IPB

Welcome Guest ( Log In | Register )

Water oceans on mars?, Images of different water oceans on mars based on MGS MOLA instrument.
Guest_Magnus Lundstedt_*
post Mar 14 2006, 11:20 PM
Post #1





Guests






I have just completed a fun little afternoon project. I have long been looking for what an ocean on mars would look like for different amounts of water - preferably with a movie for many different ocean heights. So after not finding it ever, I did it myself today:

http://magnus.infidyne.com/mars/water/
Go to the top of the page
 
+Quote Post
 
Start new topic
Replies
Guest_Richard Trigaux_*
post Mar 15 2006, 11:56 AM
Post #2





Guests






There are still many things strange and unknown about water on Mars.

For instance, if you look at Google mars you notice that huge surges of water (or at least liquid) created hyper large flow channels leading from Tharsis dome to the northern plains. The springs of these water flow are graben-like hollows which are Vales marineris itself, of parallel to it. It is really ununderstandable, it is as if there was a huge eruption of water from underground, associated with major geological features. Could magma chambers differentiate to such an extent that they contain only water? All along the southern plateau, flow marks gather water which apparently rained over this plateau, for instance Maadim Vallis, which filled the Gusev crater (Spirit landed on this filling). Other flow marks lead to Helas basin, but were apparently unable to fill it with sediments.


So whatever how this happened, it is clear that Mars, usually very dry, experienced brief episodes of flooding, and thus free liquid water on its surface, and thus a temporary atmosphere of steam. Could such an atmosphere lock Mars in a state of greenhouse heated planet? Perhaps yes, but obviously this did not happened. So in a matter of weeks, or even days, the free water was covered with ice, and likely froze to the heart in some years. Maybe this frozen ocean is still there, in the northern plains, covered with a layer of dust which prevents it from sublimating.

And steam in the atmosphere? Likely most of its molecules are broken by UV light, and hydrogen escapes. The reminder forms oxygen and hydrogen peroxyde, which are still present in Mars atmosphere today. Such an oxydizing atmosphere is the responsible of the reddish colour of Mars (by oxydizing iron).
Go to the top of the page
 
+Quote Post
Guest_Magnus Lundstedt_*
post Mar 15 2006, 01:49 PM
Post #3





Guests






Yeah I have seen those. But what I dont understand is why it has to be "huge surges"; why not a smaller continious flow during a million years or so? (if we assume mars could have hold significant amounts of water for that long)

If mars was always very dry, one explanation can be no/little water, but could not another explanation be that while there was huge oceans for a short time and a few rivers leading out to it; verry little rain fell on the landmass resulting in a very dry (desert-like) landmass, most of the steam in the atmosphere never condesated back to rain - it just ended up beeing blown away from the planet high above the surface? Maybe the larger water-outflows from the olympus-mons area is due to increased rainfall / direct condensation on mountain walls, due to more cooling of that area during night (because of extreme altitude).

Well, what I wonder is; do we really KNOW that: (and if so how, what proofs are there?)

1) There was verry little/no water on mars surface
2) The big river-like features was formed in great surges of water (and not wind, or water during X million years?)
3) That Vales marineris was formed after water under it erupted. Cant there be other explanations for that formation, for example deformation of the planet after the evaporation of a hypothetical ocean?
4) It is not possible that entire water molecules or H + O2 molecules separateley gets blown away high above mars surface. If we would have a ground atmospheric pressure of around that of earth, on mars, I assume the highest layers of the atmosphere would be quite far away from the surface; thus the force of gravity acting on those molecules would be far lower than that force on the molecules high up in earths atmosphere. Thus solar winds might be able to blow away larger and heavier atoms/molecules?

It would be intresting if there are any papers on this matter.
Go to the top of the page
 
+Quote Post
Guest_Richard Trigaux_*
post Mar 15 2006, 03:29 PM
Post #4





Guests






QUOTE (Magnus Lundstedt @ Mar 15 2006, 02:49 PM) *
Yeah I have seen those. But what I dont understand is why it has to be "huge surges"; why not a smaller continious flow during a million years or so? (if we assume mars could have hold significant amounts of water for that long)



Why "giant surges"? because these water beds are huge, 100kms large or more, while showing erosion-sedimentation marks of a mountain torrent. So the flow was much larger than Earth's Amazon, and much faster, implying a flow rate several orders of magnitude greater than anything known on Earth. Such a flow rate would have quickly filled an ocean, so it cannot have lasted millions of years. The mystery is where this water came from, and how such a quantity made to the surface, apparently from underground. The most commonly accepted explanation is that Mars had a watertable, of a mixture of water and carbon dioxid. At the occasion of a tectonic process, the pressure released, inducing a massive boiling of the carbon dioxid and the release of a torrent of mud. Personally I add that some volcanic eruptions may have released huge clouds of steam, carbon dioxyd and dust. But until now nobody can be sure of what happened.


