Liquid chemicals case analysis

Views from the Viking Orbiters: Because the atmosphere is so thin, the greenhouse effect is insignificant and Mars has rapid cooling between night and day. The large temperature differences create strong winds.

Liquid chemicals case analysis

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Views from the Viking Orbiters: Because the atmosphere is so thin, the greenhouse effect is insignificant and Mars has rapid cooling between night and day.

The large temperature differences create strong winds. The strong winds whip up dust and within a few weeks time, they can make dust storms that cover the entire planet for a few months.

Two "before-after" image sets are shown below. The first pair is from the Mars Global Surveyor of the Tharsis bulge side of the planet.

Liquid chemicals case analysis

The "before-after" images are about 1. The "before-after" images are about 2. Liquid Water Color view of river drainage system from Viking orbiter on left and black-and-white zoom-in of Nanedi Vallis canyon using Viking wide-field view and Mars Global Surveyor magnified view images on right.

In Eberswalde Crater is a "fossil delta" that shows that Mars experienced ongoing, persistent flow of water over an extended period of time. It also shows that some sedimentary rocks on Mars were deposited in a water environment. Select the image to find out more details leading to these deductions.

Fossil delta in Jezero Crater. Color-enhancing shows the clay-like minerals green here that were carried into the lake, forming the delta. The clays would be Liquid chemicals case analysis good place to look for signs of ancient life. What makes Mars so intriguing is that there is evidence for sustained running liquid water in its past.

Some geologic features look very much like the river drainage systems on Earth and other features points to huge floods.

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The Mars Pathfinder studied martian rocks in the summer of and found some rocks are conglomerates rocks made of pebbles cemented together in sand that require flowing water to form. Abundant sand also points to widespread water long ago. More recently, the larger and more advanced Mars Exploration Rovers one called "Spirit" and the other called "Opportunity" have further strengthened the conclusion that there was liquid water on Mars in the past.

Highly magnified images of the rocks examined by Opportunity see image below show a particular type of rippling patterns on the rocks that are formed under a gentle current of water instead of wind.

In the image below the green stripes show the sedimentary layers laid down in flowing water and the blue lines show the boundaries between the layers. Furthermore, detailed chemical analysis of the compositions of the rocks by Opportunity show that they formed in mineral-rich water when the water got very concentrated with the minerals as the water evaporated spectrum 1spectrum 2spectrum 3spectrum 4spectrum 5spectrum 6 links.

More recently, Opportunity found veins of the mineral gypsum near the edge of the large crater Endeavour. The gypsum veins show that water flowed through the rocks and they are even stronger evidence for water than mentioned above.

Liquid chemicals case analysis

It has a suite of instruments for identifying organic compounds such as proteins, amino acids, and other acids and bases that attach themselves to carbon backbones and are essential to life as we know it.

It is also able to detect gases that could be the result of biological activity but it does not the instruments to determine if there is currently existing biological activity going on. It will identify the best possible sites of biological activity past or present for a follow-up mission to more definitely confirm.

Gale Crater is kilometers 96 miles across with a large mountain Mount Sharp inside it that appears to be the remnant of an extensive series of deposits. The layers at the base of the mountain contain clays and sulfates that very likely formed in liquid water. Curiosity will also investigate: The image above shows sections of the first deg color pan of Gale Crater where Curiosity landed.

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The image was brightened during processing. The crater wall is visible on the left and right sides of the image and Mount Sharp is near the center of the image with the dark dunes near its base containing clays and sulfates that very likely formed in liquid water probably 3.

Parts of the rover are visible as well. The black areas are places where the images making up the pan had not been all beamed to Earth yet. At locations near where Curiosity landed in Gale Crater, it found deposits of gravel made of well-rounded pebbles eroded off of sedimentary conglomerate outcrops left image.

On Earth right image of sedimentary conglomeraterocks that are well-rounded are a common sign of rocks that have been transported by water in a river or stream. If the flow of water is great enough, the pebbles are lifted up in the flow or rolled along the bed and they get pounded against each other so the edges get rounded off.

The sizes of the pebbles on Mars are too large to have been transported by wind; they must have been transported by a sustained, vigorous flow of water.E-liquid is the mixture used in electronic cigarettes.

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