«Understanding properties of silicate melts and glasses at ultra-high pressure is crucial to understand how the Earth has formed in its infancy, where
impacts of large asteroids led to a completely molten Earth,» said Prescher.
Formed by
the impact of a large asteroid or comet, Caloris is one of the largest, and possibly one of the youngest, basins in the Solar System.
Not exact matches
This group was probably one
of the
largest groups
of dinosaurs to do so before the assumed
asteroid impact 66 million years ago, which killed all non-bird dinosaurs.
Over 30 years ago, scientists proposed a
large asteroid impact to explain the disparate elevations
of Mars» northern and southern hemispheres; the theory became known as the «single
impact hypothesis.»
New research by University
of Colorado Boulder professor Stephen Mojzsis outlines a likely cause for these mysterious features
of Mars: a colossal
impact with a
large asteroid early in the planet's history.
Sauropods, a group
of large plant - eaters like Brontosaurus, may have started dying off 50 million years before the Chicxulub
asteroid impact, they found.
The threat to our security is in the form
of asteroids too small to be detected at long range but
large enough to cause major catastrophes; NASA is now searching for
asteroids one kilometer or
larger in diameter, the
impact of which could have global consequences.
In 1992 there was a meeting at Los Alamos National Laboratory to look at the consequences
of large asteroid impacts on Earth.
Other theories involve planetary collisions that knock worlds off course or simply a
large mass
of materiallike an
asteroid that jumps aboard and, by its mass and
impact, tilts the once - flat orbit.
The discovery
of coesite in the Chicxulub Crater under the Yucatan Peninsula in Mexico was significant evidence that this geological formation resulted from the
impact of a comet or
large asteroid.
Marchi's team proposes a novel, more efficient mechanism As the planet was pummeled by primordial
asteroids — some
larger than 100 kilometers in diameter —
impacts would melt
large volumes
of rock, creating temporary lakes
of lava.
New images indicate that most
of the cavities are secondary
impacts from rocks kicked up when
large asteroids hit.
That feature — in which the crust thickness drops from 30 to about 10 miles (50 to 20 kilometers) over a
large area that is the most visible feature on Mars — has been known to astronomers for more than 30 years and was long suspected to be due to an
asteroid impact that flung most
of the crust out the area.
The kind
of asteroid needed to form the Martian dichotomy would fall in between that size and those
of the rocks that formed other
large craters, such as the South Pole — Aitken
impact basin on the moon and the Hellas Basin in Mars's southern hemisphere, both more than 1,30 miles (2,000 kilometers) wide.
Millions
of them are
large enough to do serious damage in an
impact, including the
asteroid Apophis, which has a small chance
of hitting Earth in 2036.
Three potential events were considered as part
of their research, including;
large asteroid impact, and exploding stars in the form
of supernovae or gamma ray bursts.
This view
of 1,000 - mile - wide Caloris basin — among the
largest known
asteroid impacts in the solar system — shows how lava (orange) filled the blast site before new craters excavated the original basin (purple).
But in spite
of this, most civilian astronomers believe that tackling the catastrophically
large but very rare
impacts should be the first priority («How to destroy the doomsday
asteroid», New Scientist, 6 June).
This period was apparently associated with increased meteoric
impacts (around 100 times more frequent than today) associated with the break - up in the Main
Asteroid Belt of the L - chondrite parent body — the largest documented asteroid breakup event over the past few billio
Asteroid Belt
of the L - chondrite parent body — the
largest documented
asteroid breakup event over the past few billio
asteroid breakup event over the past few billion years.
The research contradicts other suggestions that the
large valley networks on the red planet were the result
of short - lived catastrophic flooding, lasting just hundreds to a few thousand years and perhaps triggered by
asteroid impacts.
This artist's conception shows the immediate aftermath
of a
large asteroid impact around NGC 2547 - ID8, a 35 million - year - old star.
Asteroid impacts, especially the
large ones, can excite atmospheric waves capable
of revealing information about the internal structures
of the planets that probably can not be obtained in any other way.
Because smaller chunks
of asteroids drift from the point
of collision faster than
larger pieces do, these
asteroid families become shaped like the letter «V.» Smaller pieces spread out far and wide from the original
impact site, while
larger fragments remain condensed at the point.
Mapping this microstructure to a
large asteroid could help to predict the height and strength
of the explosion, for example, or the likely
impacted area
of an impending meteorite strike after midair breakup.
«No sufficiently
large asteroid currently exists in an Earth - crossing orbit; however, a comet
of sufficient size to cause human extinction could
impact the Earth, though the annual probability may be less than 10 − 8.
``... we lack compelling scenarios leading to the origin
of iron meteorites... Early solar system collisions have been called upon to excavate this iron [from the cores
of the
largest asteroids], although numerical
impact models have found this task difficult to achieve, particularly when it is required to occur many dozens
of times, yet not a single time for
asteroid Vesta.»
New high - resolution observations
of Vesta by the DAWN mission reveal that the creatr is part
of an even
larger impact basin that was created by two massive overlapping
impacts roughly around one and two billion years ago, which scooped out around one percent
of the
asteroid's estimated volume and blasted it into space (more from NASA's DAWN Mission and NEO Program; 1997 NASA / Hubble news release; Cornell University; Thomas et al, 1997; Kelley et al, 2003; and Jerry Coffrey, Universe Today, June 15 2009; and Russell et al, 2012; Jaumann et al, 2012; Marchi et al, 2012; and Schenk et al, 2012).
This artist's rendition shows how an
asteroid collision might appear at the moment
of impact, although the space rock in this image is considerably
larger than the one Becker's team believes hit 250 million years ago.
Since then, astronomers have become increasingly a ware
of the risk
of future
impacts, and major efforts are underway to discover and calculate the orbits for all
asteroids larger than 1 km wide.
Eventually, one
of my students asked about what a
large asteroid impact would do to our Moon.
For example, even though the threat
of asteroid impact is low, the threat is so
large that it has to be taken seriously.
Some mechanisms for that are hypothesized, e.g. methane release from polar regions, increased melting
of Greenland leading to stopping the Gulf Stream, rapid reduction
of Arctic sea - ice and its positive feedback, collapse
of Antarctic ice shelves, loss
of the Amazon,
large volcanoes,
asteroid impacts, unexpected solar variation.
Suppose an astronomer discovered an
asteroid heading for an
impact with the Earth — how would the argument «On geological timescales Earth has been struck by lots
of objects, including some much
larger than this one» be taken?