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Catherine
Weitz and her colleagues from the Institute of Planetology (USA) have
discovered yet another proof that there could have been life on Mars at
some point. This conclusion was made based on the information obtained
by interplanetary station NASA Mars Reconnaissance Orbiter. The
researchers are talking about two depressions 30-40 km long, located in
the region of Noctis Labyrinthus ("the labyrinth of the night").
These depressions contain a type of clay
called smectites, which contains a blend of silica with aluminum, iron
or magnesium. This is a group of hydrous silicates formed by weathering
of mainly alumina-silicates and silicates of igneous and metamorphic
rocks on the soil surface. These rocks are formed in the water with
neutral acidity.
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