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Lamb Creek

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Figure 4. Lamb Creek debris flood of September 2004. (a) An erosional reach of Gold Hill Creek channel, showing glacial till exposed after flood has stripped away overlying sediment. (b) Debris-flood deposits lower down Gold Hill Creek channel. Photos by: Doug Nicol, BC Forest Service.
Published: 01 November 2009
Figure 4. Lamb Creek debris flood of September 2004. (a) An erosional reach of Gold Hill Creek channel, showing glacial till exposed after flood has stripped away overlying sediment. (b) Debris-flood deposits lower down Gold Hill Creek channel. Photos by: Doug Nicol, BC Forest Service.
Journal Article
Published: 01 November 2009
Environmental & Engineering Geoscience (2009) 15 (4): 217–234.
...Figure 4. Lamb Creek debris flood of September 2004. (a) An erosional reach of Gold Hill Creek channel, showing glacial till exposed after flood has stripped away overlying sediment. (b) Debris-flood deposits lower down Gold Hill Creek channel. Photos by: Doug Nicol, BC Forest Service. ...
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Figure 2. Maps showing BARC burn severity, watersheds, and post-wildfire events for portions of the five fires. Solid-color thick lines indicate debris-flow paths, dashed lines indicate debris-flood paths, and diamond symbols indicate landslides. Shading indicate burn severity: red  =  high; orange  =  moderate; green  =  low; white  =  unburned. Watershed boundaries are outlined; contour interval is 100 m. (a) Okanagan Mountain Park fire; (b) Cedar Hills fire; (c) Kuskonook fire; (d) Lamb Creek fire; (e) Ingersoll fire.
Published: 01 November 2009
 =  moderate; green  =  low; white  =  unburned. Watershed boundaries are outlined; contour interval is 100 m. (a) Okanagan Mountain Park fire; (b) Cedar Hills fire; (c) Kuskonook fire; (d) Lamb Creek fire; (e) Ingersoll fire.
Journal Article
Published: 01 January 2016
Journal of Paleontology (2016) 90 (1): 133–146.
...Albert Prieto-Márquez; Susana Gutarra Abstract The Careless Creek Quarry (CCQ) is a multitaxic bonebed in the Campanian Judith River Formation of south-central Montana (USA) that produced a diverse assemblage of vertebrates, including several dinosaurian clades. We describe the morphology...
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—Map of southeastern Kansas and margin of northeastern Oklahoma, showing oil pools and classes of oil in Arbuckle limestone for which analyses are available. Numbers beside pools indicate classes of oil shown in Table III: 1, Graham; 2, Slick-Carson; 3, Winfield; 4, Hittle; 5, Porter; 6, Moline; 7, Lamb; 8, Clemmer; 9, Bellaire; 10, Coffeyville; 11, Edna; 12, Chetopa; 13, Pond Creek.
Published: 01 January 1947
, Moline; 7, Lamb; 8, Clemmer; 9, Bellaire; 10, Coffeyville; 11, Edna; 12, Chetopa; 13, Pond Creek.
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Map of geologic features in the northern and central Basin and Range Province, western USA. The Golconda and Roberts Mountains thrusts and Antler foreland basin are from Dickinson [171], and the Sevier fold-and-thrust belt is from DeCelles [5]. The Cretaceous Sierra arc is after Van Buer and Miller [172]. Paleogene basins in the Sevier hinterland are from Haynes [144], Lamb et al. [124], Smith et al. [167], and this study. Their timing of sedimentary deposition is from Dubiel et al. [147], Rahl et al. [14], McGrew et al. [15], Druschke et al. [21], Lund Snee et al. [17], Lamb et al. [124], Canada et al. [11], Lund Snee and Miller [3], and this study. The late Paleocene shoreline is after Reid [173] and Lechler and Niemi [23]. Middle Cenozoic magmatic isochrons are based on ages from this and other studies [3, 38-40, 123, 126, 174] and from NAVDAT (www.navdat.org). Basin and Range Province and subdomain boundaries are modified from Sonder and Jones [175] and Dickinson [176] to more closely follow patterns of physiography, faulting, and gravity anomalies. Metamorphic core complex outlines are after Chapman et al. [177]. ARG, Albion–Raft River–Grouse Creek; B, Black Mountains; F, Funeral Mountains; REH, Ruby–East Humboldt; S, Snake Range.
