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Deming Glacier

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Journal Article
Journal: Geosphere
Published: 01 August 2013
Geosphere (2013) 9 (4): 827-852.
... Tertiary normal fault, and the Canyon Creek scarp lies in close proximity to the south-dipping Canyon Creek fault and the south-dipping Glacier Extensional fault. Both scarps are south-side-up, opposite the sense of displacement observed on the nearby bedrock faults. Trenches excavated across these scarps...
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Series: GSA Field Guide
Published: 01 January 2007
DOI: 10.1130/2007.fld009(04)
EISBN: 9780813756097
... was witnessed by Hudson’s Bay traders at Fort Langley on the Fraser River and “covered the whole country with ashes” ( Gibbs, 1874 ). Hydrothermally altered lapilli and ballistic blocks were ejected onto the glaciers and upper slopes of the mountain, and tephra set YP (Stop 3) was deposited on the surrounding...
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Series: GSA Field Guide
Published: 01 January 2007
DOI: 10.1130/2007.fld009(02)
EISBN: 9780813756097
... Abstract As the Vashon glacier retreated from its terminal position in the southern Puget-Lowland and thinned rapidly, marine waters invaded the central and northern lowland, floating the ice and depositing Everson glaciomarine drift over a wide area from southern Whidbey Island...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2013
GSA Bulletin (2013) 125 (3-4): 445-452.
... dry conditions in this region occurred as rapidly as 300 yr during the early Holocene, with a subsequent increase in moisture occurring rapidly in the late Holocene. Here, we report a 9500 yr multiproxy sediment record from Deming Lake, Minnesota, USA, that demonstrates only subtle dynamics during...
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Journal Article
Journal: GSA Bulletin
Published: 01 February 2001
GSA Bulletin (2001) 113 (2): 274-288.
... free except for a small tongue of ice from the piedmont tongue. Thus, the position of the Cordilleran ice-sheet margin was well north of the Nooksack drainage at this time and well below intervening drainage divides. The Nooksack Middle Fork ( Figs. 1 and 4 ) originates from the Deming Glacier...
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Image
Figure 13. Black Buttes stratovolcano and south side of ice-mantled Mount B...
Published: 01 June 2003
andesitic breccia sheets wraps ice-filled bowl where Deming Glacier has removed altered fragmental core of the volcano. Portrait Rock, the cliffy window enclosed by Deming Glacier, consists of six andesitic lava flows derived from Mount Baker. Between gorge occupied by Deming Glacier and moraine-rimmed
Series: GSA Field Guide
Published: 01 January 2007
DOI: 10.1130/2007.fld009(05)
EISBN: 9780813756097
... cumulative effects analysis (also known as watershed analysis). One of the elements of this analysis is a mass wasting assessment ( Fig. 6 ; Benda, 1996 ). From Glacier Creek Lodge, backtrack west on Mount Baker Highway toward Bellingham. Approximately 3 miles west of Deming, turn right (north) on SR 9...
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Series: GSA Field Guide
Published: 01 January 2014
DOI: 10.1130/2014.0038(03)
EISBN: 9780813756387
... as debris flow, 8.8 as hyperconcentrated flow Deming Glacier debris flow June 1927 10 100 Glacial ice 4.7 as debris flow Debris flow at Elbow Lake trailhead 1740 ± 30 14 C yr B.P. 10 100 Glacial ice 6 as debris flow † Ridley Creek lahar 5782 B.P.§ 1 50 15 130 >32.4 Middle...
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Series: GSA Field Guide
Published: 01 January 2014
DOI: 10.1130/2014.0038(05)
EISBN: 9780813756387
... just across the border in British Columbia north of Lynden. Note person for scale. Figure 18. (A) Radiocarbon dates on wood and shells from Bellingham gmd. (B) Radiocarbon dates from Bellingham gmd, Deming sand, and Kulshan gmd. Figure 19. (A) LiDAR image of Lake Padden...
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Journal Article
Journal: GSA Bulletin
Published: 01 June 2003
GSA Bulletin (2003) 115 (6): 729-764.
