FDL Frozen Debris Lobes

FDL Frozen Debris Lobes are slow-moving landslides occurring in permafrost made up of soil, rocks, trees, and ice. Many are located on the slopes in the southern Brooks Range of Alaska.

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This website fdlalaska.org was first submitted to the registrar on October 15, 2013. It is currently five hundred and fifty weeks, fifteen days, two hours, and one minute young.
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University of Alaska

University of Alaska

PO Box 755320

Fairbanks, AK, 99775-5320

US

Shawn Armstrong

PO Box 755320

Fairbanks, AK, 99775-5320

US

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PAGE TITLE

FDL Frozen Debris Lobes

DESCRIPTION

FDL Frozen Debris Lobes are slow-moving landslides occurring in permafrost made up of soil, rocks, trees, and ice. Many are located on the slopes in the southern Brooks Range of Alaska.

CONTENT

This website had the following in the site, "Looming over Alaskas most economically important highway." We viewed that the web site stated " What are Frozen Debris Lobes? Frozen debris lobes or FDLs are slow-moving landslides occurring in permafrost." It also said " Made up of soil, rocks, trees, and ice, many are located on the slopes in the southern Brooks Range of Alaska. Why do we care about FDLs? FDL-A is approaching the Dalton Highway at an increasing rate. Distance to Dalton Highway on August 13, 2017 29. Todays distance to Dalton Highway." The header had Frozen Debris Lobes as the highest ranking search term. It is followed by FDL, permafrost, and Brooks Range which isn't as ranked as highly as Frozen Debris Lobes. The next words they uses is Alaska. soil was included and could not be understood by web engines.

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