Last week, TVA released a comprehensive report which detailed the probable cause of the failure. In a nutshell, there was an inherent weakness under the dike that probably contributed to the failure.
This weakness consisted of a six-inch thick "slimes" layer of flyash, eroded dike soils and re-deposited river sediments formed from how the plant was operated in the 1950s. The layer was named for its slippery, viscous feel. Creep failure of this slime layer occurred under the loose wet ash which may have started the failure sequence.
Images from Root Cause Analysis full report.
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