Polygonal Dunes on Mars


  Polygons are of great interest because they often indicate the presence of shallow ice or of desiccation such as in a mud flat. However, nature sometimes seems too clever for us.
  
  Polygons form by the intersecting ridges of sand dunes. If this deposit were to become indurated and eroded, we might not be able to tell that they originated as wind-blown dunes, and interpret the polygons as evidence for a dried-up lake, for example. Dunes often accumulate in the bottoms on craters, also a good setting for a (temporary) lake.
  
  The illumination is coming from the upper left, so the bluish ridges are high-standing.

Polygonal Dunes on Mars

Polygons are of great interest because they often indicate the presence of shallow ice or of desiccation such as in a mud flat. However, nature sometimes seems too clever for us.

Polygons form by the intersecting ridges of sand dunes. If this deposit were to become indurated and eroded, we might not be able to tell that they originated as wind-blown dunes, and interpret the polygons as evidence for a dried-up lake, for example. Dunes often accumulate in the bottoms on craters, also a good setting for a (temporary) lake.

The illumination is coming from the upper left, so the bluish ridges are high-standing.


  This image covers many shallow irregular pits with raised rims, concentrated along ridges and other topographic features. How did these odd features form?
  
  One idea is that they could be from sublimation of shallow lenses of nearly pure ice, but why do the pits have raised rims? They can’t be impact craters with such fortuitous alignment and irregular margins. They aren’t wind-blown deposits because there are many boulders, too big to be moved by the wind. There are younger wind-blown drifts on top of the pits, and there’s no clear connection to volcanism.
  
  Some speculate that there were ancient oceans over this region—could that somehow explain these features? Ancient glaciation is another possibility, perhaps depositing ice-rich debris next to topographic obstacles.Future images of this region may provide clues, but for now this is a mystery.

This image covers many shallow irregular pits with raised rims, concentrated along ridges and other topographic features. How did these odd features form?

One idea is that they could be from sublimation of shallow lenses of nearly pure ice, but why do the pits have raised rims? They can’t be impact craters with such fortuitous alignment and irregular margins. They aren’t wind-blown deposits because there are many boulders, too big to be moved by the wind. There are younger wind-blown drifts on top of the pits, and there’s no clear connection to volcanism.

Some speculate that there were ancient oceans over this region—could that somehow explain these features? Ancient glaciation is another possibility, perhaps depositing ice-rich debris next to topographic obstacles.Future images of this region may provide clues, but for now this is a mystery.

“Maybe we’re on Mars because of the magnificent science that can be done there - the gates of the wonder world are opening in our time. Maybe we’re on Mars because we have to be, because there’s a deep nomadic impulse built into us by the evolutionary process, we come after all, from hunter gatherers, and for 99.9% of our tenure on Earth we’ve been wanderers. And, the next place to wander to, is Mars. But whatever the reason you’re on Mars is, I’m glad you’re there. And I wish I was with you.” — Carl

“Maybe we’re on Mars because of the magnificent science that can be done there - the gates of the wonder world are opening in our time. Maybe we’re on Mars because we have to be, because there’s a deep nomadic impulse built into us by the evolutionary process, we come after all, from hunter gatherers, and for 99.9% of our tenure on Earth we’ve been wanderers. And, the next place to wander to, is Mars. But whatever the reason you’re on Mars is, I’m glad you’re there. And I wish I was with you.”Carl

Fuck yeah they finally decided to radar one of the Mars HiRISE pics I’ve featured, you deserve it bby. Witcha gorgeous martian self.

beautifulmars:

South Pole Residual Cap Interannual Change Monitoring - 

beautifulmars:

South Pole Residual Cap Interannual Change Monitoring - 


  Megabreccia on the Floor of an Impact Crater in Mars
  
  “Megabreccia” is a term we use to describe jumbled, fragmented blocks of rock larger than 1 meter across, in a matrix of finer-grained materials. It’s the result of energetic processes, typically from an impact event.
  
  This image was acquired by HiRISE only in the narrow color strip, as a ridealong with a CRISM target, since HiRISE had previously imaged this location.

Megabreccia on the Floor of an Impact Crater in Mars

“Megabreccia” is a term we use to describe jumbled, fragmented blocks of rock larger than 1 meter across, in a matrix of finer-grained materials. It’s the result of energetic processes, typically from an impact event.

This image was acquired by HiRISE only in the narrow color strip, as a ridealong with a CRISM target, since HiRISE had previously imaged this location.

beautifulmars:

Jeans Crater Dunes - Defrosting going on all over the place here. http://www.uahirise.org/ESP_030181_1105 

beautifulmars:

Russell Crater Dunes - 

beautifulmars:

Richardson Crater Dunes Sublimation - Sublimation is the process of going directly from a solid state to a gaseous one. In these cases, the process can expose darker subsurface material that fan outward, and are also moved by the wind.

Hey just an fyi to you all, Beautiful Mars, to my understanding is an official NASA HiRISE run blog with a constant stream of updates from HiRISE (High Resolution Imaging Science Experiment) which acquires data from Martian landforms via the Mars Reconnaissance Orbiter (MRO) mission. And if you’ve been a long time follower you know how much I love me some HiRISE updates so go follow!

beautifulmars:

Richardson Crater Dunes Sublimation - Sublimation is the process of going directly from a solid state to a gaseous one. In these cases, the process can expose darker subsurface material that fan outward, and are also moved by the wind.

