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Cheekye River basin

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Journal Article
Published: 01 February 2003
Environmental and Engineering Geoscience (2003) 9 (2): 99–115.
... floods originating in the upper Cheekye River basin northeast of Stump Lake. Comparison of the volume of lower Cheekye fan and the thickness and areal extent of individual event deposits indicates that the fan may be a product of hundreds of debris flows ( Thurber Engineering and Golder Associates, 1993...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP320.14
EISBN: 9781862395688
... landforms; MR, Mamquam River landforms. Exposures in the upper Cheekye fan include Cat Lake (CA), Mashiter Creek (MC) and Garibaldi Springs (GS). To determine a paraglacial sediment budget, we assume that Mount Garibaldi volcano erupted onto ice filling the Cheekye basin below 1300 m asl, as suggested...
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Journal Article
Published: 01 March 2000
Canadian Journal of Earth Sciences (2000) 36 (12): 2023–2031.
... the reduction in annual sediment yield from the Cheekye basin (∼50 km 2 ), from the onset of the paraglacial period to the present. The total volume of material delivered to the valley bottom and stored in the lower Cheekye fan or the Squamish River delta is about 16 × 10 8  m 3 . Mathews ( 1952...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2001.211.01.08
EISBN: 9781862394599
... of Cheekye fan and its catchment basin showing stream orders. Prior to progradation of the Squamish River delta to its present position, the proto lower fan extended into the Howe Sound fjord as a fan-delta. The fan-delta was built during a period of higher sea level 10.2–9.8 ka BP and later developed...
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Journal Article
Published: 10 January 2018
Canadian Journal of Earth Sciences (2018) 55 (4): 331–342.
... of sediment to Cheakamus River ( Friele and Clague 2009 ). The exponential decline in sediment yield in the Cheekye basin through the Holocene fits the primary exhaustion model of sediment delivery in smaller paraglacial watersheds ( Ballantyne 2002 ; Friele and Clague 2009 ). Sediments exposed...
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Journal Article
Journal: GSA Bulletin
Published: 22 March 2018
GSA Bulletin (2018) 130 (9-10): 1457–1473.
... for investigating: ( i ) the postglacial lateral migration of the Adige River in relation to sediment delivered from the Gadria-Strimm and Lasa basins; and ( ii ) the internal architecture of the two fans, for gaining geomorphic insights on the style of fan progradation and aggradation. Line Lasa 3, which crosses...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2010
GSA Bulletin (2010) 122 (3-4): 537–562.
... and in small lakes in the central and northern basin after construction of a topographic high that prevented the Quartzite-Chert Member through-going braided river from entering this part of the basin. The Krum Hills expose the King Lear Formation and underlying phyllites of the backarc basinal terrane...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2010
GSA Bulletin (2010) 122 (9-10): 1569–1584.
... width and basin hydrology responses, and are presumed constant. It may be shown that no matter what the details of the formulation, for all points in a river channel, we may write where k s and θ are parameters known as the channel steepness and channel concavity indices, respectively (e.g...
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Image
Figure 8. Simplified reconstruction of events affecting Stump Lake and envi...
Published: 01 February 2003
) block the north end of the Stump Lake basin, deepening and enlarging the lake. (D) Early Holocene debris flows are routed down Cheekye River and do not enter Stump Lake. (E) A large debris flow enters Stump Lake about 6,900 years ago and raises its level. (F) Middle and late Holocene debris flows
Journal Article
Published: 13 February 2004
Canadian Journal of Earth Sciences (2004) 41 (2): 165–182.
.... Woodsworth G.J. 1995 . Improved age estimates for White River and Bridge River tephras, western Canada . Canadian Journal of Earth Sciences , 32 : 1172 – 1179 . Clague J.J. Friele P.A. Hutchinson I. 2003 . Debris flows in the Cheekye River basin, British Columbia...
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Journal Article
Published: 03 March 2021
Environmental and Engineering Geoscience (2021)
... events. These include the Johnson Landing event, where a debris flow resulted in four fatalities in July 2012, and Cheekye River and Rubble Creek (Figures 3 and 6). Details on these exceptions include: Flow-R propagation does not replicate the special case of the Johnsons Landing debris flow, where...
Journal Article
Journal: Geology
Published: 10 June 2019
Geology (2019) 47 (8): 791–794.
... Geomorphologie , v. 104 , supplement, p. 13 – 26 . Jakob , M. , and Friele , P. , 2010 , Frequency and magnitude of debris flows on Cheekye River, British Columbia : Geomorphology , v. 114 , p. 382 – 395 , https://doi.org/10.1016/j.geomorph.2009.08.013 . Jakob , M. , Bovis , M...
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Journal Article
Journal: Geosphere
Published: 01 April 2017
Geosphere (2017) 13 (2): 369–390.
... , 2012b ) provided a first description of the event, including seismic signal analysis, a general geomorphic description, and numerical modeling. Roche et al. (2011) studied the effects of the landslide on the Lillooet River discharge. Allstadt (2013) analyzed the seismic data from the event to infer...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2011
DOI: 10.1144/SP351.14
EISBN: 9781862395992
... geology is clearly important, locally concentrated glacial trough erosion and rebound stresses may be involved. This new category also embraces certain fans reported in the Himalaya (prehistoric), British Columbia (Cheekye) and the Andes (Huascaran, Peru in 1970), where active tectonics, vulcanicity...
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