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Lillooet Lake

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Journal Article
Published: 14 September 2017
Canadian Journal of Earth Sciences (2018) 55 (1): 18–32.
... and lacustrine processes responsible for the distribution and character of sediments in Lillooet Lake. He estimated average total clastic sediment yield in the Lillooet River watershed to be 334 Mg·km −2 ·a −1 . Gilbert (1975) further showed that the lake sediments are annually laminated (varved...
FIGURES | View All (13)
Journal Article
Published: 01 October 1975
Canadian Journal of Earth Sciences (1975) 12 (10): 1697–1711.
...R. Gilbert Abstract Sediment from Lillooet River Basin, 3580 sq km of alpine and subalpine landscape, 7% of which is glacier-covered, is deposited in Lillooet Lake. During the summer when the lake is stratified by temperature and suspended sediment content, processes of interflow and underflow...
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Map of the <span class="search-highlight">Lillooet</span> <span class="search-highlight">Lake</span> watershed. Inset left: bathymetry of <span class="search-highlight">Lillooet</span> <span class="search-highlight">Lake</span>...
Published: 14 September 2017
Fig. 1. Map of the Lillooet Lake watershed. Inset left: bathymetry of Lillooet Lake and core locations.
Image
Sediment yield record derived from <span class="search-highlight">Lillooet</span> <span class="search-highlight">Lake</span> sediments for the period A...
Published: 14 September 2017
Fig. 2. Sediment yield record derived from Lillooet Lake sediments for the period AD 1179–2004.
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Sediment yield record derived from <span class="search-highlight">Lillooet</span> <span class="search-highlight">Lake</span> sediments for the period A...
Published: 14 September 2017
Fig. 3. Sediment yield record derived from Lillooet Lake sediments for the period AD 1629–1997. [Colour online.]
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( a ) AD 1931 and ( b ) 1776 varves from <span class="search-highlight">Lillooet</span> <span class="search-highlight">Lake</span> cores C, 2, and E (l...
Published: 14 September 2017
Fig. 12. ( a ) AD 1931 and ( b ) 1776 varves from Lillooet Lake cores C, 2, and E (left to right; proximal to distal core locations). The vertical black bar at lower left of each photograph is 1 cm. [Colour online.]
Image
Figure 1. A: Aerial photograph of <span class="search-highlight">Lillooet</span> <span class="search-highlight">Lake</span>, showing distinct scalloped...
Published: 01 October 2005
Figure 1. A: Aerial photograph of Lillooet Lake, showing distinct scalloped plunge line of river plume where Lillooet River enters lake. Measurement locations at 17 m (D), 25 m (E, G, H, and I) and 55 m (F) and transect line (C) are shown. Insert shows location of Lillooet Lake in British Columbia
Journal Article
Published: 01 May 1991
Canadian Journal of Earth Sciences (1991) 28 (5): 800–815.
... retreating rapidly northwest up the Lillooet valley, which may have existed for no more than 400 years in the lower valley prior to opening of Lillooet Lake (which now traps most sediment derived from the upper basin); and ( ii ) inflow from the south as the late-glacial Fraser River rapidly built a delta...
Series: GSA Special Papers
Published: 01 December 2015
DOI: 10.1130/2015.2513(03)
... the following: Mojave-Sonora megashear, Melones-Bear Mountain, Wolf Creek, Bear Wallows–South Fork, Siskiyou and Soap Creek Ridge faults, Ross Lake fault zone, as well as Harrison Lake, Bridge River suture, Lillooet Lake, and Owl Creek faults. Northward within the Coast Range shear zone, pendants of continental...
Journal Article
Journal: Geology
Published: 01 October 2005
Geology (2005) 33 (10): 765–768.
...Figure 1. A: Aerial photograph of Lillooet Lake, showing distinct scalloped plunge line of river plume where Lillooet River enters lake. Measurement locations at 17 m (D), 25 m (E, G, H, and I) and 55 m (F) and transect line (C) are shown. Insert shows location of Lillooet Lake in British Columbia...