Hey just an fyi to you all, Beautiful Mars, to my understanding is an official NASA HiRISE run blog with a constant stream of updates from HiRISE (High Resolution Imaging Science Experiment) which acquires data from Martian landforms via the Mars Reconnaissance Orbiter (MRO) mission. And if you’ve been a long time follower you know how much I love me some HiRISE updates so go follow!

Used Parachute on Mars Flaps in the Wind


  Image credit: NASA/JPL-Caltech/Univ. of Arizona
  
  This sequence of seven images from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA’s Mars Reconnaissance Orbiter shows wind-caused changes in the parachute of NASA’s Mars Science Laboratory spacecraft as the chute lay on the Martian ground during months after its use in safe landing of the Curiosity rover.

Used Parachute on Mars Flaps in the Wind

Image credit: NASA/JPL-Caltech/Univ. of Arizona

This sequence of seven images from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA’s Mars Reconnaissance Orbiter shows wind-caused changes in the parachute of NASA’s Mars Science Laboratory spacecraft as the chute lay on the Martian ground during months after its use in safe landing of the Curiosity rover.


  Dark Rays and Light-Tones
  
  This image shows a relatively youthful crater with dark rayed ejecta and a light-toned zone that extends beyond that ejecta.
  
  The lighter-toned surface might be the “blast zone” as darker regolith material was ” blown away” during the impact event. With HiRISE resolution, we can see that this is the wrong explanation. Instead, the bright ejecta consists of indurated fine materials, such as dust trapped by the roughened surface, then cemented over time.

Dark Rays and Light-Tones

This image shows a relatively youthful crater with dark rayed ejecta and a light-toned zone that extends beyond that ejecta.

The lighter-toned surface might be the “blast zone” as darker regolith material was ” blown away” during the impact event. With HiRISE resolution, we can see that this is the wrong explanation. Instead, the bright ejecta consists of indurated fine materials, such as dust trapped by the roughened surface, then cemented over time.

Private Plan to Send Humans to Mars in 2018 Might Not Be So Crazy

Side Note: A few days ago I highlighted an article from WiredScience that delved into the idea, and even serious plans of humans undergoing a 501 day trip to Mars in the year 2018 and I recall many of you thought it was downright madness, a near impossibility due to our technological restraints. But is it really that crazy of an idea at this point in space exploration’s progression considering what has already been achieved? While the mission doesn’t necessarily send humans into Mars but close to its orbit much the same way astronauts like Chris Hadfield navigate close to Earth’s orbit in the International Space Station, it still provides a trove of data and experience much needed in our later attempts to actually try and colonize Mars. This follow up explains the mission a little more and gets into its possibility and chances of success.

This bold undertaking is planned by the Inspiration Mars Foundation, a non-profit company founded by millionaire and space tourist Dennis Tito that was officially unveiled on Feb. 27 after early details leaked. Though the spacecraft would not land humans on Mars or even put them in orbit, it would bring people within a few hundred kilometers of the Martian surface — roughly the same distance between the International Space Station and Earth — and represent a major milestone in human spaceflight. If successful, the mission would go down in history as the first time a private company accomplished something government agencies were unable to do in space.

The mission is extremely ambitious, well beyond anything previously accomplished by the private sector and it faces plenty of obstacles. The company has an aggressive schedule to keep if it wants to hit its 2018 mark and needs to make sure the necessary technology is developed and well-tested. Despite its deep-pocketed backer, the mission has nowhere near the funding it needs to launch and will require raising greater sums than have ever been done for a private space endeavor. Its designers also need to figure out exactly how to keep the crew healthy, both physically and psychologically, for the 501-day duration of the flight as they face dangers from radiation, bone and muscle loss, fatigue, and depression. Mission designers will have to ensure they can get the crew safely to the ground when the capsule returns to Earth at a screaming 30,000 mph.

Yet despite these hurdles, of all the bold announcements from private spaceflight companies in recent years, this one seems the most achievable.

“The reason this entire thing is possible is because it’s actually a very simple mission,” said Jane Poynter, president of the Paragon Space Development Corporation, which makes life-support systems and has partnered with Inspiration Mars. “We’re not trying to land, we’re going to fly by and we’re using extant technologies that NASA and the space industry have been developing for years.”

Inspiration Mars isn’t looking to sell a product in an unknown market, like the asteroid-mining Planetary Resources or the national-moon-ferrying Golden Spike Company, and doesn’t have incredibly aspirational aims, like the planet-colonizing Mars One. It hopes to undertake a straightforward mission that could spur innovation, inspire young scientists and engineers, and move human spaceflight forward.

“You have to have a reasonable degree of skepticism and realism,” said Taber MacCallum, who co-founded Paragon with Poynter (and is also her husband). “We might run into some insurmountable obstacle 18 months in. But with proper engineering, support, and a good mess of luck, we could see this done.”

Now all they have to do is actually fly to Mars.

Head on over to the article for more details!

beautifulmars:

Gullies on Hills in Center of Hale Crater (1 of 3) - 

beautifulmars:

Gullies on Hills in Center of Hale Crater (1 of 3) -