The researchers examined Macrobi and the boss in the middle latitudes using Faustini’s craters, a noise and a haurt near the poles of the moon, as well as photography analysis and data of Lola Laser Altimeter.
Previously, crater noise studies showed the presence of ice -shaped water. New data confirm that the low temperatures of Perpolar craters contribute to the accumulation of volatile substances, especially water.
In craters examined, hundreds of meters in diameter shock formations reign. In close -plane craters, flat soles and small craters with “lobed” shafts are observed, which may indicate the presence of ice.
Source: Ferra
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