Queen
Bess Lake, one day after catastrophic outburst
Queen Bess Lake
is filled with icebergs derived from the glacier avalanche that triggered the
outburst of July 1997. Note icebergs stranded at the pre-outburst level
of the lake, which is 8 m higher than the level of the lake when the photo was
taken. Also note the breach in the moraine dam in the foreground.
The present level of the lake is controlled by a bedrock sill at the downvalley
end of the breach. (photo courtesy of Interfor Ltd.).
Map
of Queen Bess area
This map shows the flood path of the 1997 outburst
flood from moraine-dammed Queen Bess Lake in the southern Coast Mountains of British
Columbia. It also shows positions of the snout of Diadem Glacier at various
times since 1949. The Queen Bess event occurred after Diadem Glacier retreated
out of the lake and up a steep rock slope. The unsupported toe of the glacier
broke away in hot weather in July 1997 and slid into the lake, producing a large
displacement wave that flowed over, and breached the moraine dam.