Tubes on Mars

Page 9


A Few More Things

Cephalopods at the Smithsonian Museum of Natural History in Washington DC


The caption reads:
Cirroceras nebrascense
Late Cretaceous (76-68 million years ago) South Dakota
Larger Closer

Could the "tubes" on Mars be the remains of
a life form like the cephalopods?


Here is another interesting thing to look at.

This rock also resides at the Smithsonian Museum of Natural History.

The caption reads:
Sandstone
Shows leisegang weathering
Durbach,Germany
"Water carrying dissolved iron along two perpendicular
sets of cracks percolated into this rock, forming iron
oxide minerals that cemented the grains. These
cemented areas resist weathering."

There are some "tube" image enhancements out here on the

web that can compare to this natural formation.
The Cydonia Imperative
Please visit this interesting web site.

This
does not mean that the image at The Cydonia Imperative is of liesegang weathering, or that that method of enhancement discovered a type of liesegang weathering formation. Although it might have discovered such a thing. It means that the enhancement resembles some kind of weathering process that could have happened on Mars. It could have happened in that polygonal terrain, in those fissures and/or canyons; the harder material remained in a rib-like pattern, and the softer, more easily eroded stuff washed away during a season of thaw.


In black and white
Closer
It might look more Martian - more MGS/MOC-ish - in black and white.


This
rock has an archeological look to it - as if made by intelligent design. It looks like part of an ancient wall, with patterns carved into blocks of limestone or sandstone. But it is not.
Cementation
is an important part of how loose materials become rock. The three most common cements are silica, carbonates, and iron oxide. Calcium carbonate is probably the most familiar cementing agent. We use forms of it in our everyday building materials. As we can see from the geology of caves, calcite minerals have a very active, dynamic cycle of precipitation and dissolution. Silica cement is very hard and forms at great depths. Iron oxide cement comes from weathered iron-rich rocks. Water containing the minerals in solution percolates through the vacant spaces in the sediment. Eventually the material precipitates out of the water and acts as an adhesive, connecting all the particles together.
Weathering
is a principle factor in how rocks change form and chemical structure. No doubt, all manner of shapes and forms can result from the cementing of soft sediment, especially if other geologic forces also act upon it.
I
gather, from the information provided by the Smithsonian Institute, iron-rich water entered the cracks and pore spaces of an existing rock. The iron precipitated out of solution, further hardening the area and altering the structure there. Over time, the less hard, non-iron and possibly calcite rich portions, of the rock eroded, forming the liesegang patterns.


Yes, all manner of shape and form.

This beautiful creation is also at the Smithsonian Museum of Natural History.
Title:
Sand Grains Cememted with a Twist
The Smithsonian write-up: "Water and wind deposited quartz sand along an ocean beach about 35 million years ago, and other sediment buried the sand. Later, the overlying rock was eroded and the sand exposed. Withn the past 400,000 years, circulating groundwater dissolved quartz from some areas of the exposed sand and redeposited it in others. There the quartz cemented loose sand grains into sinuous shapes."

Closeup


I
have gone from geology to giant life forms and back to geology again. Time and time again our own planet has sculpted and remade itself. Over great expanses of time various creatures have dominated the seas and land. Some of these were very large. If flesh and blood life ever existed on Mars, it is possible that it experienced and age of dinosaurs similar to that on Earth. However, life on Mars would have developed according to the Martian environment. Mars may not have been able to support creatures like Tyrannosaurus Rex, but it may have been able to sustain very large worms or crinoid-like animals. We are only beginning to discover and understand what exists far below the surface of Earth and what thrives in our own deepest oceans - environments of unbearable temperatures, lethal pressures and poison atmospheres, strange and completely alien to ourselves.
If
science accepts the possibility of microscopic life on Mars, it should be at least open to the possibility that higher/larger forms of life could exist there. One has to examine all the possibilities. Geology offers many answers. Still this is all speculation - what if scenarios. It is not easy to come to a final conclusion when no one has directly experienced the geology (and paleontology) of Mars. For now, when pondering the mysteries of Mars, imagination mixed with the knowledge of how our own planet works is one of the most powerful tools we have.


And now