Hubble resolves Martian surface features with a level of detail only exceeded by planetary probes, such
as impact craters and other features as small as 30 miles (50 kilometers) across.
Extraterrestrial sample analysis and terrestrial field work on fundamental geological processes such
as impact cratering, and their implications for the origin and evolution of life.
Not exact matches
[241] The attractions and major tourist destinations of Ghana include a warm, tropical climate year - round; diverse wildlife; exotic waterfalls such
as Kintampo Waterfalls and the largest waterfall in west Africa, Wli Waterfalls; Ghana's coastal palm - lined sandy beaches; caves; mountains, rivers; meteorite
impact crater and reservoirs and lakes such
as Lake Bosumtwi or Bosumtwi meteorite
crater and the largest man - made lake in the world by surface area, Lake Volta; dozens of castles and forts; UNESCO World Heritage Sites; nature reserves and national parks.
Many scientists think these permanently shadowed regions, such
as the floors on
impact craters in the Moon's polar regions, could hold large deposits or water ice.
By examining the
craters that formed on top of it, researchers estimate that Rembrandt formed in an
impact some 3.9 billion years ago, near the end of a barrage of
impacts in the inner solar system known
as the Late Heavy Bombardment.
The
impact melted the surface that it hit and gouged out a 77 - kilometre - wide basin known
as King
crater.
Key to the basin's identification
as a potential
impact crater are the decrease in the strength of Earth's gravity over the site, indicating a large basin filled with younger low - density sediments, and a strong increase in the strength of Earth's magnetism at the site.
Each grainy image took eight hours to receive, but the payoff was huge: Surprising evidence of deep
impact craters banished the popular idea of Mars
as a chillier version of Earth.
The chance of a giant
impact producing a
crater so precisely aligned with Charon is vanishingly slim, Keane says, so he and his team (
as well
as Nimmo's) went searching for another explanation.
At the same time, the
impact would have plastered preexisting river and swamp deposits onto the flanks of the
impact crater, where they would later be imaged
as the chaotic deposits in our acoustic - echo profiles.
In this instance, researchers have been able to use new imaging techniques to measure the atomic nanostructure of ancient crystals at
impact locations, using the 150 - kilometre - wide
crater at Sudbury
as a test site.
If that upwelled material is denser than what was blasted away by the
impact, the
crater ends up with the same mass
as it had before the
impact happened.
This is more than double previous estimates and, if correct, places the Alamo
crater as one of the largest marine
impacts in the last 550 million years, conservatively larger than the well - studied Chesapeake Bay
impact crater (about 35 million years old) on the eastern shore of North America.
The
crater was filled - in with fragmented rock, and later with more typical ocean deposits,
as the energy from the
impact lessened and the environment returned to normal.
As the drill approaches the
crater, 800 meters down, scientists expect to find fewer species of the shell - producing animals that make up the limestone, because life was just recovering from the
impact.
The shapes seen both in the models and in reality are similar to other funnel - shaped
impact craters, such
as those seen on NASA's Stardust spacecraft, which collected space dust particles in aerogel.
The
impact that produced the
crater was two million times more powerful than the largest nuclear device ever tested, a 58 - megaton hydrogen bomb known
as Tsar Bomba, detonated by the Soviet Union in 1961.
Not a single
impact crater is to be seen in this region, so the surface must be very young — reshaped by some sort of geological activity such
as faulting or icy volcanism.
Some surface features, such
as volcanoes and
impact craters, are self - evident, but the images give only indirect clues to the all - important internal processes.
Although no very ancient terrestrial
impact structures are preserved, the Sudbury basin provides a unique opportunity to study the sediment that filled the basin
as a guide to what the earlier
impact craters would have looked like.
The spherules, known
as microtektites, are droplets of molten rock that were melted and thrown out of the
impact crater by the energy of the projectile, or condensed from rock that was vaporized upon
impact.
The
cratering record on the moon provides a proxy for similar
impacts by interplanetary debris such
as comets and asteroids on Earth, the effects of which have largely been erased by billions of years of erosion and geologic activity.
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.
They reasoned that without continual renewal, the surfaces of such bodies should have become densely covered with
craters as a result of
impacts by meteorites and comets over the 4.5 billion years that they have existed.
The
impact that formed a large basin known
as Orientale in the western area of the moon's near side, which the group investigated in detail, obliterated all prior
craters within the basin itself, an area of nearly 700,000 square kilometers.
Project scientists were so unsure of the
impact's effects that they had a betting pool
as to how large the
crater would be — one of the most important indicators of the structure of the comet nucleus.
You can scoop up bits of stishovite at the scene of meteorite
impacts, such
as a 50,000 - year - old meteor
crater in Arizona that measures about 3 / 4 - mile across and about 570 feet deep.
