Title | Surficial geology, Hartley Bay, Douglas Channel area, British Columbia, parts of NTS 103-H/6 and 11 |
Download | Downloads |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Maynard, D E; Weiland, I C; Blais-Stevens, A ; Geertsema, M |
Source | Geological Survey of Canada, Canadian Geoscience Map 302, 2017, 1 sheet, https://doi.org/10.4095/299824 Open Access |
Links | Erratum
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Links | Surficial geology map collection
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Links | Collection de données de géologie de surface
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Image |  |
Year | 2017 |
Publisher | Natural Resources Canada |
Edition | Prelim. |
Document | serial |
Lang. | English |
Maps | 1 map |
Map Info. | surficial geology, surficial deposits terrain stability, 1:25,000 |
Projection | Universal Transverse Mercator Projection, UTM zone 9U (NAD83) |
Media | on-line; digital |
Related | NRCan photo(s) in this
publication |
Related | For all publications in this group, see the following publications |
File format | readme
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File format | pdf (Adobe® Reader®); rtf; docx (Microsoft® Word®); xlsx (Microsoft® Excel® 2010); gdb (ESRI® ArcGIS(TM) v.10.x); shp (ESRI® ArcGIS(TM) v.10.x); xml (ESRI® ArcGIS(TM) v.10.x); mxd (ESRI® ArcGIS(TM)
v.10.x) |
Province | British Columbia |
NTS | 103H/06; 103H/11SE; 103H/11SW |
Area | Hartley Bay; Douglas Channel; Kishkosh Inlet; Verney Passage; Hawkesbury Island; Gribble Island; Wright Sound; Grenville Channel; Coghlan Anchorage; Promise Island |
Lat/Long WENS | -129.3500 -129.0833 53.5167 53.3111 |
Subjects | surficial geology/geomorphology; glaciation; Wisconsinian glacial stage; landslides; landslide deposits; debris flows; slope stability; sediment transport; slope development; deformation; debris fans;
talus; mass wasting; slopewash deposits; debris flow deposits; rockfall chutes; slumps; postglacial deposits; organic deposits; fens; bogs; wetlands; peat; colluvial deposits; fans; hummocks; weathering; alluvial deposits; alluvial fans; flood
plains; marine deposits; beach deposits; terraces; deltaic deposits; emergence; deglaciation; glacial deposits; glaciomarine deposits; glaciofluvial deposits; meltwater channels; tills; clays; silts; sands; gravels; boulders; planning; Fraser
Glaciation; Natural hazards; anthropogenic deposits; Phanerozoic; Cenozoic; Quaternary |
Illustrations | location maps; index maps; tables; photographs; geoscientific sketch maps |
Program | Public Safety
Geoscience Marine Geohazards |
Released | 2017 07 19; 2018 10 04 |
Abstract | Douglas Channel is a 100 km long fjord located south of the municipality of Kitimat, in northwest British Columbia. The Hartley Bay map area covers the southern portion of Douglas Channel where it meets
Wright Sound and Verney Passage. The area also covers Promise Island, the southwest portion of Gribbell Island, southwest Hawkesbury Island, and a stretch of the western shore of Douglas Channel (mainland) that extends over about 17 km southward from
Kiskosh Inlet. 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. The
photograph (Figure 1) taken from the southwest side of Hawkesbury Island, looking north, shows the surface expression of deep-seated gravitational slope deformation features (DSGSD; black arrows) also called tension cracks or "sackungen". |
Summary | (Plain Language Summary, not published) This is one of six surficial geology an d landslide inventory maps that cover Douglas Channel. Douglas Channel is a 100-km long fjord located south of
the municipality of Kitimat, in NW British Columbia. The purpose is to provide baseline geoscience information on surface sediments and landslide hazard to decision-makers. |
GEOSCAN ID | 299824 |
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