You have that point, Sputnik!
A tad small, but let it go.
Sputnick wrote:
And what has kept the steam from expanding before it reaches the surface.
Answer: Pressure within Phobos - pressure of rock and ice.
How has the rock & ice exerted that pressure? The gravity on the surface of Phobos varies due to its irregular shape, but is never more than 0.09g. So there is very little weight, presing the surfeca down on the core.
Sputnick wrote:
Answer: Tidal gravity could be immense, creating eough pressure to heat both ice and rock to liquid at high temperatures - or a least ice to superheated steam. Of Mintoes fountains I have no knowledge.
Not so. The gravity well of a primary tends to pull a satellite apart, not squeeze it together. A moon big enough to be held togther by its own gravity will be stressed by the tide, this is one theory for the presence of
liquid water on Enceladus. But a gas giants gravity is needed, esl;e the Moon would have active volcanos.
.
Sputnick wrote:Answer: Not much pressure is needed to blast out a large crater in volcanic ash .. the surfae of Phobos appears to consist of loosely pack, perhaps granular material.
Who knows, I don't!
See above, but I chose those as being the most powerful on Earth, and they have no craters.
However, some of the biggest explosions on earth have involved water and lava. Mt.St.Helens, the volcanic eruption that silenced Waimangu Geyser, maybe Krakatoa. But those require a lot of lava and a lot of water, plentiful on Earth. Pretty scarce on Phobos now.
Answer: In one of these posts I read Phobos is half ice and half rock. Not much temperature change is needed to change ice to water.
Cite it!
If it was a thrown off piece of Mars, complete with sedimentary rock that included lots of water - it's sedimentary! Where does the lava, or at least heat come from?
Answer: Tidal gravity forcing the layers together.
See above, tides work to pull aprt, not push together.
And if it was sedimentary, I would expect the lines of eruption of warmed water to follow the strata. How in Geology do strata cross over, as you have pointed out?
Answer: I have lived and travelled often in our Canadian Shield. I have seen strata crisscross, and I have seen U shaped strata. Rock is very flexible. A short length of steel seems inflexible - however, I have helped lay 1/4 mile lengths of railroad track weighing 120 lbs. per foot (or was that 160 lbs? I think 160 lbs., but it was 25 years ago)and know they are more like a rubber band, relatively, which their names reflect, "Ribbon Rail".
Bent strata, sure! But crossed over strata?? Evidence, please.
Answer: Erosion by wind or water WHEN Phobos was part of a planet - I don't think Phobs is from Mars. The soft layers would erode in gullies, grooves.
When it was part of a planet. All over a 28km ball. On a planet. Hmmmmmm.
Well, different eyes see different things. As I follow any 'groove' I see wavy sides, as if the groove is a concatentation of a series of craters. As the groove gets fainter that wavyness diminishes until the groove appears smooth sided. Which I take to be the limit of resolution, not a sudden change to a different mechanism of formation.
Answer: If you examine the photos I referenced you would see two steam created craters in soft material, with a groove between the two craters .. the groove and craters together making a longer groove, exactly as on Phobs, with wavy lines.
Perhaps Phobos was once part of a planet which had atmosphere .. windblown sand could scour the layers like wind raising waves on ocean or lake .. or, I have seen 'waves' of sand created in shallow waters by the waves of the water (Canada's Great Lake Huron's famous shallow beaches being prime examples).
If you can show us a formation like Phobos ona lake floor, fine.
Answer: Visit Pinery Provincial Park on Lake Huron and see it in miniature .. but without craters. A trip to the Canadian Shield would be a real education as to rock formation.
I have emailed my friend Don, a Professor Emeritus in Geology who has an avid desire to stand on Mars for scientific and personal purposes, and requested his opinion of the photos of Phobos.
I'll look forward to that.
John
[quote="Sputnick"]An excellent example of volcanic steam vent craters on earth. http://debris.com/galleries/main.php?g2_itemId=626
These two craters creating a groove. [/quote]
You have that point, Sputnik!
A tad small, but let it go.
[quote="Sputnick"]
And what has kept the steam from expanding before it reaches the surface.