Published: 29 March 2024
Buer and Miller [ 172 ]. Paleogene basins in the Sevier hinterland are from Haynes [ 144 ], Lamb et al. [ 124 ], Smith et al. [ 167 ], and this study. Their timing of sedimentary deposition is from Dubiel et al. [ 147 ], Rahl et al. [ 14 ], McGrew et al. [ 15 ], Druschke et al. [ 21 ], Lund Snee et al
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Profile N20°E looking west at present elevations of glacial lake shorelines (grey) (after Mirynech 1962) and water and sediment columns (black lines and patterns) in small lake basins (after Terasmae 1980) studied in the region north of central and eastern Lake Ontario. The Bell Creek site of buried logs in the lowland southeast of Lake Ontario is also shown. Lambs Pond, Long Pond, and Bell Creek are projected to the profile along isobases in the Lake Iroquois map of Bird and Kozlowski (2016). Small black filled circles are intersections of isobases drawn on the Iroquois and Belleville shores; the other shores were indicated as vertical distances below the shore immediately above (Mirynech 1962). The thicknesses of the grey curves represent the range of elevations of each of the Iroquois and post-Iroquois shorelines in the Trenton, Ontario, area, mainly from Mirynech (1962). The geological material, where known, underlying each small lake sequence is stated below the sequence diagrams from Terasmae (1980) and Rayburn et al. (2007) for Long Pond. Solid black triangle beneath the x axis denotes the location of Trenton, Ontario, on the profile. Adapted mainly from Mirynech (1962) and Terasmae (1980).
Published: 24 July 2019
site of buried logs in the lowland southeast of Lake Ontario is also shown. Lambs Pond, Long Pond, and Bell Creek are projected to the profile along isobases in the Lake Iroquois map of Bird and Kozlowski (2016) . Small black filled circles are intersections of isobases drawn on the Iroquois
Journal Article
Journal: GSA Bulletin
Published: 05 April 2024
GSA Bulletin (2024) 136 (9-10): 4398–4410.
... of a broad knickpoint or cataract complex several km in length ( Hanson, 1970 ; Larsen and Lamb, 2016 ). Whether Wilson Creek was eroded by a prominent knickpoint is unclear, but we assume that headward incision by plucking played a role in its incision for the purpose of calculating cataract retreat rates...
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The Saddle Mountain fault zone, shown in regional tectonic context. (a) OxCal model (version 4.2.2; Bronk Ramsey, 2009a) of the timing of the most recent earthquakes along the Seattle fault zone, the Tacoma fault zone, the Olympia fault zone, and the Saddle Mountain fault zone. Radiocarbon ages are shown for the Seattle fault zone (SF; Atwater, 1999), the Tacoma fault zone (TF; Sherrod et al., 2004), the Olympia fault zone (OF; Sherrod, 2001); and the Saddle Mountain fault zone (SMFZ; data presented in this paper and from Witter et al., 2008). Age ranges are 2σ; m shows the median value for probability density function, a circle indicates the mean value, and a cross shows the median value. The calibrated maximum ages are shown for the Canyon River fault (CF; Walsh and Logan, 2007); Frigid Creek fault (FCF; Blakely et al., 2009); and Lake Creek‐Boundary Creek fault (Nelson et al., 2007). (b) Regional model of the Saddle Mountain fault zone (SFMZ) as a western boundary fault. The location of possible faults that connect SF to SMFZ, interpreted from potential field and seismic data, are shown as gray, dotted lines (Blakely et al., 2009; Lamb et al., 2012). Location of folded terraces in the Big Beef Creek (BB) are from Tabor et al. (2011). Regions of relative uplift and subsidence based on gravity data are shown by stripes and dots, respectively. The box around the SMZF indicates the area of (c). (The figure is modified from Blakely et al., 2009). (c) Map view of the SMFZ and a schematic cross section of the resulting positive flower structure. The model generally is based on Woodcock and Rickards (2003).
Published: 13 January 2015
Creek fault ( Nelson et al. , 2007 ). (b) Regional model of the Saddle Mountain fault zone (SFMZ) as a western boundary fault. The location of possible faults that connect SF to SMFZ, interpreted from potential field and seismic data, are shown as gray, dotted lines ( Blakely et al. , 2009 ; Lamb et
Journal Article
Journal: GSA Bulletin
Published: 01 March 2017
GSA Bulletin (2017) 129 (3-4): 500–512.
