An image acquired by Terra on the morning of 8 November shows branching white streaks in valleys of the Appalachian Plateau and along the Cumberland River. In its account published on 10 November, NASA Earth Observatory explains that these low clouds appear to be fog. They are no longer visible in afternoon images from the same day. [1]

The phenomenon helps reveal the landscape: during long autumn nights, the ground loses heat and cools nearby air. When the dew point is reached, water vapour can condense into tiny droplets. Colder air tends to flow downhill and collect in valleys, while waterways supply moisture. This explains the process; it is not a direct measurement of every valley pictured. [1][2]