Answer: Pressure within Phobos - pressure of rock and ice.[/quote]
How has the rock & ice exerted that pressure? The gravity on the surface of Phobos varies due to its irregular shape, but is never more than 0.09g. So there is very little weight, presing the surfeca down on the core.
[quote="Sputnick"]
Answer: Tidal gravity could be immense, creating eough pressure to heat both ice and rock to liquid at high temperatures - or a least ice to superheated steam. Of Mintoes fountains I have no knowledge.[/quote]
Not so. The gravity well of a primary tends to pull a satellite apart, not squeeze it together. A moon big enough to be held togther by its own gravity will be stressed by the tide, this is one theory for the presence of
liquid water on Enceladus. But a gas giants gravity is needed, esl;e the Moon would have active volcanos.
.[quote="Sputnick"]Answer: Not much pressure is needed to blast out a large crater in volcanic ash .. the surfae of Phobos appears to consist of loosely pack, perhaps granular material.[/quote]
Who knows, I don't!
[quote]Have a look at the Old Faithful GeyserCam at: http://www.nps.gov/archive/yell/OldFaithfulcam.htm
Or at Steamboat Geyser, the highest in the world at present:
http://pages.cs.wisc.edu/~boris/photo/trip_to_the_west/ys_ng09.html
No craters!
Answer: Did you examine the two examples I provided?.[/quote]
See above, but I chose those as being the most powerful on Earth, and they have no craters.
However, some of the biggest explosions on earth have involved water and lava. Mt.St.Helens, the volcanic eruption that silenced Waimangu Geyser, maybe Krakatoa. But those require a lot of lava and a lot of water, plentiful on Earth. Pretty scarce on Phobos now.
Answer: In one of these posts I read Phobos is half ice and half rock. Not much temperature change is needed to change ice to water.
Cite it!
If it was a thrown off piece of Mars, complete with sedimentary rock that included lots of water - it's sedimentary! Where does the lava, or at least heat come from?
Answer: Tidal gravity forcing the layers together.
See above, tides work to pull aprt, not push together.
And if it was sedimentary, I would expect the lines of eruption of warmed water to follow the strata. How in Geology do strata cross over, as you have pointed out?
Answer: I have lived and travelled often in our Canadian Shield. I have seen strata crisscross, and I have seen U shaped strata. Rock is very flexible. A short length of steel seems inflexible - however, I have helped lay 1/4 mile lengths of railroad track weighing 120 lbs. per foot (or was that 160 lbs? I think 160 lbs., but it was 25 years ago)and know they are more like a rubber band, relatively, which their names reflect, "Ribbon Rail".
Bent strata, sure! But crossed over strata?? Evidence, please.
Answer: Erosion by wind or water WHEN Phobos was part of a planet - I don't think Phobs is from Mars. The soft layers would erode in gullies, grooves.
When it was part of a planet. All over a 28km ball. On a planet. Hmmmmmm.
Well, different eyes see different things. As I follow any 'groove' I see wavy sides, as if the groove is a concatentation of a series of craters. As the groove gets fainter that wavyness diminishes until the groove appears smooth sided. Which I take to be the limit of resolution, not a sudden change to a different mechanism of formation.
Answer: If you examine the photos I referenced you would see two steam created craters in soft material, with a groove between the two craters .. the groove and craters together making a longer groove, exactly as on Phobs, with wavy lines.
[quote]Perhaps Phobos was once part of a planet which had atmosphere .. windblown sand could scour the layers like wind raising waves on ocean or lake .. or, I have seen 'waves' of sand created in shallow waters by the waves of the water (Canada's Great Lake Huron's famous shallow beaches being prime examples).[/quote]
If you can show us a formation like Phobos ona lake floor, fine.
Answer: Visit Pinery Provincial Park on Lake Huron and see it in miniature .. but without craters. A trip to the Canadian Shield would be a real education as to rock formation.
I have emailed my friend Don, a Professor Emeritus in Geology who has an avid desire to stand on Mars for scientific and personal purposes, and requested his opinion of the photos of Phobos.
I'll look forward to that.
John