[meteorite-list] Catalog of Known Near-Earth Asteroids Tops 15, 000

2016-10-27 Thread Ron Baalke via Meteorite-list

http://www.jpl.nasa.gov/news/news.php?feature=6664

Catalog of Known Near-Earth Asteroids Tops 15,000
Jet Propulsion Laboratory
October 27, 2016

The number of discovered near-Earth asteroids (NEAs) now tops 15,000, 
with an average of 30 new discoveries added each week. This milestone 
marks a 50 percent increase in the number of known NEAs since 2013, when 
discoveries reached 10,000 in August of that year.

Surveys funded by NASA's Near Earth Object (NEO) Observations Program 
(NEOs include both asteroids and comets) account for more than 95 percent 
of discoveries so far.

The 15,000th near-Earth asteroid is designated 2016 TB57. It was discovered 
on Oct. 13 by observers at the Mount Lemmon Survey, an element of the 
NASA-funded Catalina Sky Survey in Tucson, Arizona. 2016 TB57 is a rather 
small asteroid -- about 50 to 115 feet (16 to 36 meters) in size -- that 
will come closest to Earth on Oct. 31 at just beyond five times the distance 
of the moon. It will safely pass Earth.

A near-Earth asteroid is defined as one whose orbit periodically brings 
it within approximately 1.3 times Earth's average distance to the sun 
-- that is within 121 million miles (195 million kilometers) -- of the 
sun (Earth's average distance to the sun is about 93 million miles, or 
150 million kilometers). This distance also then brings the asteroid within 
roughly 30 million miles (50 million kilometers) of Earth's orbit. Observers 
have already discovered more than 90 percent of the estimated population 
of the large NEOs -- those larger than 0.6 miles (one kilometer).

"The rising rate of discovery is due to dedicated NEO surveys and upgraded 
telescopes coming online in recent years," said NASA's NEO Observations 
Program Manager Kelly Fast.  "But while we're making great progress, we 
still have a long way to go." It is estimated by astronomers that only 
about 27 percent of the NEAs that are 460 feet (140 meters) and larger 
have been found to date.  Congress directed NASA to find over 90 percent 
of objects this size and larger by the end of 2020.

Currently, two NASA-funded NEO surveys -- the Catalina Sky Survey and 
the Panoramic Survey Telescope & Rapid Response System (Pan-STARRS) in 
Hawaii -- account for about 90 percent of new NEO discoveries. Both projects 
upgraded their telescopes in 2015, improving their discovery rates.

A recent upgrade to one of the Catalina Sky Survey's telescopes resulted 
in a tripling of its average monthly NEO discovery rate. When the Pan-STARRS 
system increased the observing time it devoted to NEO searching to 90 
percent, it increased its rate of discovery by a factor of three. Pan-STARRS 
also will add a second telescope to the hunt this fall. As more capable 
telescopes are deployed, the overall NEO survey effort will be able to 
find more objects as small as and smaller than 140 meters (460 feet).

The NEO Observations Program is a primary element of NASA's Planetary 
Defense Coordination Office, which is responsible for finding, tracking 
and characterizing potentially hazardous NEOs, issuing warnings about 
possible impacts, and coordinating U.S. government planning for response 
to an actual impact threat.

"While no known NEO currently poses a risk of impact with Earth over the 
next 100 years," says NASA Planetary Defense Officer Lindley Johnson, 
"we've found mostly the larger asteroids, and we have a lot more of the 
smaller but still potentially hazardous ones to find."

For asteroid news and updates, follow AsteroidWatch on Twitter:

http://www.twitter.com/AsteroidWatch

News Media Contact
DC Agle
Jet Propulsion Laboratory, Pasadena, Calif.
818-393-9011
a...@jpl.nasa.gov

Dwayne Brown / Laurie Cantillo
NASA Headquarters, Washington
202-358-1726 / 202-358-1077
dwayne.c.br...@nasa.gov / laura.l.canti...@nasa.gov

2016-284

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[meteorite-list] Further Clues to Fate of Schiaparelli Mars Lander, Seen From Orbit

2016-10-27 Thread Ron Baalke via Meteorite-list

http://www.jpl.nasa.gov/news/news.php?feature=6663

Further Clues to Fate of Mars Lander, Seen From Orbit
Jet Propulsion Laboratory
October 27, 2016

The most powerful telescope orbiting Mars is providing new details of 
the scene near the Martian equator where Europe's Schiaparelli test lander 
hit the surface last week.

