of the stereophotogrammetric adjustment, and contributed considerably to stabilize the solution.

    As a result, the camera extrinsic matrices were determined, which describe the transformation between the camera’s and the body-fixed reference system. These transformation matrices were then used to triangulate surface points from homologous image points, which were derived by means of dense stereo matching39. The resulting dense point cloud (about 5 × 106 3D points) was then connected into a regular triangular mesh. The shape model derived from stereo reconstruction has an estimated scale error of about 1.4% and covers about 45% of the body’s surface. To produce a closed shape, and allow an estimation of the body volume, the unseen hemisphere has been approximated with an analytical solid figure. For this purpose, we chose a generalized super-ellipsoid40, whose implicit representation is given by the function

    $$1={\left|\frac{x}{a}\right|}^{k}+{\left|\frac{y}{b}\right|}^{m}+{\left|\frac{z}{c}\right|}^{n}$$

    in which x, y and z are the standard Cartesian coordinates. A fit to the reconstructed hemisphere leads to a = 0.40, b = 0.40, c = 0.35 km, k = m = 2 and n = 1.35. The generalized super-ellipsoid provides a better match to the ‘top’ shape of Dinkinesh than a conventional triaxial ellipsoid.

    We estimated the uncertainty in the volume of Dinkinesh from the difference between the shape model and the super-ellipsoid convex shell. For the hemisphere covered by imaging, the difference in volume is 4.7%. To be conservative, we round this and apply an arbitrary factor of two margin to arrive at the volume uncertainty of ±10%. This uncertainty is propagated to quantities derived from the volume. In particular, we note that the volume-equivalent radius of Dinkinesh is calculated as rveq = (3V/4π)1/3, rather than from direct distance measurements.

    The dimensions of the two lobes of Selam were found by fitting ellipses to orthogonal axes in several resolved images of Selam from different viewing angles. The inner lobe of Selam is fit with an ellipsoid measuring 240 × 200 × 200 m. The outer lobe is measured at 280 × 220 × 210 m. Uncertainties were estimated to be 10% per axis by adjusting the ellipsoidal fits until they were visually too large or too small to match the images. Combining the above values, we calculate a total system volume of Vtot = 2.06 ± 0.20 × 108 m3.

    Mass and density

    System density can be estimated from the orbital period and relative semimajor axis of the two bodies. As we describe in the main text, the centre-of-figure separation between Dinkinesh and Selam was 3.11 ± 0.05 km at the time of the fly-by. The eccentricity of Selam’s orbit is not directly derivable from existing data, although it can be constrained. The regular phasing of the light-curve minima collected before encounter from the ground14 and from Lucy (Fig. 2) is consistent with a near-circular orbit, given our inference (Fig. 2) that these minima are caused by mutual eclipses. We would expect the eccentricity of Selam to be near zero, given that tidal timescales for orbit circularization are on the order of 106–107 years. The ages of asteroid pairs for which one of the members of the pair has subsequently undergone a mass-shedding event leading to the formation of a satellite suggest that binary-YORP effects41 might shorten the circularization timescale to less than about 106 years (refs. 16,42). Thus we assume e = 0 in the analysis performed here. Ground-based light-curve observations, taken at several epochs, can better constrain any orbital eccentricity that might exist.

    Assuming that Selam is in a circular orbit about Dinkinesh and has an orbital period of 52.67 ± 0.04 h, we derive a system mass of 4.95 ± 0.25 × 1011 kg (GM = 33.0 ± 1.6 m3 s2) from Kepler’s third law. In the ‘Shape’ section, we calculate a total system volume of Vtot = 2.06 ± 0.20 × 108 m3. Combining the system mass and volume, we derive a bulk density of ρ = 2,400 ± 350 kg m3. We add the caveat that, if the assumption of zero eccentricity is incorrect and the separation observed at the time of the fly-by differs from the semimajor axis, it would introduce a systematic error into the calculation of density. Conversely, however, the range of likely density for an S-type asteroid, as discussed below, constrains the maximum eccentricity to be on the order of 0.1 and the assumption of zero eccentricity is fully consistent with known asteroid properties.

