Meteor Crater in Arizona,
formed by a meteorite impact 50,000 years ago, contains bits of a hard, compressed form of silica called stishovite.
Gale Crater was
formed by meteorite impact early in the history of Mars, and it was subsequently filled with sediments transported by flowing water.
Exquisite telescopic photographs of the lunar surface had existed for decades before the Apollo missions to the Moon, but they did not resolve the controversy of the origin of lunar craters were
they formed by meteorite impact or by volcanic eruption?
Not exact matches
Precious Metals the Result of
Meteorite Bombardment, Rock Analysis Finds Sep. 9, 2011 — Ultra high precision analyses of some of the oldest rock samples on Earth
by researchers at the University of Bristol provides clear evidence that the planet's accessible reserves of precious metals are the result of a bombardment of
meteorites more than 200 million years after Earth was
formed.
Sep. 9, 2011 — Ultra high precision analyses of some of the oldest rock samples on Earth
by researchers at the University of Bristol provides clear evidence that the planet's accessible reserves of precious metals are the result of a bombardment of
meteorites more than 200 million years after Earth was
formed.
Lonsdaleite
forms only under the extreme pressure and heat accompanying
meteorite impacts, while wurtzite boron nitride is a
by - product of intense volcanic eruption.
Of the 731 rock samples the Apollo 16 astronauts brought home in April 1972, nearly all were breccia, composites
formed of fragments fused together — probably
by the heat and pressure of
meteorite impacts.
The stone's noble gas content supports an extraterrestrial origin, while the presence of tiny diamonds — larger than nanodiamonds found in a common kind of
meteorite called chondrites, but similar in size to diamond aggregates known to be
formed by impacts — supports a cometary origin.
By studying the magnetic orientations in pristine samples of ancient
meteorites that
formed 4.563 billion years ago, the team determined that the solar nebula lasted around 3 to 4 million years.
Current thinking is that these tiny diamonds can
form in three ways: enormous pressure shockwaves from high - energy collisions between the
meteorite «parent body» and other space objects; deposition
by chemical vapor; or, finally, the «normal» static pressure inside the parent body, like most diamonds on Earth.
New work from a team of Carnegie cosmochemists published
by Science Advances reports analyses of carbon - rich dust grains extracted from
meteorites that show that these grains
formed in the outflows from one or more type II supernovae more than two years after the progenitor stars exploded.
They moreover show that the light signature emitted
by Phobos and Deimos is incompatible with that of the primordial matter that
formed Mars (
meteorites such as ordinary chondrite, enstatite chondrite and / or angrite).
Tiny carbon nuggets in
meteorites from Mars were
formed by cooling magma, not left
by ancient alien microbes.
Last year, researchers found that in conditions mimicking those sparked
by a comet or
meteorite impact, intense heat and pressure converted formamide (which
forms when hydrogen cyanide reacts with water) and other simple substances into the four information - bearing nucleobases in RNA, a likely genetic precursor to DNA.
In 2000, for instance, Malin published pictures of small gullies that, judging from the absence of
meteorite craters in them, seem to have been
formed by running water within the past few million years.
Lakes may
form when
meteorite impacts heat ice in the crust or when underground reservoirs of water kept liquid
by geothermal heat leak onto the surface.
The researchers were looking at rocks from the Ries crater (inset) of southern Germany, a 24 - kilometer - wide depression
formed about 14.6 million years ago
by a
meteorite crashing into Earth with the force of 1.8 million Hiroshima bombs.
Ben Weiss at the Massachusetts Institute of Technology and his colleagues tested three
meteorites that cooled a mere 3.8 million years after the sun began to
form, a date pinned down
by the ratio of their uranium and lead content.
In contrast, the
meteorite analyzed
by Lapen's research team was
formed 2.4 billion years ago and suggests that it was ejected from one of the longest - lived volcanic centers in the solar system.
After the meteor was sighted streaking through the sky on 22 April,
meteorite hunters found fragments of the rock, identified
by the «fusion crust» that
forms when it burns in the atmosphere.
By looking at tungsten and molybdenum isotopes on iron
meteorites, the team, made up of scientists from Lawrence Livermore National Laboratory and Institut für Planetologie at the University of Münsterin Germany, found that
meteorites are made up from two genetically distinct nebular reservoirs that coexisted but remained separated between 1 million and 3 - 4 million years after the solar system
formed.
Eventually, they landed on a second asteroid, where they were buried
by other rock — until that asteroid too shed them in the
form of the
meteorites that carried them to Earth.
The composition of the matter from which the solar system
formed is deduced from that of stony
meteorites called chondrites and from the composition of the Sun's atmosphere, supplemented
by data acquired from spectral observations of hot stars and gaseous nebulas.
Experiments at Berkeley Lab are helping to retrace the chemical steps
by which complex hydrocarbons like pyrene could
form in the Murchison
meteorite and other
meteorites.
Another NASA research group, led
by Kathie Thomas - Keprta of NASA's Johnson Space Center, report in the same issue of PNAS that the magnetite crystals inside the
meteorite are similar to those
formed by «modern» magnetotactic bacteria now living on Earth.
Scientists have argued for half a century about the existence of a
form of diamond called lonsdaleite, which is associated with impacts
by meteorites and asteroids.
But
by showing how carbonate globules, similar to those in the martian
meteorite,
formed without the involvement of living organisms, Steele and his colleagues have made less compelling the argument that the visiting rock from our planetary neighbor contains evidence of life.
The Mars rock made headlines in 1996 when researchers, led
by David McKay, from NASA's Johnson Space Center, claimed in the journal Science that the
meteorite contained evidence of possible Red Planet life
forms.
There are over 3,000 cenotes in Mexico, mostly in the area covered
by the Chicxulub crater, the crater that was
formed after the
meteorite impact that extinguished dinosaurs.
The buzz is building over a paper
by Richard Hoover, an award - winning astrobiologist at NASA's Marshall Space Flight Center, concluding that filaments and other features found in the interior of three specimens of a rare class of
meteorite appear to be fossils of a life
form strongly resembling cyanobacteria.
Since the hole was spotted in mid-July
by a helicopter pilot, conjecture has abounded about how the 30 - metre - wide crater was
formed — a gas or missile explosion, a
meteorite impact and alien involvement have all been suggested.