NASA Rover Finds Old Streambed on Martian Surface
jpl.nasa.gov
jpl.nasa.gov
Mars was formed around the time Earth was, but it was blessed with only 11% of Earth's mass and less than 40% of Earth's gravity field. Shortly after cooling solid, its "Noachian Era" was similar to proto-earth: warm, a thick atmosphere, plenty of liquid water on the surface, and probably a significant magnetic field.
But this era was still during the era of the Late Heavy Bombardment, a time in which the last dregs of the solar system were still settling out. Large asteroids still pounded the planets with regularity.
Unlike Earth, Mars had trouble maintaining its liquid iron magnetic field. Since it's much smaller, it cooled and thus congealed faster. And there's growing evidence that asteroid impacts were able to drive enough heat beneath the surface that interior convection was quelled, leading to a fragmented magnetic field.
Without an adequate magnetic field to deflect solar wind, the atmosphere was prone to shedding off pieces of itself into space. This was amplified by the lower gravity which meant holding on to lightweight gasses was even harder.
Over time, Mars cooled to the point where the major forms of tectonics ceased. The water locked up beneath the ground, rusted out pulverized basalt dust from the asteroid impacts, and frizzled in the radiation-baked atmosphere, floating off.
The seas and lakes dried, the rain stopped, and that... was that.
Three billion years later, we arrive on the scene and find out we have a little sibling. Then we send robots. We hope to find life, or evidence that it once lived. Characterizing how water worked in the Martian past is a part of answering that question.
> The seas and lakes dried, the rain stopped, and that... was that.
We think there was water on mars, therefore it is true. Is it too much to put a disclaimer somewhere that explains this is the current consensus but we have more to learn? The truth is that this story is riddled with assumptions, and readers need to know that.
Pith is the central idea or essence of something. If you’re in danger, you could exclaim, “I would greatly appreciate it if someone would provide assistance.” Or, you could get right to the pith of your point by shouting, “Help!”
Following along this line of inquiry, one is led to consider the possibility (however remote) of this being an example of near-humour. Possibly of the genus: Pun, species: indirect. So, if one were to dress this up, it is perhaps alluded to as a Punnus Indirrectus.
Or, maybe Not. =D
I think a simple opening statement like "our current theory is" followed by the main text would be more than enough, but it is good to remind people that theories are just that - theories.
a proposed explanation whose status is still conjectural and subject to experimentation
but the scientific usage includes the fact that lots of facts have already been evaluated, and even that the new predictions by the theory have already been evaluated and found to be true.
It's been evaluated and found to be true...for now. Almost every major scientific discovery upends some form of thinking or fact that we had accepted up until new information is found.
A scientist might make a hypothesis that suspect A is the murderer; the prediction would be that the murder weapon would be found in their house, the fingerprints match, blood types match. Upon search, the murder weapon was actually found, and fingerprints and blood types match.
A layman would say that finding the weapon converted the theory into a nearly certain fact.
A scientist would say that finding it pushed the hypothesis towards being a theory.
I don't see how anyone would object to this definition of a theory.
The nugget of truth in your statement is that some assumptions we are more sure of than others. We can probably say how old Mars is with more certainty than how much water there was on there. That may or may not need to be clarified, depending on what the focus of the conversation is.
So: "A positive correlation was found between X and Y"--why are you even telling me? What's the message? "There is evidence that X might cause Y"--okay, how strong is this evidence? Is it enough to care? "X probably causes Y"--that is what you're really trying to say. I will hear that and put it though my own Bayesian updating to give slightly more credence to the statement that X causes Y (more or less depending on the trustworthiness of the source, where I read it, what other supporting statements were made, etc.) The previous two forms don't change this mental process one bit, except to make it harder to dig out the thing you were actually trying to get across.
Also, while it is true you will give up some brevity while you practice accuracy, eventually you will learn to write better and either shorten your posts again or present them in a more compelling way so that your readers do not notice the length much.