QUOTE (Magnus Lundstedt @ Mar 15 2006, 02:49 PM) *
... I assume the highest layers of the atmosphere would be quite far away from the surface; thus the force of gravity acting on those molecules would be far lower than that force on the molecules high up in earths atmosphere.




The gravity at high altitude (100 to 300kms) is not much smaller than on the ground. The ability of a planet to retain its atmosphere depends mainly on its gravitation, but also on its temperature and composition, and in a less extent on processes like UV or solar wind (if the later is not shielded by a magnetic field).
Go to the top of the page
 
+Quote Post
RNeuhaus
post Mar 17 2006, 12:55 AM
Post #5


Senior Member
****

Group: Members
Posts: 1636
Joined: 9-May 05
From: Lima, Peru
Member No.: 385



QUOTE (Richard Trigaux @ Mar 15 2006, 10:29 AM) *
Why "giant surges"? because these water beds are huge, 100kms large or more, while showing erosion-sedimentation marks of a mountain torrent. So the flow was much larger than Earth's Amazon, and much faster, implying a flow rate several orders of magnitude greater than anything known on Earth. Such a flow rate would have quickly filled an ocean, so it cannot have lasted millions of years. The mystery is where this water came from, and how such a quantity made to the surface, apparently from underground. The most commonly accepted explanation is that Mars had a watertable, of a mixture of water and carbon dioxid. At the occasion of a tectonic process, the pressure released, inducing a massive boiling of the carbon dioxid and the release of a torrent of mud. Personally I add that some volcanic eruptions may have released huge clouds of steam, carbon dioxyd and dust. But until now nobody can be sure of what happened.
The gravity at high altitude (100 to 300kms) is not much smaller than on the ground. The ability of a planet to retain its atmosphere depends mainly on its gravitation, but also on its temperature and composition, and in a less extent on processes like UV or solar wind (if the later is not shielded by a magnetic field).

About the geological marks originated by a "giant surge". I am not sure about your interpretation since the width of channel is not related to the magnitud of flow surge but also it is related to the time of flow. The other factor might play is the mass density. The denser is the water such as a mud along with stones, erodes the land faster than only water. The case is the very often in the andean zone in the rain time which makes big downpour which drags the land very fast and makes channels to be wider. Are you referring width of the channels from Kaiser or Marines Vallies or other where else.

The other factor about the width erosion land is of its composition. Some loose land such as sand, the water can erode it very easy and fast against on a rock and compact surface. The northern land looks less rocky and mostly of silica sand lands.

Back here about to prove about the "big surge" might be resolved after an laboratory empirical observation on different types of land and measure with liquid force (water or other liquid state such as hydrogen, methane or other which becomes liquid at lower temperature that has happened at billions years when the sun was young with less heat radiation).

Rodolfo
Go to the top of the page
 
+Quote Post
Guest_Richard Trigaux_*
post Mar 17 2006, 07:57 AM
Post #6





Guests






QUOTE (RNeuhaus @ Mar 17 2006, 01:55 AM) *
About the geological marks originated by a "giant surge". I am not sure about your interpretation since the width of channel is not related to the magnitud of flow surge but also it is related to the time of flow. The other factor might play is the mass density. The denser is the water such as a mud along with stones, erodes the land faster than only water. The case is the very often in the andean zone in the rain time which makes big downpour which drags the land very fast and makes channels to be wider. Are you referring width of the channels from Kaiser or Marines Vallies or other where else.

The other factor about the width erosion land is of its composition. Some loose land such as sand, the water can erode it very easy and fast against on a rock and compact surface. The northern land looks less rocky and mostly of silica sand lands.

Back here about to prove about the "big surge" might be resolved after an laboratory empirical observation on different types of land and measure with liquid force (water or other liquid state such as hydrogen, methane or other which becomes liquid at lower temperature that has happened at billions years when the sun was young with less heat radiation).

