Another permanently shadowed crater on the Moon shows no obvious ice

Note that the bright areas are not ice but simply overexposed
The science team operating the Shadowcam camera on South Korea’s Danuri lunar orbiter — designed to take images in places with little light — yesterday released a new image taken of the floor of a permanently shadowed crater on the Moon, Hermes-A, located near the north pole.
That picture is to the right. The rectangle indicates the area discussed by the release, focusing entirely on describing its geological features, such as impact melt and the numerous secondary smaller impacts and ejecta within the crater floor. The inset gives the context, showing the crater’s location near the north pole. The blue areas in the inset are those areas thought to be permanently shadowed, such as the entire floor of Hermes-A.
What the release fails to mention is the most important detail lacking in this picture. Though the floor of Hermes-A crater is considered permanently shadowed, the low light image taken by Shadowcam shows no obvious ice features, at all. If there is a higher content of water here, it is locked within the soil, and would require processing to access. Even so, the picture suggests that any such moisture is of extremely low concentration, likely in the parts per billion, and hardly enough to build a lunar base.
This is the same result found by previous Shadowcam pictures. Increasingly it appears that the hope of finding large quantities of easily accessible water ice in these permanently shadowed craters is proving false.
Note that the bright areas are not ice but simply overexposed
The science team operating the Shadowcam camera on South Korea’s Danuri lunar orbiter — designed to take images in places with little light — yesterday released a new image taken of the floor of a permanently shadowed crater on the Moon, Hermes-A, located near the north pole.
That picture is to the right. The rectangle indicates the area discussed by the release, focusing entirely on describing its geological features, such as impact melt and the numerous secondary smaller impacts and ejecta within the crater floor. The inset gives the context, showing the crater’s location near the north pole. The blue areas in the inset are those areas thought to be permanently shadowed, such as the entire floor of Hermes-A.
What the release fails to mention is the most important detail lacking in this picture. Though the floor of Hermes-A crater is considered permanently shadowed, the low light image taken by Shadowcam shows no obvious ice features, at all. If there is a higher content of water here, it is locked within the soil, and would require processing to access. Even so, the picture suggests that any such moisture is of extremely low concentration, likely in the parts per billion, and hardly enough to build a lunar base.
This is the same result found by previous Shadowcam pictures. Increasingly it appears that the hope of finding large quantities of easily accessible water ice in these permanently shadowed craters is proving false.