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Goose River delta

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A)  <span class="search-highlight">Goose</span> <span class="search-highlight">River</span> <span class="search-highlight">Delta</span> is located in Labrador, Canada at the western end of ...
Published: 01 June 2015
Fig. 7.— A) Goose River Delta is located in Labrador, Canada at the western end of B) Lake Melville, a fjord weakly connected to the Labrador Sea to the east. Youngest inactive lobe as labeled; of the two active, sandy, unvegetated lobes, the southern one is indicated by the box in Part B. C
Journal Article
Published: 01 June 2015
Journal of Sedimentary Research (2015) 85 (6): 699–714.
...Fig. 7.— A) Goose River Delta is located in Labrador, Canada at the western end of B) Lake Melville, a fjord weakly connected to the Labrador Sea to the east. Youngest inactive lobe as labeled; of the two active, sandy, unvegetated lobes, the southern one is indicated by the box in Part B. C...
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Journal Article
Journal: Geology
Published: 01 August 2015
Geology (2015) 43 (8): 719–722.
... to superelevation and continuation of delta lobe avulsions. The field site is the Goose River, Newfoundland-Labrador, Canada, which has experienced steady RSL fall of around 3–4 mm yr –1 in the past 5 k.y. from post-glacial isostatic rebound. Elevation analysis and optically stimulated luminescence dating suggest...
FIGURES
Image
Google Earth image of <span class="search-highlight">Goose</span> <span class="search-highlight">River</span>, Labrador, Canada (53°21′48.32″N, 60°23′1...
Published: 01 August 2015
Figure 1. Google Earth image of Goose River, Labrador, Canada (53°21′48.32″N, 60°23′1.85″W, June 2013). Delta lobes A, B, C, and D are marked by black outline. Delta lobes were defined by their distributary-channel networks and overbank deposits. Inset plot shows spatially averaged elevation
Journal Article
Published: 06 May 2024
Canadian Journal of Earth Sciences (2024) 61 (7): 808–832.
...) , and reached the bank. Fig. 10. Fraser River delta and environs, showing McCall Bank (A), debris flow channels (B), the Foreslope Hills (C), Roberts Bank failure complex (D), large sediment drift (E), pock-marked sediment deposit (F), headland (G), and Burrard Inlet scour troughs, and sediment drifts (H...
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Journal Article
Published: 14 June 2017
Canadian Journal of Earth Sciences (2017) 54 (9): 993–1006.
... with increasing distance from the Churchill River, which drains into Goose Bay, a western extension of Lake Melville. The Churchill River is the greatest source of sediment to the system, but surprisingly, MARs were greatest in western Lake Melville rather than Goose Bay, reflecting the contribution of fine...
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Journal Article
Published: 18 December 2003
Canadian Journal of Earth Sciences (2003) 40 (12): 1755–1766.
..., Hirsch Creek, and Port Simpson on the B.C. mainland were obtained from previous research. Sixty-five underwater grab samples, focusing on fluvial features, river terraces, alluvial fans, and deltas, obtained by H. Josenhans, D. Fedje, and others during a Canadian Coast Guard Ship Vector 1998 cruise from...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1947
AAPG Bulletin (1947) 31 (2): 201–226.
... in Recent if not Historic time. Indian mounds and the natural levees of a former Mississippi River distributary channel were traced by borings under the adjacent marsh. These features indicate that the east side of the Mississippi delta has been tilted toward the east. The tilting occurred after...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1989
AAPG Bulletin (1989) 73 (9): 1103–1116.
... and tractive mechanisms. Prodelta sediments, including fragments of terrestrial organic matter, probably were derived directly from river output, and indirectly from redeposited proximal delta deposits. Muds and silts also were deposited from bottom flows over a broad, dysaerobic, submarine slope southeast...
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Journal Article
Published: 01 February 1983
Journal of the Geological Society (1983) 140 (1): 133–146.
... in the lower Wabash River. J . sediment. Petrol. 46, 579-94. JOHANSSON, C. E. 1965. Structural studies of sedimentary deposits. Geol. Foren. Forhand. Stockholm. 87, 3-61. JOPLING, A. V. 1965. Hydraulic factors controlling the shape of laminae in laboratory deltas. J. sediment. Petrol. 35, KARCZ, 1. 1972...
