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Gros Morne

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Journal Article
Published: 23 January 2017
Canadian Journal of Earth Sciences (2017) 54 (3): 257–262.
...Liam S. Morrissey; Penny L. Morrill Abstract We measured CO 2 , CH 4 , and N 2 O gas fluxes from a pool of ultra-basic water discharging from serpentinized rock in Winterhouse Canyon, Gros Morne, Newfoundland. The flux of CH 4 released and CO 2 sequestered were calculated to be 4.6 × 10 −7 and 1.9...
FIGURES
Journal Article
Published: 20 July 2006
Canadian Journal of Earth Sciences (2007) 44 (6): 819–834.
...Gerald Osborn; Ian Spooner; John Gosse; Doug Clark Abstract Controversy persists in western Newfoundland regarding Pleistocene, particularly Late Wisconsinan, glacial ice volumes. Independently, a set of alpine glacial deposits on the flanks of the Tablelands in Gros Morne National Park has...
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Digital elevation model (10 m resolution) of the Tablelands in Gros Morne National Park (GMNP). BBB, Berry Barren Pond; DB, Dry Brook; DP, Devil’s Punchbowl; TRBP, Trout River Big Pond; TRSP, Trout River Small Pond; UC, unnamed cirque; WB, Winterhouse Brook.
Published: 20 July 2006
Fig. 2. Digital elevation model (10 m resolution) of the Tablelands in Gros Morne National Park (GMNP). BBB, Berry Barren Pond; DB, Dry Brook; DP, Devil’s Punchbowl; TRBP, Trout River Big Pond; TRSP, Trout River Small Pond; UC, unnamed cirque; WB, Winterhouse Brook.
Image
Triplicatella from the Forteau Formation of Gros Morne, Newfoundland. 4A–4C.Triplicatella peltata n. sp. (A, B) NFM F-453, view from above and from dorsal edge. (C)  NFM F-454, sample ICS 1421, view from above. 4D–4F.Triplicatella? sp., from 12 km east of Rocky Harbour. (D)  NFM F-455, view from above. (E, F) NFM F-456, view from above and from edge of fragment. All except C from sample JSP1982-01. Scale bar = 0.5 mm.
Published: 09 November 2004
Fig. 4. Triplicatella from the Forteau Formation of Gros Morne, Newfoundland. 4A–4C. Triplicatella peltata n. sp. (A, B) NFM F-453, view from above and from dorsal edge. (C)  NFM F-454, sample ICS 1421, view from above. 4D–4F. Triplicatella ? sp., from 12 km east of Rocky Harbour. (D)  NFM
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Photographs of Pliocene shelf-deltaic deposits of Gros Morne Formation of the Columbus Basin outcropping along the southeast coast of Trinidad show soft-sediment deformation, including (a) large channel scour truncating underlying fine-grained sandstone, siltstone, and claystones deposited in a shelf deltaic setting. The channel scours into structurally tilted sediments. Its irregular base is filled with large rectangular blocks, which were semicohesive when deposited and are composed of the substrate material. The remainder of the channel is filled with alternating wavy-bedded silty sands and shales. (b) Flame structure, characteristic of these rapidly deposited sediments. Location of photos shown in Figure 4.
Published: 01 December 2000
Figure 9 Photographs of Pliocene shelf-deltaic deposits of Gros Morne Formation of the Columbus Basin outcropping along the southeast coast of Trinidad show soft-sediment deformation, including (a) large channel scour truncating underlying fine-grained sandstone, siltstone, and claystones
Image
Photographs of Pliocene shelf-deltaic deposits of Gros Morne Formation of the Columbus Basin outcropping along the southeast coast of Trinidad show soft-sediment deformation, including (a) large channel scour truncating underlying fine-grained sandstone, siltstone, and claystones deposited in a shelf deltaic setting. The channel scours into structurally tilted sediments. Its irregular base is filled with large rectangular blocks, which were semicohesive when deposited and are composed of the substrate material. The remainder of the channel is filled with alternating wavy-bedded silty sands and shales. (b) Flame structure, characteristic of these rapidly deposited sediments. Location of photos shown in Figure 4.
Published: 01 December 2000
Figure 9 Photographs of Pliocene shelf-deltaic deposits of Gros Morne Formation of the Columbus Basin outcropping along the southeast coast of Trinidad show soft-sediment deformation, including (a) large channel scour truncating underlying fine-grained sandstone, siltstone, and claystones
Image
—Structural map, top of Cruse–Gros Morne–Manzanilla Formations.
Published: 01 September 1976
Fig. 9 —Structural map, top of Cruse–Gros Morne–Manzanilla Formations.
Image
—Structural map, top of Cruse–Gros Morne–Manzanilla Formations, showing Northern High structural province.
