|Title||The sedimentary record and Neoglacial history of Tide Lake, northwestern British Columbia|
|Author||Clague, J J; Mathews, W H|
|Source||Canadian Journal of Earth Sciences vol. 29, no. 11, 1992 p. 2383-2396, https://doi.org/10.1139/e92-186 Open Access|
|Alt Series||Geological Survey of Canada, Contribution Series 49591|
|Publisher||Canadian Science Publishing|
|Media||paper; on-line; digital|
|Program||NSERC Natural Sciences and Engineering Research Council of
|Abstract||Tide Lake was the largest glacier-dammed lake in British Columbia before its demise in the early twentieth century. Situated in the northern Coast Mountains, the lake was impounded by Frank Mackie
Glacier and its Neoglacial end moraine. A study of Tide Lake has provided information on styles of glaciolacustrine sedimentation and the chronology of the Neoglacial interval.Much of the sediment underlying the floor of Tide Lake was transported by
subglacial and proglacial meltwater streams flowing from nearby glaciers. During the last phase of the lake, large subaqueous fans were built in front of Berendon and Frank Mackie glaciers, and deltas formed on the east side of the basin.
Rhythmically bedded fine sediments, which cover much of the lake floor but are almost completely lacking on the slopes above, were deposited from underflows originating on deltas and subaqueous fans and by fallout from interflows and overflows.Three
major and one minor lake phases are recognized from stratigraphic, geomorphic, radiocarbon, and dendrochronological data: the earliest phase is undated, but older than 3000BP (1300 B.C.); the second phase has yielded radiocarbon ages of 2600 2700BP
(800 1000 B.C.); a third, minor phase, during which Tide Lake was restricted to the northern part of the basin, began before 1600BP (A.D. 350 550) and probably ended a few hundred years later; the last phase may have begun as early as 1000BP (A.D.
1000 1150), peaked in the seventeenth century, and ended in the early twentieth century. During each of the four phases, Tide Lake fluctuated in a complex fashion and at times was empty. The second phase corresponds to a widely recognized middle
Neoglacial advance in western North America; the last phase is coincident with the Little Ice Age. Outburst floods from Tide Lake in the nineteenth and early twentieth centuries devastated Bowser River valley as far downstream as Bowser Lake. The
last of the floods occurred around A.D. 1930 when the Frank Mackie moraine was breached and the lake emptied for the last time. |