When later generations of stars form, some of that material congeals
into rocky planets like Earth.
The unusual, tiny - tailed comet C / 2014 S3 seems to be a leftover piece of the stuff that clumped together
into rocky planets like Earth.
Due to Vesta's large size, many astronomers classify it as a protoplanet, saying it would have continued to develop
into a rocky planet like Earth or Mars if Jupiter's gravity had not wreaked havoc in the asteroid belt long ago.
Not exact matches
The dust grains in the disk collide and aggregate to form pebbles, which grow
into boulders, and so on increasing in size through planetesimals, planetary embryos, and finally
rocky terrestrial
planets.
Now he is looking for something far more familiar: a smallish
rocky planet with an atmosphere that bears the chemical imprint of life, like the abundant (and otherwise inexplicable) oxygen that plants pump
into our own air.
That splits the population of small
planets into those that are
rocky like Earth — 1.5 Earth radii or less — and those that are gassy like Neptune, between 2 and 3.5 Earth radii.
The production of heavier and heavier elements by subsequent generations of stars transformed the universe
into a place where new and exotic objects could grow, including a
rocky planet called Earth, and the life - forms that call it home.
City - size planetesimals —
rocky microworlds that clumped together in the solar nebula — smashed
into our
planet's surface at incredible velocities and seeped down to Earth's iron core, depositing yet more iron.
into the story of the little spacecraft that could, in principle, find many
rocky planets, her high, thin voice sometimes disappeared
into the noise of the sirens outside.
But for every C - type asteroid relocated to the belt, at least 10 were sent careening
into the region where the
rocky planets were materializing.
The seeming abundance of
rocky super-Earths lends support to the core accretion model of
planet formation, in which small
rocky bodies collide and clump together to grow
into these objects.
The work could explain why the
planet has a relatively small heart, and paints a grisly picture of the early solar system, where massive,
rocky «super-Earths» were snuffed out before they could grow
into gas giants.
Vesta is essentially a remnant protoplanet, identical to the myriad small bodies that were incorporated
into Earth and the other
rocky planets more than 4 billion years ago.
PUFFED UP Early in its development, a
rocky planet may turn
into a synestia (illustrated), a spinning disk of vaporized rock that looks like a jelly - filled doughnut with a small, solid core (gray).
Lead author, Dr Jay Farihi (UCL Physics & Astronomy), said: «Building
rocky planets around two suns is a challenge because the gravity of both stars can push and pull tremendously, preventing bits of rock and dust from sticking together and growing
into full - fledged
planets.
The meteorites» mineralogical composition showed that, like Earth and the other
rocky planets but unlike almost all other asteroids, the newly formed Vesta melted and stratified
into a
rocky crust, a mantle, and an iron.
The greater estimate of shrinkage accords with models that predict how much a
rocky planet should contract as its interior cools; the new work may also lend insight
into the evolution of extrasolar
planets that, like Mercury and unlike Earth, lack any moving continents.
As Jupiter retreated from its closest approach to the sun (about the distance of Mars's orbit today), it left behind the mostly
rocky remnants that later coalesced
into our solar system's inner
planets, including Earth.
Over the course of about 100 million years, most of the material in that nebulous cloud accreted
into the existing eight
planets — four
rocky (including Earth) and four gaseous.
Sometimes a few
rocky planets are packed close to their star; most of these systems will become unstable, and the
planets will crash
into one another.
However, in a few billion years our sun will become a red giant, engulfing Mercury and Venus, turning Earth and Mars
into sizzling
rocky planets, and warming distant worlds like Jupiter, Saturn and Neptune — and their moons — in a newly established red giant habitable zone.
That heat led to the separation of the primordial body
into a
rocky crust, an underlying
rocky mantle, and a central metallic core, hallmarks of
planet Earth and the other
rocky planets.
Jupiter might have had a hand in flushing an earlier generation of
rocky worlds
into the sun to their doom, clearing the way for the current
planets to form.
A rain of asteroids hurled
into the inner solar system by a wandering Jupiter could have swept up a family of large
rocky planets huddled up close to the sun, researchers report online March 23 in the Proceedings of the National Academy of Sciences.
