This truly interesting Contextual Image (or "CTX Frame", for short) of the Dwarf Planet 1-Ceres, taken by the NASA - Dawn Spacecraft on December, 21, 2015, shows us the Floor of Dantu Crater, which reveals Surface Structures hinting (---> suggesting) at the occurrence of Tectonic Processes that, in a very remote past, formed and defined the Dwarf Planet's Surface. As you can see, some sort of semi-Linear Surface Structures (---> in fact, they are small and relatively shallow and intricated cracks) are spread almost all over the Crater's Floor while, on the other hand, outside the Crater's Rim (of course not visible here), the presence of these Linear and semi-Linear Structures continues in the form of Scarps (---> Linear and semi-Linear, Cliff-like Slopes) and Ridges. However, similar Fractures are seen in Tycho, one of the youngest large Impact Craters on Earth's Moon. This cracking may have resulted from the cooling of Impact Melt, or when the Crater's Floor was uplifted after the Crater formed. Probably it is useless to say it (but we wnat to underline it anyway), a relatively large and irregularly-shaped White Spot is clearly visible at about 2 o'clock of the frame, on its right (Dx) side, near a truly small Crater Cluster. Dantu Crater's diameter is roughly 78 miles (such as about 125,528 Km). Just as usual for 1-Ceres, a number of White Spots (some truly well defined and clear) can be easily seen inside, on the steep Inner and Outer Rim, and also outside Dantu Crater. The original photo was taken during its Low-Altitude Mapping Orbit (or "LAMO", for short) and from an altitude of approx. 240 miles (such as about 386,2416 Km) from the Surface, with a resolution of roughly 120 feet (such as about 36,576 meters) per pixel. This image (which is an Original NASA - Dawn Spacecraft's b/w and NON Map-Projected frame published on the NASA - Planetary Photojournal with the ID n. PIA 20193) |