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This
was found to be in error- correction is here
The artifact in question turns out to be the
edge of the rover solar panel out of focus in the image. The
markings are either corrosion or frost on the edge. The image
is here
at the NASA/JPL website.
Being solely responsible for the contents of this
page, I have decided to keep the error clearly marked and in place
so that other will not make the same mistakes.
| As you can see from the inset, the upper, red
outlined image is the original image that appeared to contain
water. The lower image shows the edge of the rover solar
panel with the pattern of what appears to be frost on it.
I have overlaid the two so you can see that the exact
pattern of markings matches on both. |
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(previous contents, unchanged)
One
of the goals of Mars research is to find water on the planet.
While checking some of the older images for geysers and water flow
features, I found an image of a brine pool located in Eagle Crater
early in the mission. The reason this has not been spotted
before is that the image shows just one corner of the pool, and
without assembling it in relatively accurate color, the significance
of the image would be easy to miss.
I will present the before and after images first, then explain
how I located them.
| This is the "before" image, showing a
puddle of brine in the lower left corner of the image.
It was made at 12:01:24 Mars local time. The original
image is here
at the NASA/JPL web site. The image was taken with
the L7 (left panoramic violet) filter. |
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| Now we can see the "after" image which
was taken at 12:02:48 Mars local time. The original
image is here
at the NASA/JPL web site. The image was taken with
the R1 (right panoramic violet) filter. Look at the
lower left corner and you can see the difference- the puddle
is now missing. Spherules are in its place. |
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The left image shows the puddle, clearly visible to the lower
left. The right image of the exact same spot, just over a
minute later, shows no puddle. This change occurred in a space
of one minute, twenty four seconds.
Note that I have kept the color saturation high in the following images
to help make the features more clearly visible. True color
images would be much darker with soil about chocolate brown and the
rock slabs not much lighter. The fossil spherules in that case
would be more gray than blue.
| While looking at the stone slabs and the geyser
vents around them, I located the pool of brine. Here is
a thumbnail of a false color image constructed from L2 and L7
data. I used these filters because they closely
correspond to the R2 and R1 respectively, and allow an
excellent full color 3D image to be assembled.
Click the image for a full-sized view. The original
data is here
at the NASA/JPL web site. |
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| I spotted two geysers in the above image and
constructed stereo views of them. Three features in the
image stood out at once. First, the lower center geyser
itself was apparent. Click here
for a color stereo image of it. Second, the upper right
geyser was smaller but clear. Click
here for a color stereo view of it. But finally, the
undercut edge or lip showing at the lower left of the
image showed what appeared to be water erosion.
I decided to try tracking the source of the water and
examined all the lip features in the panoramic images for Sol
050. This image showed the best detail. Click it
for a larger view. It was taken at 11:56 Mars local
time, just before noon. The original image data is here
at the NASA/JPL web site. |
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| In the lower left corner, we can see an odd
looking area. Here is a closer look at it. We see
a darker outline on the rock where it is wet, and just below
it, we see a brine pool. How can we tell? Because
as the water is evaporating, the salts are concentrating and
we can see the patches on the surface. They appear bluish
in this color exaggerated image.
Note the soft, rounded contours to the patches and the dark
level surface of the brine. It looks completely
different from the muddy soil at the lower right.
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Now let's look at the detail at a higher magnification. This
image shows concentrated salt water, or brine, that resulted from
the eruption of a small geyser, and the solution of salts in the
soil. This water will dry rapidly and leave little more than
darkened soil and a higher concentration of salts behind.
However, this proves that liquid water is in fact present on the
surface of Mars today.

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