FIGURES
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Comparison of suspended sediment yield for the <span class="search-highlight">Lillooet</span> River watershed (th...
Published: 14 September 2017
1989 , p. 452) in British Columbia. Closed symbols are data from natural landscapes; open symbols are data from landscapes influenced by natural or human disturbances. Measurements for Lillooet Lake are derived from a 57 year record of lake sedimentation reported by Gilbert (1973) . Modified from
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Schematic depiction of the debris flow and rock avalanche phases of the two...
Published: 13 February 2004
Fig. 14. Schematic depiction of the debris flow and rock avalanche phases of the two large Pylon Peak landslides. The extent of the rock avalanche deposit defines the proximal hazard zone. The debris flows reached Lillooet Lake at times when the delta front was much farther upvalley, and thus
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Relation between annual sediment deposition in Green <span class="search-highlight">Lake</span> and the <span class="search-highlight">Lillooet</span> ...
Published: 07 February 2007
Fig. 10. Relation between annual sediment deposition in Green Lake and the Lillooet River annual maximum daily discharge. Extreme autumn rainstorm and unusual snowmelt years are labeled. Regression model is for average regime years (excludes labeled rainstorm and snowmelt years and identified
Journal Article
Published: 05 July 2006
Canadian Journal of Earth Sciences (2006) 43 (6): 671–678.
... considered. The most significant predictors of Green Lake varve thickness include flood magnitude and average air temperature during the spring, summer, and autumn. Varve thickness is correlated to the annual maximum mean daily discharge of Lillooet River, but this relationship is not stable through time...
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Journal Article
Published: 11 September 2000
Canadian Journal of Earth Sciences (2000) 37 (10): 1321–1334.
... and the 100 year record of varved lake sedimentation in Lillooet Lake (located 80 river kilometres downstream of Meager Creek) ( Gilbert 1975 ; Desloges and Gilbert 1994 ). This indicates that although Meager Creek and its tributaries probably dominate the delivery of coarse sediment to Lillooet River...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP320.14
EISBN: 9781862395688
... in the headwaters of Lillooet River, which has a watershed area upstream of Lillooet Lake of about 3150 km 2 . The edifice is imposing and covers an area of about 80 km 2 , but it represents only 2.5% of the area of the Lillooet River watershed. Fig. 7. Geology and landforms of the Mount Meager massif...
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Journal Article
Published: 07 February 2007
Canadian Journal of Earth Sciences (2006) 43 (12): 1777–1790.
...Fig. 10. Relation between annual sediment deposition in Green Lake and the Lillooet River annual maximum daily discharge. Extreme autumn rainstorm and unusual snowmelt years are labeled. Regression model is for average regime years (excludes labeled rainstorm and snowmelt years and identified...
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Journal Article
Journal: Geology
Published: 01 January 2016
Geology (2016) 44 (1): 43–46.
... sedimentary record of Lillooet Lake, British Columbia : Journal of Hydrology , v. 159 , p. 375 – 393 , doi:10.1016/0022-1694(94)90268-2. Dietze M. Dietze E. , 2013 , EMMAgeo: End-member modelling algorithm and supporting functions for grain-size analysis, R package version 0.9.1 : http...
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Journal Article
Published: 07 July 2006
Canadian Journal of Earth Sciences (2006) 43 (6): 679–689.
... from the vent, which would be as far as present-day Alberta ( Stevenson 1947 ; Nasmith et al. 1967 ; Westgate and Dreimanis 1967 ). Welded block-and-ash flow deposits blocked Lillooet River, creating a temporary lake upstream. Subsequent failure of the dam released the lake water as a catastrophic...
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Journal Article
Published: 06 August 2004
Canadian Journal of Earth Sciences (2004) 41 (8): 903–918.
...Alberto V. Reyes; John J. Clague Abstract Holocene lateral moraines in the Coast Mountains of British Columbia are commonly composed of multiple drift units related to several glacier advances. In this paper, we document lateral moraine stratigraphy at Lillooet Glacier in the southern Coast...
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