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The sanford guide to antimicrobial therapy 2013 noble 42nd edition

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Try using another card. � D-brief |� The Crux |� Body Horrors |� Citizen Science Salon |� Dead Things |� The Extremo Files |� ImaGeo |� Inkfish |� Lovesick Cyborg |� Neuroskeptic |� Out There |� Science Sushi |� Seriously, Science?

|� Field Notes | On Sunday, skydiver Felix Baumgartner stepped out of a high-altitude balloon and plummeted 40 kilometers back to Earth. I wanted to watch it live but missed it due to an appointment I had to keep. I heard it was heart-pounding, and Twitter went nuts over it.

I wish I had seen it!Still, my feelings on it are mixed. While I really am glad it got people excited, I couldn�t shake the feeling it wasn�t more than a stunt. A cool stunt, but a stunt. It was plugged as a way to learn more about spacesuits and all that, but I had my doubts. Having it sponsored by a sugary caffeinated energy drink marketed to teens also made me a bit wary.I was thinking of writing something up about it, but then my friend and space historian Amy Shira Teitel wrote an excellent piece crystallizing my thoughts, so go read her article for more in that vein (which is also mirrored on Discover Magazine�s blog The Crux).But what I really wanted to write about was this image I saw around Twitter and Facebook:Why do I want to write about this?

Because, in a nutshell, it�s everything wrong about attitudes on our space program. If I sound a little peeved, I am. Here�s why.This meme was started in a tweet by revulv. I suspect it was just a joke, and to be honest it�s funny enough; I smirked when I read it. But someone took that joke and added the picture, and then it got spread around. And I can tell by the comments I�m seeing people really think it�s true � this idea has been around since the Shuttle retired, and it�s unfair.

It�s simply not true.First, as Amy points out in her post, Baumgartner�s jump was a record breaker, but he wasn�t in space. Our atmosphere thins out with height, and doesn�t really have an edge where air ends and vacuum begins. Because of this, there�s an arbitrarily agreed-upon height where we say space "starts" � it�s called the Karman line, and it�s 100 km (62 miles) above sea level. Baumgartner was less than half that high.

When I talked about his jump I used the phrase "edge of space", which is probably fair. He was in a pretty good vacuum by ground standards, but in space itself he was not.Second, he wasn�t in orbit.

A lot of folks confuse being in orbit and being in space, which is understandable. When we say something is in space that means it�s just higher than that arbitrary limit. You can get there via rocket by going straight up 100 km and then back down, for example.

That�s a suborbital flight.But being in orbit is different. An orbit is where you are free-falling around the Earth. Think of it this way: in orbit the Earth is pulling you down to the surface, but you�re going fast enough sideways that you never actually hit (to paraphrase Douglas Adams: orbiting is learning how to throw yourself at the ground and miss). Your velocity down and your velocity to the side add together to give you a circular (or elliptical) path.Baumgartner used a balloon to go straight up.

He wasn�t in orbit.And that�s two of the three things that bother me about that meme picture: he wasn�t in space, and he wasn�t in orbit, two things the US has rockets that can do.Now, some people will point out that in fact the US cannot do that, at least not with people.

We don�t have any rockets rated for human flight into space.That�s true, but brings up my third point, the most important, what a lot of people don�t seem to get: you need to add the words "right now" to the end of that sentence.We can�t launch humans into space right now. But in just a few years we�ll have that ability. In spades.SpaceX is working on making sure their Falcon 9 rocket is human-rated for flight � even as I write these words they have a Dragon capsule berthed to the International Space Station.

ATK is another. There�s also Sierra Nevada, Blue Origin (which just had a successful engine firing test), XCORR, and others. Let�s the sanford guide to antimicrobial therapy 2013 noble 42nd edition forget Virgin Galactic, too. [Update: D�oh! Shame on the sanford guide to antimicrobial therapy 2013 noble 42nd edition, and ironic too: I forgot to add Boeing and ULA�s work on the sanford guide to antimicrobial therapy 2013 noble 42nd edition as well.]Both SpaceX and ATK think they�ll be ready to take people into orbit in 2015.

Virgin Galactic and XCORR may be ready to do commercial suborbital flights before that date. [Note added after posting: I want to be clear; these are not NASA programs, but some have contracts with NASA, and I�m talking about the US as a nation, not necessarily as a government space program.]The Space Shuttle was retired in 2011. We�re in the middle of what�s planned to be a five year gap where the US can�t take humans into space.