The interior of Vesta, unlike that of most asteroids, separated
into layers resembling a
planet's, with a
rocky crust covering a mantle composed of the mineral olivine.
On January 15, 2010, a team of astronomers released the results of computer simulations indicating that kilometer - size planetesimals can form and accrete
into rocky Earth - size
planets around Alpha Centauri B despite gravitational perturbations from Alpha Centauri A.
During the crossing, icy and
rocky debris in the belt could crash
into the
planet's atmosphere and create the type of cosmic fireworks seen when comet Shoemaker - Levy 9 crashed
into Jupiter,» Kalas said.
«This
planet has the interior structure of a hybrid super - Earth / Neptune, with a
rocky core surrounded by a significant amount of water compressed
into solid form at high pressures and temperatures.»
The moons that orbit the
planets in our solar system fall
into two categories: icy or
rocky.
Planets that are smaller (i.e. 1.5 Earth radii or less) or have less hydrogen and helium early in their lives turn into dense, rocky planets with solid surfaces, while larger planets or those with more gas turn into Neptune - like planets with no discernable solid surface and thick atmos
Planets that are smaller (i.e. 1.5 Earth radii or less) or have less hydrogen and helium early in their lives turn
into dense,
rocky planets with solid surfaces, while larger planets or those with more gas turn into Neptune - like planets with no discernable solid surface and thick atmos
planets with solid surfaces, while larger
planets or those with more gas turn into Neptune - like planets with no discernable solid surface and thick atmos
planets or those with more gas turn
into Neptune - like
planets with no discernable solid surface and thick atmos
planets with no discernable solid surface and thick atmospheres.
As Neptune raced outward and the other
planets shifted, they flung asteroids and comets
into an icy,
rocky blizzard.
By learning about the layering of these materials, scientists can explain why some
rocky planets turn
into an «Earth» rather than a «Mars» or «Venus» — a factor that is essential to understanding where life can appear in the universe.
Armed with this type of information, scientists will be able to turn the fraction of stars harboring Earth - sized
planets into the fraction of stars harboring bona - fide
rocky planets.
Researchers have found that most
planets discovered by Kepler so far fall
into two distinct size classes: the
rocky Earths and super-Earths, and the mini-Neptunes.
Both objects formed among the
rocky and icy protoplanets beyond the Solar System's «ice line» now located around 2.7 AUs, but the early development of Jupiter apparently prevented such large protoplanets between the gas giant and
planet Mars from agglomerating
into even bigger planetary bodies, by sweeping many
into pulverizing collisions as well as slinging them
into the Sun or Oort Cloud, or even beyond Sol's gravitational reach altogether.
As a result, Vesta «differentiated»
into a relatively dense metallic core (of approximately 136 miles or 220 kilometers across), lighter mantle, and crust, like the
rocky inner
planets, many large planetary satellite's like the Earth's Moon, and probably most, if not all, of the newly named «dwarf
planets» like Ceres.
In addition to
rocky asteroids and icier bodies further out from the Sun, many agglomerated
into larger planetesimals that eventually collided to form
planets like the Earth, and more than 250 minerals, including olivine and zircon, developed within the planetesimals with the help of melting, collisional shocks, and reactions with water.
«
Planets in our Solar System with atmospheres can be divided into two types: What we call rocky planets, i.e., those with solid surfaces and relatively thin atmospheres, and giant planets, which are primarily gaseous with very thick atmospheres,» explained Anthony Del Genio, a planetary scientist a
Planets in our Solar System with atmospheres can be divided
into two types: What we call
rocky planets, i.e., those with solid surfaces and relatively thin atmospheres, and giant planets, which are primarily gaseous with very thick atmospheres,» explained Anthony Del Genio, a planetary scientist a
planets, i.e., those with solid surfaces and relatively thin atmospheres, and giant
planets, which are primarily gaseous with very thick atmospheres,» explained Anthony Del Genio, a planetary scientist a
planets, which are primarily gaseous with very thick atmospheres,» explained Anthony Del Genio, a planetary scientist at GISS.
In that way, Arctic ice is unlike land - based ice sheets and glaciers in places like Greenland and Antarctica — when that ice tips off its
rocky seat
into the ocean, high tides all over the
planet lap a little farther up the shoreline.