Published: 01 September 1976
Fig. 10 —Structural map, top of Cruse–Gros Morne–Manzanilla Formations, showing Northern High structural province.
Image
—Structural map, top of Cruse–Gros Morne–Manzanilla Formations, showing Diapiric Fold structural province.
Published: 01 September 1976
Fig. 11 —Structural map, top of Cruse–Gros Morne–Manzanilla Formations, showing Diapiric Fold structural province.
Image
—Structural map, top of Cruse–Gros Morne–Manzanilla, showing Block-Fault structural province.
Published: 01 September 1976
Fig. 12 —Structural map, top of Cruse–Gros Morne–Manzanilla, showing Block-Fault structural province.
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—Structural map, top of Cruse–Gros Morne–Manzanilla, showing Monoclinal structural province.
Published: 01 September 1976
Fig. 13 —Structural map, top of Cruse–Gros Morne–Manzanilla, showing Monoclinal structural province.
Journal Article
Published: 01 November 1998
Canadian Journal of Earth Sciences (1998) 35 (11): 1307–1322.
... to the allochthonous Cow Head Group contain abundant acritarchs and Gloeocapsamorpha sp. These rocks are marginally mature to mature within Gros Morne National Park; maturation levels increase farther north (e.g., Parsons Pond), becoming overmature somewhere south of Port au Choix. It is concluded that neither...
Journal Article
Published: 01 June 1995
Bulletin of Canadian Petroleum Geology (1995) 43 (2): 187–213.
... de Gros Morne au nord et l’évolution croissante de l’ouest vers l’est dans la région de Port-au-Port. Les carbonates d’âge Cambro-Ordovicien du plateau/plate-forme dolomitisé et les clastiques en eau plus profonde offrent une abondance de bonnes possibilités de faciès réservoirs. La déformation...
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Uncertainties herein are given at the 2σ level. A: 40Ar/39Ar spectra for BT22-sample from “Gros Morne” dacite dome of Deshaies; B: Inverse isochron for BT22-sample from “Gros Morne” dacite dome of Deshaies. MSWD = Mean Square Weighted Deviation.
Published: 13 September 2019
Fig. 9 Uncertainties herein are given at the 2 σ level. A: 40 Ar/ 39 Ar spectra for BT22-sample from “Gros Morne” dacite dome of Deshaies; B: Inverse isochron for BT22-sample from “Gros Morne” dacite dome of Deshaies. MSWD = Mean Square Weighted Deviation.
Journal Article
Published: 13 September 2019
Bulletin de la Société Géologique de France (2019) 190 (1): 10.
...Fig. 9 Uncertainties herein are given at the 2 σ level. A: 40 Ar/ 39 Ar spectra for BT22-sample from “Gros Morne” dacite dome of Deshaies; B: Inverse isochron for BT22-sample from “Gros Morne” dacite dome of Deshaies. MSWD = Mean Square Weighted Deviation. ...
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Journal Article
Published: 30 January 2012
Canadian Journal of Earth Sciences (2012) 49 (1): 59–90.
...Svend Stouge Abstract Middle Ordovician (late Dapingian–Darriwilian) conodonts from the Shallow Bay and Green Point formations, Cow Head Group, and the Lower Head Formation are recorded from three sections in Gros Morne National Park. The collection was investigated to clarify local age...
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Journal Article
Published: 01 January 2011
Journal of Paleontology (2011) 85 (1): 156–177.
...Mun-Zu Won; William J. Iams Abstract Radiolarians have been recovered from lowermost Arenigian rocks of the Cow Head Group in Gros Morne National Park, Newfoundland. Two new faunal assemblages include eight families, 13 genera, and 25 species. Among these, the family Neoaspiculumidae, the genus...
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Journal Article
Published: 01 May 2005
Journal of Paleontology (2005) 79 (3): 433–459.
... assemblages are from Green Point, Martin Point, Broom Point North and South, and St. Paul's Inlet in Gros Morne National Park. Latest Cambrian faunas were also recovered from Green Point and St. Paul's Inlet, but are extremely low in both abundance and diversity. The radiolarian faunas include five families...
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Journal Article
Published: 01 January 2002
Journal of Paleontology (2002) 76 (1): 1–33.
..., one from a stratum at Martin Point, and three from strata at Broom Point South in Gros Morne National Park. The faunas contain nine genera, five of which are new, and 33 species, all but two of which are new. The five new genera are Curvechidnina , Grosmorneus , Pararcheoentactinia , Ramuspiculum...
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Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5405-4.451
EISBN: 9780813754116
... Location The Bay of Islands Complex forms a discontinuous north easterly trending belt of mafic-ultramafic massifs approximately 60 mi ( 100 km) long and 15 mi (25 km) wide on the west coast of Newfoundland (Fig. 1). The northernmost of the massifs, Table Mountain, lies within the Gros Morne...