Mind you, when the Apollo program shut down there was a nine year gap before we had a program to take humans to space again (with the exception of a few Saturn flights to orbit for Skylab and the Apollo-Soyuz mission; even then there was a six year gap until the Shuttle launches began).My poi� D-brief |� The Crux |� Body Horrors |� Citizen Science Salon |� Dead Things |� The Extremo Files |� ImaGeo |� Inkfish |� Lovesick Cyborg |� Neuroskeptic |� Out There |� Science Sushi |� Seriously, Science?

|� Field Notes | I am endlessly fascinated by the Moon. There may be an inherent bias there because it is, after all, the closest astronomical object in the sky. Still, it has an amazingly varied surface with lots of really odd features.One of my favorite types of things to look at are overlapping features. It can produce a very complicated terrain, difficult to understand. Or can also create a lovely tableau that cleanly separates the two features, like this very pretty shot from Lunar Reconnaissance Orbiter (LRO) showing a fresh crater near a graben:[Click to enlunenate.]A graben is a crack or fracture.

They form on the Moon when the crust is stretched, splitting the surface. They look like long, relatively straight and narrow valleys with steep sides. You can only see a part of it on the right side of the image above; the Sun is shining from the right and illuminating the left-hand side of the graben.

The picture below is zoomed out and should help you see the situation.The crater is clearly younger than the graben feature. The radial streaks around the crater are called rays, and are formed when plumes of material ejected from the impact fall back down to the ground. They�re common around young craters; solar wind, later impacts, and even thermal compression and expansion of rocks over the Moon�s day-night cycle eventually erode them away.You can see the rays extended over and into the graben, so the crater must be younger.

It�s hard to say just how much younger, but even relative ages can help geologists understand the lunar surface better. And detailed images like this � you can see individual blocks of rock inside the crater itself � are crucial for study. Someday, I think, human geologists will be investigating places like this in person, and mapping missions like LRO will make that possible.Image credit: NASA/GSFC/Arizona State UniversityRelated Posts:� A fresh Martian impact� Ash hole on the Moon� Peaking into lunar craters� Clair de Mercury One of the more enduring questions about the Apollo Moon missions is seemingly simple: after 40+ years, are the flags the astronauts planted on the lunar surface still there?It�s an interesting question.

Buzz Aldrin claims he saw the flag blow over when the ascent module carrying him and Neil Armstrong lifted off from the Moon � which was never confirmed (until now; hang on for that), but the fates of the flags from the other five missions have never been ascertained. In 2009 there was tantalizing evidence the flags from Apollo 17 was still standing, but the images were just barely too fuzzy to know for sure.But now, apparently, we do know: the Lunar Reconnaissance Orbiter has now confirmed that the flags at all the landing sites are still there, except for Apollo 11.

It looked like Buzz was right!Here�s an image showing the Apollo 16 flag:The flag itself is visible in the picture � LRO�s angle on it shows the shadowed side, which is slightly darker than the the sanford guide to antimicrobial therapy 2013 noble 42nd edition surface � and the shadow it casts on the surface is obvious.I have to admit, I�m surprised *.

The flags were made of simple nylon, which can disintegrate when exposed to ultraviolet light. I figured that after all this time they�d be nothing more than red, white, the sanford guide to antimicrobial therapy 2013 noble 42nd edition blue powder at the base of their poles. I guess I was wrong. And I�m happy to be! [UPDATE: In the comments below, BABloggee Maxx points out that polymers need oxygen to be degraded by UV light, so this may be why the flags haven�t disintegrated.]That picture from Apollo 16 is impressive, and I have to admit, that�s my favorite flag of the missions.

It�s where Charlie Duke took a picture of John Young doing a "big Navy salute" � Young jumped up, and Duke snapped the photo while Young was still off the surface (not while he was in the air, of course, since that�s a commodity the Moon lacks):Read More Large impacts are fascinating.

There�s the thriller-movie aspect of them, of course, spiced with enough reality to make them legitimately scary. But the physics of them is equally enthralling, and complex enough that it will be a rich field for scientists to study for years to come.The good news for both these aspects is our Moon.

Seriously! There are enough craters there for anyone to be happy studying them, and since the Moon is a giant lifeless chunk of rock, impacts there seem less urgently threatening.I want to show you two craters on the Moon that are very different, and therefore very interesting.First up, Copernicus.