Rodolfo


Thanks for your contribution. Yes, certain factors like mud, or sandy terrain, could make appear flow marks wider. but I still maintain that such water surges (linking the Nort east part of Tharsis dome, and Vales Marineris, to the northern low lands), were formed by something much more powerfull than our usual rivers. If you look at the Google Mars, these traces are very visible, while M'aadim Vallis (the one which flows into Gusev) is barely visible. However M'aadim vallis is already huge to our standards. At the same scale even our largest rivers would not be visible.

Also the images clearly show a one-time short event. A smaller flow working for a long time can form a large valley, but this valley shows meanders and a narrow bed (Like in France the lower Seine valley), not sand banks the width of the valley. Try to go on a beach, and manage to make some water flow in the sand: if forms water beds which look exactly like the martian formations, but at a much lesser scale. And you notice that these formations are the width of the actual water flow, and that they appear in some seconds, compared to hours with a lesser flow to obtain the same width.


So I still maintain that these formations were created by huge water surges, maybe muddy, or boiling with carbon dioxyd, but not by a continuous small river. This is the mystery.
Go to the top of the page
 
+Quote Post

Posts in this topic
- Magnus Lundstedt   Water oceans on mars?   Mar 14 2006, 11:20 PM
- - ElkGroveDan   QUOTE (Magnus Lundstedt @ Mar 14 2006, 11...   Mar 15 2006, 01:36 AM
|- - RNeuhaus   Very interesting pictures and these give us the id...   Mar 15 2006, 01:56 AM
|- - Magnus Lundstedt   QUOTE (ElkGroveDan @ Mar 15 2006, 02:36 A...   Mar 15 2006, 08:09 AM
|- - helvick   QUOTE (Magnus Lundstedt @ Mar 15 2006, 08...   Mar 15 2006, 08:20 AM
- - Richard Trigaux   Interesting work! But to be noted that, Mars ...   Mar 15 2006, 08:27 AM
|- - Magnus Lundstedt   QUOTE (Richard Trigaux @ Mar 15 2006, 09...   Mar 15 2006, 09:49 AM
- - Richard Trigaux   There are still many things strange and unknown ab...   Mar 15 2006, 11:56 AM
|- - Magnus Lundstedt   Yeah I have seen those. But what I dont understand...   Mar 15 2006, 01:49 PM
|- - Richard Trigaux   QUOTE (Magnus Lundstedt @ Mar 15 2006, 02...   Mar 15 2006, 03:29 PM
|- - Magnus Lundstedt   QUOTE (Richard Trigaux @ Mar 15 2006, 04...   Mar 15 2006, 04:23 PM
|- - RNeuhaus   QUOTE (Richard Trigaux @ Mar 15 2006, 10...   Mar 17 2006, 12:55 AM
|- - Richard Trigaux   QUOTE (RNeuhaus @ Mar 17 2006, 01:55 AM) ...   Mar 17 2006, 07:57 AM
|- - RNeuhaus   QUOTE (Richard Trigaux @ Mar 17 2006, 02...   Mar 17 2006, 09:03 AM
|- - Bob Shaw   QUOTE (Richard Trigaux @ Mar 17 2006, 07...   Mar 17 2006, 09:03 AM
- - David   You can play a similar game over at Viktor Toth...   Mar 15 2006, 01:58 PM
|- - Magnus Lundstedt   QUOTE (David @ Mar 15 2006, 02:58 PM) You...   Mar 15 2006, 02:25 PM
- - tty   QUOTE (Magnus Lundstedt @ Mar 15 2006, 12...   Mar 17 2006, 01:57 PM
- - ljk4-1   The Wikipedia section on Terraforming: http://en....   Mar 17 2006, 04:31 PM


Reply to this topicStart new topic

 



RSS Lo-Fi Version Time is now: 19th April 2024 - 09:53 AM
RULES AND GUIDELINES
Please read the Forum Rules and Guidelines before posting.

IMAGE COPYRIGHT
Images posted on UnmannedSpaceflight.com may be copyrighted. Do not reproduce without permission. Read here for further information on space images and copyright.

OPINIONS AND MODERATION
Opinions expressed on UnmannedSpaceflight.com are those of the individual posters and do not necessarily reflect the opinions of UnmannedSpaceflight.com or The Planetary Society. The all-volunteer UnmannedSpaceflight.com moderation team is wholly independent of The Planetary Society. The Planetary Society has no influence over decisions made by the UnmannedSpaceflight.com moderators.
SUPPORT THE FORUM
Unmannedspaceflight.com is funded by the Planetary Society. Please consider supporting our work and many other projects by donating to the Society or becoming a member.