There's a time and place for them. I don't think this was it.
When you react to something like this are your saying "I don't like narratives being presented to me like this. or "I don't want narratives being presented to people dumber than me like this."?
Major: 96.5% Carbon Dioxide (CO2), 3.5% Nitrogen (N2)
Minor (ppm): Sulfur Dioxide (SO2) - 150; Argon (Ar) - 70; Water (H2O) - 20;
Carbon Monoxide (CO) - 17; Helium (He) - 12; Neon (Ne) - 7
That's interesting because if you take away the products of volcanism (a major source of sulfur dioxide and carbon dioxide here on Earth), you're left with... Nitrogen... Argon... Water... and noble gasses. Look familiar?The best thinking right now is that Earth outgassed and held on to a similar volume of gasses as Venus. But since we had a substantial volume of liquid water on the surface, the oceans naturally absorbed CO2 and then deposited it on the sea bottom as carbonate minerals. (Life eventually learned that trick too, leading to things like shells)
So limestone, dolostone, chalks, calcite, marble, etc.... all those carbonates are likely the product of our liquid water oceans drawing out the vast bulk of the C02 in our atmosphere, leaving relict gasses in its place. Same starting point but we ended up with vastly lower pressure and vastly different final composition.
Venus had no such luck. She suffocates forever.
http://nssdc.gsfc.nasa.gov/planetary/factsheet/venusfact.htm...
In short, scientists think there has to be a convecting, rotating, liquid metal core in order to create a substantial magnetosphere. Venus's planetary core is almost certainly missing one, two, or three of those things.
The fact that Venus is extremely hot on the surface (460ºC) is at least partially assisting with creating a "stagnant lid" tectonic regime where no heat-venting plate action is seen. So if the surface of the planet is nearly as hot as the mantle and the mantle is nearly as hot as the core, convection doesn't happen. Wiki "geothermal gradient" for more.
Thus no magnetosphere, thus no electromagnetic deflection of the sun's blast. Not a dealkiller, but certainly not preferable if you'd like to move in someday.
http://spacemonitor.blogspot.com/2007/05/floating-city-on-ve...
http://www.flickr.com/photos/europeanspaceagency/3694512868/
Check the lat/long co-ordinates.
But it's a very small amount of the suspected former total (perhaps 10% to 1% or much less). Assuming that the Martian canyons and valleys that appear to be carved out by water were actually carved out by water, they were absolutely torrential floods - of a scale unlike ever seen on Earth. Now? Ice glaze. Polar snow flurries. Underground ices. Hypersaline water tables, perhaps. Dusty crusty dune ice at the poles.
It's not so much that the Martian hydrosphere isn't present, it's that it doesn't resemble ours much at all. And figuring out how life might fit into the present day is tricky: Mars is essentially a much drier and colder Antarctica.
I'm not sure if Mars suffers impacts from it, but impacts from sources such as the Oort Cloud (http://en.wikipedia.org/wiki/Oort_cloud) often contain ice and other materials. There are other examples if you search around.
The universe is a big and crazy thing, the possibilities of what can and have happened are almost endless.
An article from 2007 on the debate : http://www.newscientist.com/article/dn12026-mars-rover-finds... there are still some that believe at 'just the right time and place' you could get liquid water on the surface, but everyone seems to think it would be short lived.
The story of Mars in short: flop planet, can't hydrosphere.
There is extremely strong evidence that in the very early years Mars was capable of holding on to a great deal of water: Enough to cover the Southern Hemisphere. The streambed seen here is from that time.
That downer is that this was over 3 billion years ago. Through a variety of processes and for a number of reasons most of Mars' water was lost to space or trapped underground.
The billion-dollar question that would be epic to answer: Did Mars develop Or acquire life during the time it had liquid water on the surface and if so is there any trace of it left, alive or dead?
That's an interesting, and very specific number that I hadn't heard before. Is there a story behind that?
