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Permafrost layer in Kaktovik, North Slope Borough, Alaska   

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Permafrost layer in Kaktovik, North Slope Borough, Alaska
Photographer: Gerald and Buff Corsi
Collection: CalAcademy

ID: 6666 6666 0814 0016 (2014-08-05)

Copyright © 2014 California Academy of Sciences

 
INFORMATION PROVIDED WITH THE PHOTO
  • date of photo  Oct 1, 2012
  • location   Kaktovik (Alaska, US)
  • notes   In geology, permafrost or cryotic soil is soil at or below the freezing point of water 0 °C (32 °F) for two or more years. Most permafrost is located in high latitudes. Overlying permafrost is a thin active layer that seasonally thaws during the summer. Plant life can be supported only within the active layer since growth can occur only in soil that is fully thawed for some part of the year. Kaktovik in North Slope Borough, Alaska,
  • CalAcademy slide #   Permafrost layer 121001 _D803585
  • photo category: Landscape - habitat
  • original filename: Permafrost layer 121001 _D803585.jpg
  •  
    Using this photo   The thumbnail photo (128x192 pixels) on this page may be freely used for personal or academic purposes without prior permission under the Fair Use provisions of US copyright law as long as the image is clearly credited with Gerald and Buff Corsi © California Academy of Sciences.

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