- There is snow since this is a
              winter.
              It may be true colors, 
              but it looks a little overly grey.
              
              The view is oblique and to the west.
              
           
 - The Manicouagan crater
               is in Quebec,
               Canada, ∼ 200 km north of
               Baie-Comeau,
               Quebec---i.e., the middle of nowhere.
               
               The area of the Manicouagan crater
               is rugged and heavily timbered and is in the
               Canadian Shield.
               
           
 - The Manicouagan crater
               is multi-ring crater
               of ∼ 100 km in diameter.
               
               The visible part 
               is ∼ 72 km in diameter
               (see Wikipedia:
               Manicouagan Reservoir:  Manicouagan impact crater). 
               
 
               The Manicouagan crater is the 6th largest
               confirmed impact crater
               on Earth.
               
 
          
 - The Manicouagan crater is one of the
          more obvious Earth
          impact crater.
          For most impact craters, you'd need
          some authority to tell you they were there.
              
           
 - The annular lake seen in the image is
               Manicouagan Reservoir
               which has a diameter.
               of ∼ 70 km and may be a depression between two rings of
               the multi-ring crater,
               but Wikipedia is NOT saying.
               
               The island
               formed by 
               Manicouagan Reservoir
               is Rene-Levasseur Island.
               
               Manicouagan Reservoir
               is drained at the south end by 
               Manicouagan River
               which flows south ∼ 200 km and empties into the 
               Saint Lawrence River
               not far from it becomes the  
               Gulf of Saint Lawrence.
               
           
 - The crater is 214(1) Myr old
               (thus formed in the 
               Triassic (252.2(5)--201.3(2) Myr BP).
               
               The impactor is believed to
               be an asteroid
               of ∼ 5 km in size scale.
               
 
           
 - Mount Babel
               (peak 952 m above sea level)
               is believed to be the
               central peak
               of the crater
               which is also then a 
               central-peak crater.
               
           
 - The crater
               has been heavily eroded particularly by 
               glaciers
               during the 
               Quaternary glaciation (AKA the current ice age).
               
          
 
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