    Angular momentum

    Knowledge of the component masses and the spin state can be combined to calculate the angular momentum of the system. For simplicity, we assume that the moment of inertia of Dinkinesh can be adequately represented by a sphere of volume-equivalent radius. Assuming that Selam is tidally locked, the contribution to the angular momentum from its spin is small. Likewise, the orbital motion of Dinkinesh around the barycentre is small and we ignore it. The system angular momentum is nearly equally divided between the spin of Dinkinesh, Lspin = 11.2 ± 1.9 × 1012 kg m2 s1, and the orbital motion of Selam, Lorb = 8.0 ± 4.0 × 1012 kg m2 s1. The total angular momentum of the system is Lsys = 19.3 ± 4.4 × 1012 kg m2 s1. The normalized angular momentum, αL, is computed from the total system angular momentum divided by the angular momentum of a sphere containing the total mass of the system rotating at the maximum rate for a cohesionless rubble pile43. That rate is given by ωmax = (4πρG/3)1/2, corresponding to a spin period of Tmax = 2.13 h, that is, the observed main-belt spin barrier. We find αL = 0.88, consistent with that expected for a binary produced by fission26.

    [ad_2]

    Source link

  • Save the forest to save the tiger — why vegetation conservation matters

    Save the forest to save the tiger — why vegetation conservation matters

    [ad_1]

    Nature, Published online: 21 May 2024; doi:10.1038/d41586-024-01368-y

    The Royal Botanic Gardens, Kew, emphasizes the importance of conserving wild plant species, plus a wonderstruck sky-watcher spots a brilliant meteor, in the weekly dip into Nature’s archive.

    [ad_2]

    Source link

  • Asteroid that broke up over Berlin was fastest-spinning one ever seen

    Asteroid that broke up over Berlin was fastest-spinning one ever seen

    [ad_1]

    Long-exposure photo showing the trail of asteroid 2024 BX1 shortly before impact. The changes in brightness are caused by the asteroid’s spin

    L. Buzzi, Schiaparelli Astronomical Observatory, Italy (MPC 204)

    An asteroid that hit Earth’s atmosphere earlier this year was spinning once every 2.6 seconds, faster than any we knew of.

    Called 2024 BX1, the object – probably no more than 1 metre wide – entered Earth’s atmosphere on 21 January, breaking apart over Berlin, Germany. Some pieces survived the fireball and were recovered. It was a rare example of a tracked asteroid fall, in which the incoming rock is spotted before it encounters Earth, in this case just 3 hours ahead of the event.

    Maxime Devogele at the European Space Agency’s Near-Earth Object Coordination Centre in Italy and his colleagues took images of the asteroid prior to its impact. Despite it moving at some 50,000 kilometres per hour, its elongated shape meant changes in its brightness caused by rotation were particularly prominent in these images.

    Those changes in brightness corresponded to a rotation time of 2.588 seconds – roughly 30,000 rotations per day. “It’s the fastest [spin] we’ve ever observed,” says Devogele.

    Asteroids spin for a number of reasons, such as collisions earlier in their life. In general, space rocks larger than a kilometre can’t rotate more than once every 2.2 hours because they would break apart. But smaller asteroids like 2024 BX1 can withstand much faster spins because they are more compact. “They have internal strength, so they can rotate faster,” says Devogele.

    Gauging the spin of objects like this could be useful for planetary defence, letting us know how strong a small asteroid is and how likely it might be to survive its passage through Earth’s atmosphere. “If it’s hard, it will react differently than if it’s a piece of snow that has no internal strength,” says Devogele.

    Topics:

    [ad_2]

    Source link

  • Birthplace of red asteroid Kamo‘oalewa pinned to specific moon crater

    Birthplace of red asteroid Kamo‘oalewa pinned to specific moon crater

    [ad_1]

    The redness of asteroid 469219 Kamo‘oalewa marks it out as probably originating on the moon, and now we might know the exact impact crater it was launched from

    [ad_2]

    Source link

  • Did ‘alien’ debris hit Earth? Startling claim sparks row at scientific meeting

    Did ‘alien’ debris hit Earth? Startling claim sparks row at scientific meeting

    [ad_1]

    An electron microprobe image of a grey sphere on a black background. The sphere has a partially irregular surface and is about 200 micrometres across according to the scale bar.

    Avi Loeb and his team say that metallic balls found near Papua New Guinea could be of extraterrestrial origin.Credit: Avi Loeb’s photo collection

    The Woodlands, Texas

    A sensational claim made last year that an ‘alien’ meteorite hit Earth near Papua New Guinea in 2014 got its first in-person airing with the broader scientific community on 12 March. At the Lunar and Planetary Science Conference in The Woodlands, Texas, scientists clashed over whether a research team has indeed found fragments of a space rock that came from outside the Solar System.

    The debate occurred at a packed session featuring Hairuo Fu, a graduate student at Harvard University in Cambridge, Massachusetts, who is a member of the team that found the fragments. Team leader Avi Loeb, an astrophysicist at Harvard who did not attend the conference, has made other controversial claims about extraterrestrial discoveries. Many scientists have said that they don’t want to spend much of their time analysing and refuting these claims.