... location of photos in Figure 4 . Channel flow is from east-northeast to west-southwest. To predict incision rates along White Branch Creek, we used a one-dimensional (1-D) mechanistic model of bedrock abrasion by total sediment load ( Lamb et al., 2008b ). Sediment supply has a strong influence...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1955
AAPG Bulletin (1955) 39 (12): 2515–2524.
... is present at or near the lithologic change at each locality. On Coal Creek near Cedar City, the change from Chinle to Dinosaur Canyon lithologic features is clearly visible, and the contact is marked by a disconformity at the top of a calcareous layer containing shale fragments. Judged by the description...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2015
GSA Bulletin (2015) 127 (3-4): 539–559.
... and Dietrich, 2004 ), extensive fluting of bedrock surfaces in lower Big Tujunga Creek suggests high erosion rates within the suspension regime ( Hancock et al., 1998 ; Whipple et al., 2000 ; Hartshorn et al., 2002 ; Lamb et al., 2008a ; Scheingross et al., 2014 ). Last, the waterfalls on the main stem...
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Journal Article
Published: 01 April 2020
Earth Sciences History (2020) 39 (1): 184–218.
... and Jenkins, 2007 ). The BNABC disbanded for the winter and resumed their expedition from Wood End the following year. In early July of 1874, the BNABC made their way 20 miles (32 km) southwest of Wood Mountain, and entered an area of badlands on Rock (Rocky) Creek that now sits within the East Block...
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Journal Article
Published: 05 August 2015
Canadian Journal of Earth Sciences (2015) 52 (8): 557–568.
... near Johnston Creek in Banff National Park ( Lambe 1916 , plate III). Gardiner (1966) referred this species to the genus Pteronisculus but Schaeffer and Mangus (1976) questioned its specific status. Although some specimens from Wapiti Lake have also been referred to the genus Pteronisculus...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2016
GSA Bulletin (2016) 128 (7-8): 1228–1248.
...Dirk Scherler; Michael P. Lamb; Edward J. Rhodes; Jean-Philippe Avouac Abstract Fill terraces along rivers represent the legacy of aggradation periods that are most commonly attributed to climate change. In the North Fork of the San Gabriel River, an arid bedrock landscape in the San Gabriel...
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Journal Article
Journal: Geosphere
Published: 01 December 2014
Geosphere (2014) 10 (6): 1123–1138.
... north of Lake Mead. U-Pb age spectra of detrital zircons from Miocene–Pliocene basin fill of the Muddy Creek Formation in the Virgin River depression preclude any paleo–Colorado River sand in Muddy Creek exposures but fail to show that a Miocene paleo–Colorado River never flowed into the Virgin River...
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Journal Article
Published: 01 July 2006
Journal of Paleontology (2006) 80 (4): 672–683.
... scale; vcf, ventral caudal fulcrum; vlps, ventrolateral caudal peduncle scute; vmps, ventromedial caudal peduncle scute Judith River Group (Oldman Formation?), Red Deer River, Alberta, Canada; late Cretaceous; fresh and brackish water ( Osborn, 1902 ; Lambe, 1902 ; L. S. Russell, 1964...
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Journal Article
Published: 01 September 2005
Journal of Paleontology (2005) 79 (5): 997–1001.
... ). Virtually all of the common major groups of theropods and ornithopods typical of the Late Cretaceous of northern North America are present. Most of the skeletal remains are found in rocks assigned to the Prince Creek Formation of the Colville Group ( Detterman et al., 1963 , 1975 ; Phillips, 1990...
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Journal Article
Published: 19 February 2024
Journal of Sedimentary Research (2024) 94 (1): 103–124.
.... Many of the basins in southern Nevada that contain deposits of the Muddy Creek Formation were closed fluvio-lacustrine systems during the latest Miocene and into the Pliocene. They were subsequently integrated into the regional Colorado River system. Lacustrine deposits of the Muddy Creek Formation...
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Journal Article
Journal: Geology
Published: 22 February 2021
Geology (2021) 49 (6): 682.
...Alexander R. Beer; Michael P. Lamb Abstract River incision into bedrock drives landscape evolution and couples surface changes to climate and tectonics in uplands. Mechanistic bedrock erosion modeling has focused on plucking—the hydraulic removal of large loosened rock fragments—and on abrasion...
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