... andesitic breccia sheets wraps ice-filled bowl where Deming Glacier has removed altered fragmental core of the volcano. Portrait Rock, the cliffy window enclosed by Deming Glacier, consists of six andesitic lava flows derived from Mount Baker. Between gorge occupied by Deming Glacier and moraine-rimmed...
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Journal Article
Published: 18 December 2003
Canadian Journal of Earth Sciences (2003) 40 (12): 1767-1772.
... in Washington, these sediments include the Kulshan (glaciomarine), Deming (fluvial), and Bellingham (glaciomarine) members and are thought to be equivalent to the Fort Langley sediments in B.C. (Fig.  1 b ). Deposits include a distinctive blue-gray fossiliferous stony mud, with till-like mixtures, marine clay...
FIGURES
Series: Field Guide
Published: 01 January 2003
DOI: 10.1130/0-8137-0004-3.137
EISBN: 9780813756042
... terrace (Easterbrook, 1979). Return to Highway 2; turn right and return to Farmer. Turn right at Farmer and drive 9 mi to the Withrow moraine. Return to Welcome and turn left on Mosquito Lake Rd. Drive across the Nooksack Middle Fork bridge to Deep Kettle Bog. Figure 18. Deming glacier...
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Journal Article
Journal: Geology
Published: 01 March 2006
Geology (2006) 34 (3): 169-172.
... 07 2005 04 11 2005 Geological Society of America 2006 ice glacier water veins bacteria eukaryote bacterial habitat Until recently, ice on Earth was thought to be devoid of life due to a combination of low temperatures, absence of liquid water, dilute chemical...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2012
AAPG Bulletin (2012) 96 (2): 355-374.
... in the nearby Glacier Pool ( Figure 2 ). In the study area, the shaly siltstone interval overlying the distal turbidite lobe is the main reservoir interval. Figure 1 A schematic stratigraphic cross section of the westward prograding clastic wedge of the Lower Triassic Montney Formation showing...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 2002
AAPG Bulletin (2002) 86 (5): 907-918.
... sediments. Propagation of fluid-filled fractures has been invoked to explain crevasses in glaciers ( Weertman, 1971a , 1971b ), magma transport in the crust ( Weertman, 1971a , 1971b ; Secor and Pollard, 1975 ; Spence and Turcotte, 1985 ; Maaloe, 1987 ), and fluid transport during metamorphism...
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Journal Article
Published: 01 March 2010
Journal of the Geological Society (2010) 167 (2): 401-416.
.... We determined best-fit lines to volcano vent centre points by Deming regression analyses (i.e. orthogonal linear regression; Deming, 1943 ) to define volcano alignment trends. Volcanoes in the linear arrays defined here have low standard deviation distances from the best-fit lines of 0.97 km (Flood...
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Journal Article
Journal: GSA Bulletin
Published: 01 April 2000
GSA Bulletin (2000) 112 (4): 550-563.
... in compartments bounded by low-permeability rocks that inhibit pressure equilibration between adjacent regions. Clay-rich strata are most often cited as potential seals ( Deming, 1994 ), but recent studies have proposed that seals may also be formed by diagenetic and hydrothermal minerals ( Ortoleva et al., 1995...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2009
GSA Bulletin (2009) 121 (7-8): 1071-1088.
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Journal Article
Published: 01 November 2012
Vadose Zone Journal (2012) 11 (4): vzj2012.0045.
... Israelachvili J . 1992 . Intermolecular and surface forces. Academic Press , London . Krembs C. Eicken H. Deming J.W. . 2011 . Exopolymer alteration of physical properties of sea ice and implications for ice habitability and biogeochemistry in a warmer Arctic . Proc. Natl. Acad. Sci...
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Journal Article
Published: 01 June 2016
Journal of Sedimentary Research (2016) 86 (6): 683-711.
... readily. To enable K-metasomatism in shales by fluid flow as modelled by Rowan and de Marsily (2001) , the shale permeability might be enhanced by faulting and fracturing as outlined by Deming (1994) , Simmons et al. (2008) , and Ingebritsen and Appold (2012) . Ultimately, a combination of fracture...
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