An Oct. 25 observation using the High Resolution Imaging Science Experiment 
(HiRISE) camera on NASA's Mars Reconnaissance Orbiter shows three impact 
locations within about 0.9 mile (1.5 kilometers) of each other. An annotated 
view is available online at

http://www.jpl.nasa.gov/spaceimages/details.php?id=PIA21131

The scene shown by HiRISE includes three locations where hardware reached 
the ground. A dark, roughly circular feature is interpreted as where the 
lander itself struck. A pattern of rays extending from the circle suggests 
that a shallow crater was excavated by the impact, as expected given the 
premature engine shutdown. About 0.8 mile (1.4 kilometers) eastward, an 
object with several bright spots surrounded by darkened ground is likely 
the heat shield. About 0.6 mile (0.9 kilometer) south of the lander impact 
site, two features side-by-side are interpreted as the spacecraft's parachute 
and the back shell to which the parachute was attached. Additional images 
to be taken from different angles are planned and will aid interpretation 
of these early results.

The test lander is part of the European Space Agency's ExoMars 2016 mission, 
which placed the Trace Gas Orbiter into orbit around Mars on Oct. 19. 
The orbiter will investigate the atmosphere and surface of Mars and provide 
relay communications capability for landers and rovers on Mars.

Data transmitted by Schiaparelli during its descent through Mars' atmosphere 
is enabling analysis of why the lander's thrusters switched off prematurely. 
The new HiRISE imaging provides additional information, with more detail 
than visible in an earlier view with the Context Camera (CTX) on the Mars 
Reconnaissance Orbiter.

With HiRISE, CTX and four other instruments, the Mars Reconnaissance Orbiter 
has been investigating Mars since 2006.

The University of Arizona, Tucson, operates HiRISE, which was built by 
Ball Aerospace & Technologies Corp. of Boulder, Colorado. NASA's Jet Propulsion 
Laboratory, a division of Caltech in Pasadena, California, manages the 
Mars Reconnaissance Orbiter Project for NASA's Science Mission Directorate, 
Washington. Lockheed Martin Space Systems, Denver, built the orbiter and 
collaborates with JPL to operate it. For additional information about 
the project, visit:

http://mars.nasa.gov/mro

News Media Contact
Guy Webster
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-6278
guy.webs...@jpl.nasa.gov

Markus Bauer
European Space Agency, Villanueva de la CaƱada, Spain
0031 61 594 3 954
markus.ba...@esa.int

Dwayne Brown / Laurie Cantillo
NASA Headquarters, Washington
202-358-1726 / 202-358-1077
dwayne.c.br...@nasa.gov / laura.l.canti...@nasa.gov

2016-283

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[meteorite-list] GRAIL Moon Mission Shares Insights into Giant Impacts

2016-10-27 Thread Ron Baalke via Meteorite-list

http://www.jpl.nasa.gov/news/news.php?feature=6662

NASA Moon Mission Shares Insights into Giant Impacts
Jet Propulsion Laboratory
October 27, 2016

Fast Facts:

* Orientale basin is a giant, ringed impact crater on Earth's moon.
* Until now, how impact craters with rings form had not been well 
understood.
* Scientists have reconstructed Orientale's formation using data 
from NASA's GRAIL mission.

New results from NASA's Gravity Recovery and Interior Laboratory (GRAIL) 
mission are providing insights into the huge impacts that dominated the 
early history of Earth's moon and other solid worlds, like Earth, Mars, 
and the satellites of the outer solar system.

In two papers, published this week in the journal Science, researchers 
examine the origins of the moon's giant Orientale impact basin. The research 
helps clarify how the formation of Orientale, approximately 3.8 billion 
years ago, affected the moon's geology.

Located along the moon's southwestern limb -- the left-hand edge as seen 
from Earth -- Orientale is the largest and best-preserved example of what's 
known as a "multi-ring basin." Impact craters larger than about 180 miles 
(300 kilometers) in diameter are referred to as basins. With increasing 
size, craters tend to have increasingly complex structures, often with 
multiple concentric, raised rings. Orientale is about 580 miles (930 
kilometers) 
wide and has three distinct rings, which form a bullseye-like pattern.

Multi-ring basins are observed on many of the rocky and icy worlds in 
our solar system, but until now scientists had not been able to agree 
on how their rings form. What they needed was more information about the 
crater's structure beneath the surface, which is precisely the sort of 
information contained in gravity science data collected during the GRAIL 
mission.

The powerful impacts that created basins like Orientale played an important 
role in the early geologic history of our moon. They were extremely disruptive, 
world-altering events that caused substantial fracturing, melting and 
shaking of the young moon's crust. They also blasted out material that 
fell back to the surface, coating older features that were already there; 
scientists use this layering of ejected material to help determine the 
age of lunar features as they work to unravel the moon's complex history.

The Importance of Orientale

Because scientists realized that Orientale could be quite useful in 
understanding 
giant impacts, they gave special importance to observing its structure 
near the end of the GRAIL mission. The orbit of the mission's two probes 
was lowered so they passed less than 1.2 miles (2 kilometers) above the 
crater's mountainous rings.