Those results set the age boundary for the oldest terrains on Mercury to be contemporary with the so - called Late Heavy Bombardment (LHB), a period of intense asteroid and comet
impacts recorded in lunar and asteroidal rocks and by the numerous
craters on the Moon, Earth, and Mars,
as well
as Mercury.
The size and shape of the
crater and the amount of material excavated depends on factors such
as the velocity and mass of the
impacting body and the geology of the surface.
This location was chosen because it is one of the most Mars - like locales on the face of the Earth: the island is completely uninhabited and unvegetated; it receives almost no precipitation, and is thus nearly
as dry
as Mars; temperature extremes approach those of Mars; the
impact crater where the station is located is similar to many such
craters on Mars.
Recently, geologists suggested these grains may have formed in huge
impact craters produced
as chunks of rock from space, up to several kilometres in diameter, slammed into a young Earth.
As five
impact craters on Mercury receive names, NASA's MESSENGER spacecraft is about to create another, since it has run out of propellant and is predicted to
impact on the surface of the planet at 8:26 pm BST today.
The minerals could not have been formed in a local event, such
as an
impact into an ice - filled
crater.
Some of this brighter material appears to have flowed further downslope to form the heart shape,
as the small
impact occurred on the ejecta blanket of a much larger
impact crater.
In addition, the collision with a 372 - kilogram (820 - pound) projectile launched by NASA's Deep
Impact probe in 2005 has created a 150 - meter - wide (490 - foot - wide) crater with a small mound in the center, as some of the ejecta of the impact apparently fell back down within the crater, but the crater's relatively soft outline indicates that its edges have undergone significant changes since the 2005 impact (NASA / STARDUST / NExT news release; Astronomy Picture of the Day; David Shiga, New Scientist, February 15, 2011; Jonathan Amos, BBC News, February 15, 2011; and Richard A. Lovett, Nature News, February 15,
Impact probe in 2005 has created a 150 - meter - wide (490 - foot - wide)
crater with a small mound in the center,
as some of the ejecta of the
impact apparently fell back down within the crater, but the crater's relatively soft outline indicates that its edges have undergone significant changes since the 2005 impact (NASA / STARDUST / NExT news release; Astronomy Picture of the Day; David Shiga, New Scientist, February 15, 2011; Jonathan Amos, BBC News, February 15, 2011; and Richard A. Lovett, Nature News, February 15,
impact apparently fell back down within the
crater, but the
crater's relatively soft outline indicates that its edges have undergone significant changes since the 2005
impact (NASA / STARDUST / NExT news release; Astronomy Picture of the Day; David Shiga, New Scientist, February 15, 2011; Jonathan Amos, BBC News, February 15, 2011; and Richard A. Lovett, Nature News, February 15,
impact (NASA / STARDUST / NExT news release; Astronomy Picture of the Day; David Shiga, New Scientist, February 15, 2011; Jonathan Amos, BBC News, February 15, 2011; and Richard A. Lovett, Nature News, February 15, 2011).
Bright features such
as these are caused by the presence of freshly crushed rock material that was excavated and deposited during the highly energetic collision of a meteoroid with Mercury to form an
impact crater.
Impact craters at many latitudes sometimes expose thin ice layers a foot or so beneath Mars» surface.132 «At polar latitudes,
as much
as 50 percent of the upper meter of soil may be [water] ice.»
As distinct from
impact craters, these
craters are not formed from the clashing of bodies or projectiles from space.
In another scene, mimicking the popular Absolut Vodka advertising of the time, GALA's ad featured a liquor - bottle shaped
impact crater as damage to the Alfred P. Murrah Federal Building, site of the 1995 Oklahoma City Bombing, a domestic terrorist attack that killed 168 people.
The record of history,
as written in the many
impact craters on Earth and the moon, demonstrate that it is just a matter of time before astronomers discover a near Earth object (NEO) headed toward a collision with Earth.
Yet even if the Siberian
craters do prove to be an unexpected mechanism of accelerated methane release, the best analogy here remains «boiling a frog»
as impacts accumulate gradually, until eventually a tipping point is reached.
But then, you see, the
impact crater cools,
as the heat is radiated, convected, and conducted away.
Guest shoot - down by David Middleton Preface In my previous two posts on uniformitarian
impact craters, we examined the pitfalls of drawing cartoons on Google Earth images without ever looking at the geology and how the Carolina Bays are
as antithetical to
impact features
as any dents in the ground possibly could be.
The firestorms would have produce an enormous injection of CO2
as well
as soot, and the
impact crater in partially calcium carbonate rock would have produced direct CO2 from the reduction of that rock, but neither the «nuclear winter» not the subsequent global warming extinguished life.