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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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FDL: Frozen Debris Lobes | fdlalaska.org Reviews
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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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2 FDL
3 permafrost
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5 Alaska
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7 rocks
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9 ice
10 landslides
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FDL: Frozen Debris Lobes | fdlalaska.org Reviews

https://fdlalaska.org

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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FDL: Frozen Debris Lobes

http://fdlalaska.org/press.html

Looming over Alaska's most economically important highway. Warming speeds world's slowest moving landslides. A cold, creeping menace. Many angles to decode frozen debris lobes. Effective stress and FDL science. Temperamental machinery and FDL science. Attack of the Debris Lobes. Source: KUAC radio broadcast. Debris Lobe Threatens Dalton Highway. As frozen debris field slides toward Dalton Highway, state makes plans to move road. Creeping frozen landslide threatens critical highway and pipeline.

2

FDL: Frozen Debris Lobes

http://fdlalaska.org/partners.html

Looming over Alaska's most economically important highway. Alaska Division of Geological and Geophysical Surveys (DGGS). Key FDL investigators work with DGGS, who has partnered with UAF, providing field support and logistics, and graduate student support. Alaska Department of Transportation and Public Facilities (ADOT&PF). Alaska University Transportation Center (AUTC). US Department of Transportation (USDOT) Office of the Assistant Secretary for Research and Technology (OST-R). Potential infrastructure ...

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FDL: Frozen Debris Lobes

Looming over Alaska's most economically important highway. What are Frozen Debris Lobes? Frozen debris lobes (or FDLs) 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. 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: 29.1 m. Current average rate: 1.7 cm/day. Today's distance to Dalton Highway.

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