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Neoglacial history of the Coast Mountains near Bella Coola
The maximum Holocene extent of glaciers in the study area is marked by late Neoglacial (Little Ice Age) terminal moraines. Moraine stratigraphy and 14C dates from a small number of sites suggest thatExpand
Sediment source and hydroclimatic inferences from glacial lake sediments: the postglacial sedimentary record of Lillooet Lake, British Columbia
Lillooet River drains 3850 km2 of partly glacier-covered terrain before entering Lillooet Lake in the southern Coast Mountains of British Columbia. The elongated lake covers an area of 21 km2 andExpand
LITTLE ICE AGE HISTORY OF TZEETSAYTSUL GLACIER, TWEEDSMUIR PROVINCIAL PARK, BRITISH COLUMBIA
This paper describes licheno- metric and dendroglaciological investigations of Little Ice Age (LIA) deposits at Tzeetsaytsul Glacier, Tweedsmuir Provincial Park, British Columbia. The glacierExpand
Physical Geography of Ontario
Introduction Ontario, the second largest province of Canada, covers approximately 1 million km2 and extends approximately from 42°N to 57°N latitude and from 75°W to 95°W longitude. The majorExpand
Glaciolacustrine varved sediment as an alpine hydroclimatic proxy
The physical significance of a negative correlation between a varve record from Mud Lake, British Columbia, and temperature is discussed in the context of a process-network. The process-network isExpand
Glacimarine sedimentation in Kangerdluk (Disko Fjord), West Greenland, in response to a surging glacier
Abstract Beginning in 1995, a large outlet glacier of the Sermersauq Ice Cap on Disko Island surged 10.5 km downvalley to within 10 km of the head of the fjord, Kuannersuit Sulluat, reaching itsExpand
Channel and Floodplain Facies in a Wandering Gravel-Bed River
Bella Coola River drains 5050 km2 of glacierized mountains on the central coast of British Columbia. Spring snowmelt and autumn rainstorm floods occur up to 1000 m3sp'. The valley-fill is composed ofExpand
Late-Holocene record of lagoon evolution, climate change, and hurricane activity from southeastern Cuba
A sediment core from a lagoon in southeastern Cuba was the focus of a multi-proxy paleoenvironmental study to investigate lagoon response to sea-level change and climate change and also to inferExpand
Paleohydrology of the Bella Coola River basin : an assessment of environmental reconstruction
Recent geomorphic and hydrologic environments of a mid-latitude alpine basin are investigated under the integrative theme of paleohydrology. The aims of t h i s research are: 1) to characterize theExpand
WANDERING GRAVEL‐BED RIVERS
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