Surface features on Ceres – and its interior evolution have a closer relationship than one might think. A recent study analyzed Ceres’ surface features to reveal clues about the dwarf planet’s interior evolution. Specifically, the study explored linear features — the chains of pits and small, secondary craters common on Ceres.
The findings align with the idea that, hundreds of millions (up to a billion) years ago, materials beneath Ceres’ surface pushed upward toward the exterior, creating fractures in the crust.
“As this material moved upward from underneath Ceres’ surface, portions of Ceres’ outer layer were pulled apart, forming the fractures,” said JenniferScully, lead study author and associate of the Dawn science team at NASA’s Jet Propulsion Laboratory in Pasadena, California.
The indication of upwelling material under Ceres’ surface allows for another perspective in establishing how the dwarf planet may have evolved.
Dawn scientists generated a map of over 2,000 linear features on Ceres greater than 0.6 mile (one kilometer) in length that are located outside of impact craters. The scientists interpreted Dawn’s observations of two kinds of linear features to further understand their connection to the upwelling material. Secondary crater chains, the most common of the linear features, are long strings of circular depressions created by fragments thrown out of large impact craters as they formed on Ceres. Pit chains, on the other hand, are surface expressions of subsurface fractures.
Among the two features, only pit chains provide insight into Ceres’ interior evolution. Scully said the study’s greatest challenge was differentiating between secondary crater chains and pit chains. Although the features are strikingly similar, researchers were able to distinguish between them based on their detailed shapes. For example, secondary craters are comparatively rounder than pit chains, which are more irregular. In addition, pit chains lack raised rims, whereas there is usually a rim around secondary craters.
While it is possible that the freezing of a global subsurface ocean formed the fractures, this scenario is unlikely, as the locations of pit chains are not evenly dispersed across Ceres’ surface. It is also unlikely that the fractures formed by stresses from a large impact because there is no evidence on Ceres of impacts substantial enough to generate fractures of that scale. The most probable explanation, according to the Dawn scientists, is that a region of upwelling material formed the pit chains. The material may have flowed upward from Ceres’ interior because it is less dense than surrounding materials.
Dawn scientists look forward to seeing how these characteristics will help other researchers model Ceres’ interior evolution, which can test whether upwelling may have occurred near the fractures.
The Dawn mission is managed by JPL for NASA’s Science Mission Directorate in Washington. Dawn is a project of the directorate’s Discovery Program, managed by NASA’s Marshall Space Flight Center in Huntsville, Alabama. UCLA is responsible for overall Dawn mission science.
The NASA image at the top of the page shows Occator Crater, one of the more than 130 bright areas, and most of them are associated with impact craters. The global nature of Ceres’ bright spots suggests that this world has a subsurface layer that contains briny water-ice.
The Daily Galaxy via Dawn/JPL
via The Daily Galaxy