Filters: Contacts: Gilbert, Robert (X) > partyWithName: Desloges, Joseph R. (X)

Filters Date Range Past year (0) Past month (0) Past week (0) Past day (0) Custom range... To   Search Extensions Citation (9) Shapefile (2) Types Citation (9) Downloadable (2) Map Service (2) OGC WFS Layer (2) OGC WMS Layer (2) Shapefile (2) Contacts Gilbert, Robert Hodder, Kyle R. Lamoureux, Scott F. Serink, Andrea Categories Publication (9) Data (2) View Results as: JSON ATOM CSV

The geomorphic and paleoenvironmental record in the sediments of Atlin Lake, northern British Columbia Atlin Lake in northern British Columbia and southern Yukon Territory is the largest natural lake in the North American Cordillera (791 km super(2)). Inflow from the Juneau Ice Field delivers large volumes of sediment to the proximal basins of Willison Bay and Llewellyn Inlet. Sediment is distributed by interflow and underflow through these basins. Based on acoustic data, each of these basins contain Holocene deposits about 120 m thick, representing mean annual accumulation since deglaciation of more than 1 cm/a. Cores confirm this, except that the formation of a small lake at the toe of Llewellyn Glacier during about the past 50 years is trapping sediment and has reduced accumulation in Llewellyn Inlet by an order... Categories: Publication; Types: Citation; Tags: M2-Standardized Stream and Lake Information, Paleo and Holocene The record of Glacial Lake Champagne in Kusawa Lake, southwestern Yukon Territory Categories: Data, Publication; Types: Citation, Downloadable, Map Service, OGC WFS Layer, OGC WMS Layer, Shapefile; Tags: P3b-Vegatation Productivity Changes Due to Temperature change The record of Glacial Lake Champagne in Kusawa Lake, southwestern Yukon Territory Categories: Publication; Types: Citation; Tags: P3b-Vegatation Productivity Changes Due to Temperature change The geomorphic and paleoenvironmental record in the sediments of Atlin Lake, northern British Columbia Atlin Lake in northern British Columbia and southern Yukon Territory is the largest natural lake in the North American Cordillera (791 km super(2)). Inflow from the Juneau Ice Field delivers large volumes of sediment to the proximal basins of Willison Bay and Llewellyn Inlet. Sediment is distributed by interflow and underflow through these basins. Based on acoustic data, each of these basins contain Holocene deposits about 120 m thick, representing mean annual accumulation since deglaciation of more than 1 cm/a. Cores confirm this, except that the formation of a small lake at the toe of Llewellyn Glacier during about the past 50 years is trapping sediment and has reduced accumulation in Llewellyn Inlet by an order... Categories: Publication; Types: Citation; Tags: M2-Standardized Stream and Lake Information, Paleo and Holocene The geomorphic and paleoenvironmental record in the sediments of Atlin Lake, northern British Columbia Atlin Lake in northern British Columbia and southern Yukon Territory is the largest natural lake in the North American Cordillera (791 km super(2)). Inflow from the Juneau Ice Field delivers large volumes of sediment to the proximal basins of Willison Bay and Llewellyn Inlet. Sediment is distributed by interflow and underflow through these basins. Based on acoustic data, each of these basins contain Holocene deposits about 120 m thick, representing mean annual accumulation since deglaciation of more than 1 cm/a. Cores confirm this, except that the formation of a small lake at the toe of Llewellyn Glacier during about the past 50 years is trapping sediment and has reduced accumulation in Llewellyn Inlet by an order... Categories: Data, Publication; Types: Citation, Downloadable, Map Service, OGC WFS Layer, OGC WMS Layer, Shapefile; Tags: Monitoring 2-Standardized Stream and Lake Information, Paleo and Holocene The geomorphic and paleoenvironmental record in the sediments of Atlin Lake, northern British Columbia Atlin Lake in northern British Columbia and southern Yukon Territory is the largest natural lake in the North American Cordillera (791 km super(2)). Inflow from the Juneau Ice Field delivers large volumes of sediment to the proximal basins of Willison Bay and Llewellyn Inlet. Sediment is distributed by interflow and underflow through these basins. Based on acoustic data, each of these basins contain Holocene deposits about 120 m thick, representing mean annual accumulation since deglaciation of more than 1 cm/a. Cores confirm this, except that the formation of a small lake at the toe of Llewellyn Glacier during about the past 50 years is trapping sediment and has reduced accumulation in Llewellyn Inlet by an order... Categories: Publication; Types: Citation; Tags: M2-Standardized Stream and Lake Information, Paleo and Holocene The record of Glacial Lake Champagne in Kusawa Lake, southwestern Yukon Territory Categories: Publication; Types: Citation; Tags: P3b-Vegatation Productivity Changes Due to Temperature change The geomorphic and paleoenvironmental record in the sediments of Atlin Lake, northern British Columbia Atlin Lake in northern British Columbia and southern Yukon Territory is the largest natural lake in the North American Cordillera (791 km super(2)). Inflow from the Juneau Ice Field delivers large volumes of sediment to the proximal basins of Willison Bay and Llewellyn Inlet. Sediment is distributed by interflow and underflow through these basins. Based on acoustic data, each of these basins contain Holocene deposits about 120 m thick, representing mean annual accumulation since deglaciation of more than 1 cm/a. Cores confirm this, except that the formation of a small lake at the toe of Llewellyn Glacier during about the past 50 years is trapping sediment and has reduced accumulation in Llewellyn Inlet by an order... Categories: Publication; Types: Citation; Tags: Monitoring 2-Standardized Stream and Lake Information, Paleo and Holocene The record of Glacial Lake Champagne in Kusawa Lake, southwestern Yukon Territory Categories: Publication; Types: Citation; Tags: P3b-Vegatation Productivity Changes Due to Temperature change