The European Space Agencys tuesday Express picked up traces of 'spiders' scattered across the South Pole of Mars.
Rather than being true spiders, these small, dark features form when spring sunlight hits layers of carbon dioxide deposited during the dark winter months. Sunlight causes the carbon dioxide ice at the base of the layer to turn into a gas, which then forms and breaks up the layers of ice above. Gas erupts freely in the Martian spring, dragging dark material to the surface as it goes and breaking up layers of ice up to a meter thick.
The escaping gas, rich in dark dust, rises up through cracks in the ice in the form of tall fountains or geysers, and falls back down to settle on the surface. It forms dark spots 45 m to 1 km across. The same process creates 'spider-shaped' patterns etched beneath the snow – so these dark spots are a telltale sign that spiders may be lurking beneath.
Another of ESA's Mars probes, the ExoMars Trace Gas Orbiter (TGO), has captured particularly vivid images of the spiders' tendril-like patterns (see below). The spiders captured by TGO are close to, but outside of, the area shown in this new Mars Express image. The Mars Express view shows black spots on the surface formed by escaping gas and material, while the TGO perspective captures spidery, web-like channels carved into the ice below.
The aforementioned dark spots can be seen throughout the Mars Express image, creeping across high mountains and vast plateaus. However, most can be seen as small dots in the dark area to the left, on the outskirts of a region of Mars nicknamed the Inca City. The reason for the name is no mystery, the linear, almost geometric network of ridges reminiscent of Inca ruins. An Inca city known as Angustus Labyrinth was discovered in 1972. NASAMariner 9 study.
This new view of Inca City and its hidden arachnid inhabitants was captured by Mars Express' high-resolution stereo camera. A version with labels is also available; Click on the image below to explore the region and learn more about the different features you can find here.
A mysterious appearance
We still don't know exactly how the Inca city came to be. Sand dunes may have turned into stone over time. Perhaps magma or sand-like material seeping through broken sheets of Martian rock. Or, the ridges may be 'eskers', twisting structures related to glaciers.
The 'walls' of the Inca city appear to trace part of a great circle 86 km in diameter. Therefore, scientists suspect that the 'city' sits in a large crater formed when a rock from space crashed into the planet's surface. The impact may have caused ripples in the surrounding plains, which were then filled by rising lava and eroded over time.
Towards the middle of the image the landscape changes somewhat, with large circular and oval swirls creating a marble-like effect. This effect is thought to occur as strata deposits erode over time.
In the right-center of the frame are a few prominent steep-sided, flat ridges and hills that rise more than 1500 meters above the surrounding terrain. These form as soft material, eroded over time by wind, water or ice flows, leaving the hard material that forms these mountains.
To the right (north) the land is heavily covered with fine, light-colored dust. A few signs of spiders can be found scattered across the plateaus here, lurking among the various ravines and troughs.
Exploring Mars
Mars Express has revealed a great deal about Mars over the past two decades. The orbiter will image the surface of Mars, map its minerals, study the composition and circulation of its atmosphere, probe beneath its crust, and study the Martian environment.
The spacecraft's HRSC showed us everything Wind-carved ridges and troughs Sinkholes in the flanks of giant volcanoes impact craters, tectonic faults, river channels, and ancient lava pools. This mission has yielded immense results over its lifetime, creating a more complete and accurate understanding of our planetary neighbors than ever before.