For starters, the remaining atmosphere on Mars is extraordinarily thin. Go to the top of Mt. Everest. Then go four times higher than that. That's the atmospheric pressure at "sea" level on Mars.
It's apparently relatively easy to determine atmospheric composition from afar, and of the atmosphere remaining on Mars, 210 parts per million is water. I have not done the math myself, but I'm assured the total "depth" of water left is measured in microns.
It's really dry. It's really cold. And we'd pop like a balloon stepping outside.
As for how much water is frozen below? SHRUGGGGGG Anyone could make a career answering that. The biggest confounding factor is that the planet is substantially covered in dust, many meters thick in places. It makes remotely sensing what's underneath a real pain in the ass.
The most solid answer so far appears to be "there is a nontrivial amount of ice below the ground". Think "enough to fill the great lakes".
Temps above freezing have been reported by Curiosity, which is interesting in itself.
http://imagine.gsfc.nasa.gov/docs/ask_astro/answers/970603.h...
From the article, "... This is the first time we're actually seeing water-transported gravel on Mars. This is a transition from speculation about the size of streambed material to direct observation of it ..."
What's cool about that is that it allows you to directly calculate how much water flow was involved in moving this gravel (taking in to account the much lower Martian gravity), you can use the pattern in which the gravel deposited itself to determine what direction the flow was going, and more.
Why isn't this front page, the implications are staggering.
Good point. The theory of a flowing river should support all types of evidence at large & small scale: alluvial fans,
"... The imagery shows an alluvial fan of material washed down from the rim, streaked by many apparent channels, sitting uphill of the new finds. ..."
to pebbles and rate of flow of liquids,
"... From the size of gravels it carried, we can interpret the water was moving about 3 feet per second, with a depth somewhere between ankle and hip deep... This is the first time we're actually seeing water-transported gravel on Mars. This is a transition from speculation about the size of streambed material to direct observation of it. ..."
All directly observable evidence, each piece confirming the conclusion.
Water has always been supposed to have played a role in the state of Gale Crater, and it must have been moving water at some point...
If life came to Earth aboard a comet (as opposed to developing here), it most likely arrived on Mars as well. In that case, the early solar system was probably teeming with life (seeds), and in that case, it could be very common elsewhere.
Also, if there was ever a significant amount of organic matter in that stream, we may be able to find out about it through the SAM instrument. It turns out someone was planning ahead and shipped a gas chromatagraph with a mass spectrometer and laser spectrometer attached. You know, just in case we wanted to pick up some dirt and figure out what the heck sort of complex chemicals are in it. Which we do!
The cemented section on the mars side is in itself most interesting I find and yet seem unable to state why. Wonderous stuff indeed.
Out of interest, how do we know it was water, and not some other liquid?
Furthermore, most liquids found at reasonable temperatures aren't all that voluminous, and a number of the minerals scanned and inspected on Mars show evidence of water contact.
Basically, there's not much else it could be. :) That said there's some really cool theorizing on underground carbon dioxide flows that might explain some washouts seen later in Mars's life.
you mean these? "small spherical hematite balls, dubbed ‘blueberries,’" ~ http://www.lifescientist.com.au/article/436306/iron_blueberr... Goethite: learn something new every day.
My mind is teeming with excitement of the possibilities, is anyone else as excited as me?
Earth has a hot, churning, iron core and therefore still has a strong magnetic field to protect our atmosphere from the solar wind. Mars cooled long ago and its magnetic field weakened.
It would also be fun to discover that in its first billion years of existence as a wet planet Mars supported life in one form or another, simply to give us a data point in the probability function.
Imagine what that would do to culture, mythology, technological development...
If traces of life are found, however distant in the past, it seems quite likely that any Mars colony or even exploration would be delayed by decades, if not longer. Preservationists would be against any interaction whatsoever.
If it's not sentient, it doesn't have a moral claim to the planet.
It's tiresome hearing of the "piling evidence" for water on Mars. Find some damn water. Prove it by melting it then boiling it on camera in a container with a thermometer.