Last week a
retired Swedish geoscientist, industry leader, consultant, Professor, and
internationally recognized expert on “Quick Clay”, Dr. Stig Bernander, spent three days studying what he described as a “live” land mass on the lower Churchill River. He was able to personally view, on the ground and from the air, a great many landslides and see physical evidence of active movement over a large area including the "North Spur".
He spent
another four days editing his notes, selecting photographic evidence and lecturing at the LSPU
Hall and at Memorial University on the dangers of Nalcor relying upon “outdated”
geotechnical analysis of the problem.
Quick Clays are unique, sensitive glaciomarine clays. The clay deposits, at the North Spur as elsewhere, occurred when sea water levels were much higher. They are unstable clays. Their peculiar characteristics are known to cause landslides. When Quick Clay is subjected to sufficient stress, the material may liquefy. (Locally, some call the clays "pug".)
When a
person of the stature of Dr. Bernander, having no connection to this Province, is troubled enough
to perform this public service, pro bono, you have a right to think there is cause for
concern.
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Rissa slide, Norway
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When the
Vice-President of Nalcor, Gilbert Bennett, shows up at Dr. Bernander’s lecture
at Memorial University, not to welcome the man or to acknowledge his internationally accepted engineering models for assessing landslide risk, not even to ask him a question, but only to express umbrage against the Professor,
you know the Corporation has gotten far too used to not being challenged by competent third parties.