In addition, researchers assumed that
the ancient equatorial regions were too hot for vertebrates to live during the Early Triassic.
Not exact matches
The map also provides a global view of the highs and lows of Titan's topography, which enabled the scientists to confirm that two locations in the
equatorial region of Titan are in fact depressions that could be either
ancient, dried seas or cryovolcanic flows.
The north - south variation in minerals indicates that the deep crust exposed in the southern Rheasilvia
region is dominated by pyroxene - rich, diogenitic material while the
equatorial region seems to retain the most
ancient eucrite - rich mineralogy.