Dwarf Planet Ceres: Evidence of Active Cryovolcanism

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These mosaics of Occator Crater are composed of several images taken by Dawn&rsq
These mosaics of Occator Crater are composed of several images taken by Dawn’s Framing Camera from a distance of 35 kilometers. Within the crater, which has a diameter of 92 kilometers (A), there are two areas of bright deposits. The deposits in the center of the crater, called Cerealia Facula (B), measure only a few kilometers in diameter. In its center a dome bulges upwards. The deposits in the northeast of the crater are called Vinalia Faculae (C). © A. Nathues et al., Nature Astronomy
These mosaics of Occator Crater are composed of several images taken by Dawn's Framing Camera from a distance of 35 kilometers. Within the crater, which has a diameter of 92 kilometers (A) , there are two areas of bright deposits. The deposits in the center of the crater, called Cerealia Facula (B) , measure only a few kilometers in diameter. In its center a dome bulges upwards. The deposits in the northeast of the crater are called Vinalia Faculae (C) . A. Nathues et al. Nature Astronomy Until a million years ago, dwarf planet Ceres, the largest body in the asteroid belt, was the scene of cryovolcanic eruptions: below the Occator Crater, subsurface brine pushed upward; the water evaporated, leaving behind bright, salty deposits.
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