GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleSurficial geology, Maitland Island, Douglas Channel area, British Columbia, parts of NTS 103-H/10, 11, 14, and 15
DownloadDownloads
AuthorWeiland, I C; Maynard, D E; Blais-Stevens, A; Geertsema, M
SourceGeological Survey of Canada, Canadian Geoscience Map 299, 2017, 1 sheet, https://doi.org/10.4095/300305
Year2017
PublisherNatural Resources Canada
EditionPrelim.
Documentserial
Lang.English
Maps1 map
Map Info.surficial geology, surficial deposits terrain stability, 1:25,000
ProjectionUniversal Transverse Mercator Projection, zone 9U (NAD83)
Mediaon-line; digital
RelatedFor all publications in this survey, see the following publications
File formatreadme
File formatpdf (Adobe® Reader®); rtf; xlsx (Microsoft® Excel® 2010); gdb (ESRI® ArcGIS(TM) 10.x); shp (ESRI® ArcGIS(TM) 10.x); xml (ESRI® ArcGIS(TM) 10.x); mxd (ESRI® ArcGIS(TM) 10.x)
ProvinceBritish Columbia
NTS103H/10; 103H/11; 103H/14; 103H/15
AreaDouglas Channel; Maitland Island; Sue Channel; Emilia Island; Hawkesbury Island; Foch Lagoon; Gilttoyees Inlet; Miskatla Inlet
Lat/Long WENS-129.2333 -128.9236 53.8000 53.6639
Subjectssurficial geology/geomorphology; landslides; landslide deposits; debris flows; sediment transport; slope stability; slope failures; postglacial deposits; organic deposits; fens; bogs; wetlands; peat; organic materials; colluvial deposits; fans; talus; mass wasting; hummocks; slumps; alluvial deposits; alluvial fans; flood plains; floods; terraces; glacial deposits; glacial features; glacial landforms; glaciomarine deposits; scarps; glaciofluvial deposits; proglacial deposits; meltwater channels; kame terraces; deformation; faults; tills; sands; gravels; clays; silts; boulders; weathering; erosion; depositional environment; sedimentary structures; glacial history; glaciation; Wisconsinian glacial stage; deglaciation; coastal environment; coastal erosion; planning; Fraser Glaciation; geological hazards; terrain stability mapping; risk assessment; folic organic material; debris slides; debris avalanches; diamicton; gravity-induced movement; debris floods; snow avalanches; rock falls; rock slides; submarine gravity flows; landslide tracks; Phanerozoic; Cenozoic; Quaternary
Illustrationslocation maps; index maps; geoscientific sketch maps; tables; photographs
ProgramMarine Geohazards, Public Safety Geoscience
Image
Released2017 07 19
AbstractDouglas Channel is a 100 km long fjord located south of the municipality of Kitimat, in northwest British Columbia. The Maitland Island map area covers the middle portion of Douglas Channel where it meets Sue Channel in the south portion of the map area and the mouths of Foch Lagoon, Gilttoyees Inlet and Miskatla Inlet in the northern portion. The total distance within Douglas Channel is roughly 21 km. Mapping of surficial sediments, compilation of landslide deposits, and preliminary interpretation of bedrock types up to height of land were primarily carried out using British Columbia airphotos dated from 2001, 2003, and 2007 ranging in scales from 1:15 000 to 1:25 000. Older, field-based mapping by the authors in some isolated parts of the study area was incorporated into this mapping, complemented with additional, reconnaissance-level field observation in 2015 and 2016.
Summary(Plain Language Summary, not published)
This is one of six maps that cover the surficial geology and landslide inventory of Douglas Channel a 100 km fjord, located in Northwest British Columbia. It was compiled to provide baseline information on the surface sediments and slope stability of the fjord.
GEOSCAN ID300305