Or more accurately, a small part of this 90+ km (55 mile) wide impact feature: its central peaks.[Click to enselenate.]This image was taken by NASA�s wonderful Lunar Reconnassance Orbiter. Copernicus is a big crater, and easy to spot even with binoculars since it sits in a vast lava plain; the surrounding material is d� D-brief |� The Crux |� Body Horrors |� Citizen Science Salon |� Dead Things |� The Extremo Files |� ImaGeo |� Inkfish |� Lovesick Cyborg |� Neuroskeptic |� Out There |� Science Sushi |� Seriously, Science?

|� Field Notes | Because the planets are so terribly old, and impacts so rare, I still have this (very slight) prejudice that craters are old too. The Moon was bombarded billions of years ago, and the craters on Earth are mostly so old that they�ve eroded away. Heck, even a "new" crater like the one in Arizona is tens of thousands of years old.Getting the age of a crater can be tricky. But sometimes it�s so easy it�s literally a matter of keeping your eyes on one spot.

Like this spot on Mars:That image (highly color enhanced; click here for a grayscale version) shows a crater seen by a camera on the Mars Reconnaissance Orbiter in 2011. We can tell it�s young because it�s still surrounded by the ejecta blanket; material that blasted out of the crater and settled around it. That stuff tends to erode away (or get covered in dust and sand by Martian winds) relatively quickly.But in this case, we know just how young it is: it wasn�t seen in images taken of the same spot by a camera on board the Odyssey Mars probe� in 2009!

In other words, this crater is less than three years old!That�s so cool. And it speaks to the power of having multiple, sustained missions to other worlds. Things change. If we take one picture and then walk away, we�ll miss a lot.Image credit: NASA/JPL/University of ArizonaRelated Posts:� Water on (shakes Magic 8 ball) Mars this time� Kablam!� New study finds giant impacts aren�t the sanford guide to antimicrobial therapy 2013 noble 42nd edition I think the Moon watched Bad Universe Large impacts are fascinating.

There�s the thriller-movie aspect of them, of course, spiced with enough reality to make them legitimately scary. But the physics of them is equally enthralling, and complex enough that it will be a rich field for scientists to study for years to come.The good news for both these aspects is our Moon.

Seriously! There are enough craters there for anyone to be happy studying them, and since the Moon is a giant lifeless chunk of rock, impacts there seem less urgently threatening.I want to show you two craters on the Moon that are very different, and therefore very interesting.First up, Copernicus.

Or more accurately, a small part of this 90+ km (55 mile) wide impact feature: its central peaks.[Click to enselenate.]This image was taken by NASA�s wonderful Lunar Reconnassance Orbiter. Copernicus is a big crater, and easy to spot even with binoculars since it sits in a vast lava plain; the surrounding material is darkish grey, while the crater is far brighter.

It�s also surrounded by a gorgeous system of rays: linear streaks caused by the collapsed plumes of material after the asteroid or comet smacked into the Moon to form the crater itself.Copernicus has a series of mountains in its center, the tallest over a kilometer high.

These weren�t created in tectonic events like on Earth, though! Giant impacts that cause big craters have weird physics. The pressure upon impact can be so high that the rock in the surface flows like a liquid.

It splashes outward, then flows back in, surging upwards in the middle of the impact point. This video showing water dropping into various surfaces might help:Lots of craters have such central peaks (like Tycho). But not all� like the spectacular Giordano Bruno, an impact crater on the lunar far side measuring 21 km (13 miles) across:Read More Someday, Mars will stop surprising me.Today is not that day.The image below was taken by the HiRISE camera on the Mars Reconnaissance Orbiter, which has been taking devastatingly high-res pictures of the Red Planet for many years.

While passing over the edge of the Tharsis Shield � a huge uplifted region of Mars home to its four gigantic volcanoes �it saw this bizarre fieldof craters:[Click to hephaestenate.]First, you may think these are mounds and not craters, but that�s an illusion. Our brain uses illumination to gauge up and down in pictures like these, and assumes the sunlight is coming from above.

However, these really are craters, but the illumination is coming from below � north is roughly toward the top of the picture and the crater field is at a northern latitude of about 50�. Flip the picture over if it helps (I�ll be honest, even doing that makes it hard for me to see these as other than mounds; confounded brain!). You can see more examples of this illusion here, here, and here.But that�s not the weirdest thing about these craters.

What�s really odd is they aren�t circular! Impacts are generally round unless 1) the impact is at a very shallow angle, b) the terrain suddenly goes from one kind of material to another, creating a discontinuity, or ?) something happened after the crater was formed to distort it.A shallow-angle impact is almost certainly not the case here, since there are so many craters spread out over the region that an incoming object would�ve had



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