"No other planetary exploration mission has made gravity science observations 
this close to the moon. You could have waved to the twin spacecraft as 
they flew overhead if you stood at the ring's edge," said Sami Asmar, 
GRAIL project scientist at NASA's Jet Propulsion Laboratory, Pasadena, 
California.

Of particular interest to researchers has been the size of the initial 
crater that formed during the Orientale impact. With smaller impacts, 
the initial crater is left behind, and many characteristics of the event 
can be inferred from the crater's size. Various past studies have suggested 
each of Orientale's three rings might be the remnant of the initial crater.

In the first of the two new studies, scientists teased out the size of 
the transient crater from GRAIL's gravity field data. Their analysis shows 
that the initial crater was somewhere between the size of the basin's 
two innermost rings.

"We've been able to show that none of the rings in Orientale basin represent 
the initial, transient crater," said GRAIL Principal Investigator Maria 
Zuber of the Massachusetts Institute of Technology in Cambridge, lead 
author of the first paper. "Instead, it appears that, in large impacts 
like the one that formed Orientale, the surface violently rebounds, 
obliterating 
signs of the initial impact."

The analysis also shows that the impact excavated at least 816,000 cubic 
miles (3.4 million cubic kilometers) of material -- 153 times the combined 
volume of the Great Lakes.

"Orientale has been an enigma since the first gravity observations of 
the moon, decades ago," said Greg Neumann, a co-author of the paper at 
NASA's Goddard Space Flight Center in Greenbelt, Maryland. "We are now 
able to resolve the individual crustal components of the bullseye gravity 
signature and correlate them with computer simulations of the formation 
of Orientale."

Reproducing the Rings

The second study describes how scientists successfully simulated the formation 
of Orientale to reproduce the crater's structure as observed by GRAIL. 
These simulations show, for the first time, how the rings of Orientale 
formed, which is likely similar for multi-ring basins in general.

"Because our models show how the subsurface structure is formed, matching 
what 

[meteorite-list] Water Detected on Largest Metallic Asteroid in Solar System (Psyche)

2016-10-27 Thread Ron Baalke via Meteorite-list


https://www.usgs.gov/news/water-detected-largest-metallic-asteroid-solar-system

Water Detected on Largest Metallic Asteroid in Solar System
USGS
Release Date: October 20, 2016

Scientists have discovered possible evidence for water-rich minerals on 
the surface of the largest metallic asteroid in the solar system, according 
to a study by the U.S. Geological Survey and NASA. 

The asteroid, called Psyche, is 186 miles across and is made of almost 
pure nickel-iron metal. It is thought to be the remnant core of a planetary 
embryo that was mostly destroyed by impacts billions of years ago.

Previous observations of Psyche had shown no evidence for water-rich minerals 
on its surface. However, new observations from the NASA Infrared Telescope 
Facility in Hawaii show evidence for water and/or hydroxyl on its surface. 
Results are published in The Astronomical Journal.

While the source of these water molecules on Psyche remains a mystery, 
scientists propose a few possible mechanisms for their formation. It is 
possible that water-rich minerals detected on Psyche might have been delivered 
to its surface by carbonaceous asteroids that impacted Psyche in the distant 
past.

"We think that Psyche may not be entirely exposed metallic core," 
says Driss Takir, lead author and scientist at the USGS Astrogeology Science 
Center in Flagstaff, Arizona. "What we see might instead have been a 
core-mantle boundary of a differentiated body that was disrupted via impacts. 
Solar radiation is another mechanism that can produce hydroxyl, which 
is a molecule consisting of one oxygen atom and one hydrogen atom, by 
interacting with the surface of Psyche."

"This work underscores how much more we have to learn about asteroids," 
says Laszlo Kestay, Director of the USGS Astrogeology Science Center. 
"It will take more of this kind of careful work with telescopes on Earth, 
and spacecraft visiting asteroids, before we understand what treasures 
await us in space."

Takir is a member of NASA's OSIRIS-REx mission and JAXA's Hayabusa 2 
mission to collect carbonaceous samples from the water-rich asteroids, 
Bennu and Ryugu.

"We are excited to continue studying Psyche, and other water-rich asteroids, 
to give us further insight into the distribution of potential resources 
in space," said Takir.

This research on Psyche is funded by the USGS/NASA Eugene M. Shoemaker 
Fellowship, NASA Planetary Science Division Planetary Geology and Geophysics 
and Solar System Observations Programs.


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[meteorite-list] Meteorite Picture of the Day

2016-10-27 Thread Paul Swartz via Meteorite-list
Today's Meteorite Picture of the Day: Twannberg

Contributed by: Andreas Gren

http://www.tucsonmeteorites.com/mpodmain.asp?DD=10/27/2016
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