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TitleSurficial geology, middle Kitimat River-Hoult Creek, Kitimat-Morice River corridor, British Columbia, parts of NTS 103-I/1 and 8
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorMaynard, D E; Weiland, I C; Blais-Stevens, AORCID logo
SourceGeological Survey of Canada, Canadian Geoscience Map 319, 2019, 1 sheet, Open Access logo Open Access
LinksSurficial geology map collection
LinksCollection de données de géologie de surface
PublisherNatural Resources Canada
Maps1 map
Map Info.surficial geology, surficial sediments and terrain stability, 1:25,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 9 (NAD83)
Mediaon-line; digital
RelatedNRCan photo(s) in this publication
RelatedFor all publications in this group, see the following publications
File formatreadme
File formatpdf (Adobe® Reader®); rtf; xls (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); tiff
ProvinceBritish Columbia
NTS103I/01; 103I/08
AreaKitimat River; Morice River; Hoult Creek
Lat/Long WENS-128.3833 -128.0667 54.2917 54.1917
Subjectssurficial geology/geomorphology; landslides; landslide deposits; debris flows; debris flow deposits; debris fans; talus; slumps; slopewash deposits; sediment transport; slope stability; slope failures; postglacial deposits; organic deposits; fens; bogs; wetlands; peat; organic materials; colluvial deposits; mass wasting; slopewash deposits; fans; talus; alluvial fans; glacial deposits; glacial features; glacial landforms; glacial lakes; tills; ice contact deposits; weathering; sands; gravels; clays; silts; boulders; erosion; scarps; topography; depositional environment; glacial history; glaciation; Wisconsinian glacial stage; deglaciation; coastal environment; coastal erosion; planning; floods; Fraser Glaciation; Risk assessment; sediment transport directions; anthropogenic deposits; organic blanket; organic veneer; colluvial and mass-wasting deposits; colluvial and mass-wasting veneer; colluvial and mass-wasting blanket; alluvial sediments; alluvial floodplain sediments; alluvial terraced sediments; alluvial veneer; glaciomarine sediments; glaciomarine veneer; glaciomarine blanket; glaciofluvial sediments; glaciofluvial outwash plain sediments; glaciofluvial terraced sediments; glaciofluvial outwash fan sediments; glaciofluvial hummocky sediments; glaciofluvial veneer; glaciofluvial blanket; till veneer; till blanket; Phanerozoic; Cenozoic; Quaternary
Illustrationslocation maps; index maps; photographs; geoscientific sketch maps; tables
ProgramPublic Safety Geoscience Marine Geohazards
ProgramProgram of Energy Research and Development (PERD)
Released2019 03 25
AbstractThe 105 km long Kitimat-Morice River corridor features mostly interconnecting valleys linking the coastal community of Kitimat in northwestern British Columbia with the interior valley system of Morice River. The middle Kitimat River-Hoult Creek map area covers a distance of about 20 km along the north valley wall of middle Kitimat River and the lower section of Hoult Creek valley. Mapping of surficial sediments, compilation of landslide deposits, and interpretation of bedrock types were primarily carried out using 1:20 000 British Columbia government aerial photographs dated from 2001 (west half of corridor in NTS 103-I) and 2013 (east half of corridor in NTS 93-L). Older, field-based mapping by the authors in some parts of the study area was incorporated into this mapping, complemented with additional reconnaissance-level field observation in 2016.
Summary(Plain Language Summary, not published)
The Kitimat-Morice River study area in northwest British Columbia is 110 km long and up to 7 km wide from Kitimat east to Morice River. 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.

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