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#40 This cropped photo is borrowed from the above JP2 PSP large file photo and placed in this section to illustrate further that what many scientists call "sand dunes" are NOT made of sand. This photo was cropped from the West side of the original JP2 photo at the above approximate PSP map coordinates using the IASViewer and is outside of the crater.
As you should be able to see, there are several "sand dune critters" who have died and their bones are bleaching out in the open. Their "flesh" may also have been eaten by insects and/or spiders. These "sand dune critters" evidently bury themselves under the sand and then emerge with sand sticking to their bodies in order to move about. These are most likely consumers and digesters of sand just as Terran earthworms on Earth consume dirt and digest it. Therefore, this species on Mars may be just as valuable for their ability to produce essential elements back to the soil.
I think, at this time, that it is most appropriate to rename these critters as "Sand Dune Worms" as that is what I believe them to be.
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This letter is from the following scientists and the complete letter (announcement) may be found at this URL: ftp://ftp.hq.nasa.gov/pub/pao/pressrel/2000/00-082.txt
At the bottom of this page, I have printed in red the part of this letter which describes the strangeness of the "Sand Dune Worms", although at the time, they were not aware of giant worms on Mars(and, in January 2008, many scientists still won't admit that these creatures exist on Mars). But it IS admitted that they cannot be dunes because of the sharpness of the crests or ridges, the symmetry of the slopes, and what they call erosion is what we now know are the hundreds or thousands of "legs" that provide mobility to these worms. Throughout most, if not all of the photos on my webpages, these sand dune worms are present.
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Donald Savage
Headquarters, Washington, DC May 22, 2000
(Phone: 202/358-1727)
Mary Hardin
Jet Propulsion Laboratory, Pasadena, CA
(Phone: 818/354-0344)
Dr. Ken Edgett
Malin Space Science Systems, San Diego, CA
(Phone: 858/552-2650 x500)
RELEASE: 00-82
PUBLIC INVITED TO BROWSE 20,000 NEW ADDITIONS TO MARS PHOTO GALLERY
The letter says, in part:
"Putting these data into perspective is very difficult. We have focused on 'themes.' Layers on the Martian surface are the biggest 'theme' or 'finding' of the imaging investigation so far. To a geologist, layers record history and they are the most geologically important, profound thing we have seen," said Dr. Michael Malin, principal investigator for the camera system at Malin Space Science Systems. "We see layers in the walls of canyons, craters, and troughs. We see layers in both the north and south polar regions. We see them in the craters on top of volcanoes, we see them in pits at the bottoms of impact craters, we see them virtually everywhere that some process has exposed the subsurface so that we can see it from above."
"Seeing Mars up close through the narrow angle camera has been a humbling
experience. We often find surfaces for which there are no obvious analogs on Earth, like certain ridges that look like dunes. Our terrestrial geologic experience seems, at times, to fail us," Edgett said. "Perhaps it is because water is the dominant force of erosion on Earth, even in the driest desert regions.
But on Mars that force of change may have been something else, like wind. The ridges seen in places like the Valles Marineris floors are strange. They aren't dunes because they occur too close together, their crests are too sharp, their slopes too symmetrical. They often appear to be a specific layer of material that has undergone erosion -- we just wish we knew what processes are involved that cause this kind of erosion."
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