Guest Post by James L. Gordon P.Eng.(Retired)
Way back in 2014, my interest in the North Spur started when I read a short book by Cabot Martin titled “Muskrat Madness”. It concentrated on the questionable stability of a natural side dam called the
North Spur which contained layers of sandy silt and sensitive clay. I emailed Cabot, a member of the 2041 committee, on August 27th commenting on his book, and have
commented several times on the Uncle Gnarley blog on the North Spur safety.
NALCOR describes the Spur as -
The north
spur forms a natural earthfill dam,
with
a crest elevation of about
60 m, and about one km long, which connects the
rock knoll to the north
bank of the valley……. The crest width varies
from
about 1,000 m at its north
end to about 70m at its south
end where it has been narrowed by erosion and landslide activity in the past. The head across the spur is presently 16 m from river
level upstream to downstream. The impounding of the reservoir to El. 39 m will increase the
hydraulic head across the spur to 36 m and
stabilization measures are then necessary to ensure its long-term stability under both normal and extreme water
levels. The soils forming the spur consist of a complex interbedded sequence
of relatively low
permeability silty
sands and sands, and sensitive marine
clays.