Journal Article
Published: 19 November 2004
Canadian Journal of Earth Sciences (2004) 41 (11): 1285–1297.
... in the freshwater fauna until the Pliocene ( Howard 1973 ). The bone probably came from a White-fronted Goose that was following the Pacific Flyway between the Yukon Delta, Alaska, and southern California during the fall migration. The modern route seems to be off the western coast of Vancouver Island ( Bellrose...
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Journal Article
Published: 01 December 1987
Bulletin of Canadian Petroleum Geology (1987) 35 (4): 460–468.
... facies domains recognized in the Lower Devonian carbonate succession of Arctic Canada (Smith, 1984). F rom south- east to northwest hese are: i) tidal fiat (Goose Fiord, Vendom Fiord and Disappointment Bay formations), ii) shallow shelf and shelf margin (Blue Fiord Formation) , iii) slope and basin (Cape...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1989
AAPG Bulletin (1989) 73 (4): 431–453.
... Joaquin Rivers in the delta area ( Figure 1 ) ( Safonov, 1968 ). Steeply eastward-dipping Upper Jurassic and Cretaceous strata are exposed along the western margin of the basin and have an aggregate thickness in excess of 50,000 ft (15,000 m) ( Lachenbruch, 1962 ; Hackel, 1966 ). Originally deposited...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2016
GSA Bulletin (2016) 128 (7-8): 1121–1146.
... are dispersed widely across the continental United States ( Perkins et al., 1998 ). The Cassia range in southern Idaho and northern Nevada has a relief of ∼1100 m and is bounded by the Snake River, Oakley, Goose Creek, and Shoshone basins ( Fig. 1 ). It is intensely faulted, and deep valleys (e.g., Rock...
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Journal Article
Published: 27 May 2004
Canadian Journal of Earth Sciences (2004) 41 (5): 587–602.
... asserted that alluvial fans sensu stricto are readily distinguishable from high-gradient gravel bed rivers on the basis of a number of features. Blair and McPherson ( 1994 ) described alluvial fans as being dominated by catastrophic fluid and sediment gravity flows, including debris flows, rock falls...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1930
AAPG Bulletin (1930) 14 (11): 1379–1400.
...Donald C. Barton ABSTRACT A new vista of the petroleum potentialities of the Gulf Coast petroleum province of Texas and Louisiana has been opened by the developments of the past few years. The coastal salt-dome area has been extended eastward to, and across, Mississippi River. The area of good...
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Journal Article
Published: 29 May 2012
Canadian Journal of Earth Sciences (2012) 49 (6): 709–731.
...) reported zircon ages of 90.2 ± 2.7 Ma (tonalite) and 111.0 ± 1.6 Ma (trondhjemite) from deformed plutons exposed near locality MC22-91 of Unruh et al. (2008) . Metaplutonic rocks comprising the syntectonic Hazard Creek complex, Little Goose Creek complex, and Payette River tonalite ( Manduca...
FIGURES
Series: SYMPOSIUM VOLUME
Published: 01 January 1984
DOI: 10.32375/1984-SV1.6
EISBN: 9781733984485
... the “Wild Goose” sands were deposited near sea level. Rejuvenation of streams, possibly by uplift of the adjacent land areas, moved sand deposition to deeper waters and the rejuvenated streams eroded down into the previous delta. As indicated by the presence of graded beds in the basal “gorge” sand...
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Journal Article
Published: 22 August 2023
Canadian Journal of Earth Sciences (2023) 60 (11): 1573–1596.
... (lines): black dashed, outboard margin of the Humber Zone; red and black solid, regional faults. Map sources: van de Poll et al. (1995) , Rivers (1997) , Bourque et al. (2000) , Dickin (2000) , Waldron and van Staal (2001) , Heaman et al. (2002) , Whitmeyer and Karlstrom (2007) , van Staal et al...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 1893–1907.
... into the Powder River basin. The regional setting influenced the depositional nature of the Goose Egg Formation, of which the Opeche Shale is the basal member. A barrier to free circulation of the sea was set up, caused in part by buildup of Phosphoria carbonates on the west, resulting in the deposition of red...
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