    During his presentation, Fu described tiny metallic blobs that Loeb’s expedition dredged from the sea floor near Papua New Guinea last year, and said that the spherules have a chemical composition of unknown origin1. He then faced questions from a long line of scientists sceptical of the implications of extraterrestrial material. “At the very least, it is something different from what we know,” Fu responded.

    New work questions the team’s findings. In a manuscript posted on the arXiv preprint server on 8 March2, ahead of peer review, a researcher argues that the debris collected by Loeb and his co-workers is actually molten blobs generated when an asteroid hit Earth 788,000 years ago.

    “What they found has all the characteristics of microtektites — little pieces of melted Earth that came from this impact,” says preprint author Steve Desch, an astrophysicist at Arizona State University in Tempe.

    Meanwhile, other studies are challenging different aspects of Loeb’s claim, such as whether the meteor that reportedly produced the fragments was on the trajectory Loeb says it was. Together, the findings show how the broader scientific community is engaging with Loeb’s extraterrestrial claims, in spite of reluctance to do so.

    A unique find?

    ‘Interstellar’ objects remained in the realm of theory until 2017, when astronomers spotted the first known celestial object to be on a trajectory that meant it could only have come from outside the Solar System. Loeb made headlines when he speculated that the object, a comet-like body named ‘Oumuamua, was an artefact sent by an extraterrestrial civilization.

    ‘Oumuamua passed through the Solar System far from Earth, but Loeb hoped to find another interstellar object that had hit the planet. He later proposed that a bright meteor that appeared in the sky north of Papua New Guinea in January 2014 had an interstellar trajectory and could have scattered debris in the ocean.

    Three people use a vacuum tool on a metallic sledge on board a ship.

    Avi Loeb (in hat) and colleagues recover particles from a magnetic sledge on their 2023 expedition.Credit: Avi Loeb’s photo collection

    In June 2023, Loeb led a privately funded expedition to the site that used magnetic sledges to recover more than 800 metallic spherules from the sea floor. About one-quarter of the spherules had chemical compositions indicating that they came from igneous, or once-molten, rocks. Of those, a handful were unusually enriched in the elements beryllium, lanthanum and uranium. The researchers concluded that those spherules are unlike any known materials in the Solar System1.

    However, Desch counters that the spherules could have come from an asteroid impact in southeast Asia. Key to his proposal2 is a kind of soil called laterite, which forms in tropical regions when heavy rainfall carries some chemical elements from the topmost layers of soil into deeper ones. This leaves the upper soil enriched in other elements, including beryllium, lanthanum and uranium — similar to the composition of the spherules collected by Loeb and his colleagues. Desch says that an asteroid known to have struck the region around 788,000 years ago3 probably hit lateritic rock and created the molten blobs found by Loeb’s team.

    In an e-mail to Nature, Loeb argues that spherules from an impact 788,000 years ago should have been buried by ocean sediments. Desch counters that sedimentation rates are relatively low in the offshore area where the spherules were collected.

    But others are sceptical of Desch’s proposal, too. Scientists have yet to find any confirmed tektites from lateritic rock, notes Pierre Rochette, a geoscientist at Aix-Marseille University in Aix-en-Provence, France, who is not affiliated with either team. And very few tektites are magnetic, he says, so it would be difficult for Loeb and his colleagues to have pulled up hundreds from the sea floor.

    Fiery critiques

    Desch was not the only scientist to challenge Loeb’s work this week.

    After Fu’s conference presentation, Ben Fernando, a seismologist at Johns Hopkins University in Baltimore, Maryland, spoke and took aim at claims concerning the 2014 meteor. Fernando and his colleagues, including Desch, analysed seismic and acoustic data gathered by ground-based sensors at the time the meteor hit the atmosphere4. Data from a seismometer on nearby Manus Island, which Loeb and his team studied as they were deciding where to dredge, show no characteristics of a high-altitude fireball — but do indicate a vehicle driving past, Fernando said. “This is almost certainly a truck,” he told the meeting. A second set of observations, made using infrasound sensors that listen for clandestine nuclear tests, seems to have detected the meteor hitting the atmosphere, but suggests it happened around 170 kilometres away from where Loeb’s team calculates.

    Loeb told Nature that such critiques do not take into account US Department of Defense data that he says confirm the exact trajectory of that fireball. But because those data are held by the government, they have not been independently cross-checked by other scientists.

    As conference-goers poured out of the room after his talk, Fu told Nature that Loeb’s team is working on further analyses, such as isotopic studies, that could shed more light on what the spherules are. After that, Fu said, he is looking forward to graduating and working on a new project — on how the Moon was formed.

    [ad_2]

    Source link