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Cape Fear Slide Complex

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Series: Geological Society, London, Special Publications
Published: 30 September 2019
DOI: 10.1144/SP477.17
EISBN: 9781786203861
...Abstract Abstract The Cape Fear Slide is one of the largest (>25 000 km 3 ) submarine slope failure complexes on the US Atlantic margin. Here we use a combination of new high-resolution multichannel seismic data (MCS) from the National Science Foundation Geodynamic Processes at Rifting...
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Journal Article
Journal: Geology
Published: 01 July 2013
Geology (2013) 41 (7): 807–810.
... , L24617 , doi:10.1029/2005GL024862 . Hornbach M.J. Lavier L.L. Ruppel C.D. , 2007a , Triggering mechanism and tsunamogenic potential of the Cape Fear Slide complex, US Atlantic margin : Geochemistry Geophysics Geosystems , v. 8 , Q12008 , doi:10.1029/2007GC001722 . Hornbach...
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Journal Article
Journal: Geology
Published: 01 November 2010
Geology (2010) 38 (11): 967–970.
... turbidites : Annual Review of Earth and Planetary Sciences , v. 31 , p. 555 – 577 , doi: 10.1146/annurev.earth.31.100901.141246 . Hornbach M. Lavier L. Ruppel C. , 2007 , Triggering mechanism and tsunamogenic potential of the Cape Fear Slide complex, U.S. Atlantic margin...
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Journal Article
Journal: Geology
Published: 01 January 2004
Geology (2004) 32 (1): 53–56.
...-water temperature that may have caused gas hydrate destabilization, as suggested for the Cape Fear slide ( Popenoe et al., 1991 ) and for the Santa Barbara Basin ( Kennett et al., 2003 ), and (2) an increased continental wetness that may have produced increased sediment deposition ( Maslin et al., 1998...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1974
AAPG Bulletin (1974) 58 (6): 1169–1178.
... is reported to be 315 m thick ( Gill et al. , 1963 , Table 4). Under the outer shelf the Tertiary section off New Jersey is about 1,070 m thick ( Garrison, 1970 ), and deltaic sedimentation apparently continued into the Tertiary. The entire region north of Cape Fear, North Carolina, is a Late Cretaceous...
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Journal Article
Published: 30 October 2019
Seismological Research Letters (2020) 91 (1): 533–540.
... . Hill J. C. Brothers D. S. Hornbach M. J. Sawyer D. E. Shillington D. J. , and Bécel A. 2018 . Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin , Geol. Soc. Lond. Spec. Publ. 477 , SP477‐17 , doi: 10.1144/SP477.17...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1970
AAPG Bulletin (1970) 54 (11): 2216–2218.
... to the present configuration of the Atlantic. In contrast, Precambrian structures generally trend transverse to the present margins of the Atlantic as, for example, the Cape Fear arch and the Reguibat high, the Peninsular arch and the Guinea high; these pairs of opposing structures may have joined prior to drift...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1970
AAPG Bulletin (1970) 54 (1): 44–108.
.... This ridge complex probably is related to the deeper ridge beneath the outer edge of the continental shelf ( Drake et al. , 1959 ); both served as dams behind which sediments accumulated prior to development of the present continental shelf and slope. Off Cape Hatteras and farther south the ridge complex...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1985
AAPG Bulletin (1985) 69 (7): 1133–1144.
... Studies in Geology 7 , p. 193 – 224 . Pilkey , O. H. , I. G. Macintyre , and E. Uchupi , 1971 , Shallow structures : shelf edge of continental margin between Cape Hatteras and Cape Fear, North Carolina: AAPG Bulletin , v. 55 , p. 110 – 115 . Shinn , E. A. , 1977...
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Journal Article
Published: 01 March 2000
Environmental Geosciences (2000) 7 (1): 46–56.
... regions of embayments northeast of Cape Elizabeth, Maine ( Figure 1 ) ( Kelley, 1987 ). Their modern sediment is usually derived from an adjacent, eroding bluff ( Smith, 1990 ) and is typically a very thin deposit overlying glacial sediment which may also crop out on tidal flats. Sediment on the tidal...
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Journal Article
Published: 01 October 1973
Bulletin of the Seismological Society of America (1973) 63 (5): 1841–1846.
... Atlantic Ridge, January 1, 1973, 1lh42m37.5s, 35.5°S, 16.2°W, focal depth about 33 km restricted (ERL). Maglaitude 5.4 (ERL rob),6.0 (ERL Ms). North Island, New Zealand, January 5, 1973, 13h54m27.6s, 39.13°S, 175.18°E, focal depth about 173 km (Wellington). "This earthquake was felt from the East Cape...
Series: Geological Society, London, Special Publications
Published: 30 September 2019
DOI: 10.1144/SP477-2018-190
EISBN: 9781786203861
... caused by some, often distant process. In the Cape Fear Slide complex, the origin of slides has been attributed to hydrate dissociation and salt tectonics (diapirism) owing to the pervasiveness of these features (e.g. Carpenter 1981 ; Cashman & Popenoe 1985 ; Schmuck & Paull 1993 ). On taking...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 2011
AAPG Bulletin (2011) 95 (9): 1495–1524.
.... Several studies have linked slope failure events with the presence of gas hydrates, for example, the Cape Fear slide, North Carolina ( Popenoe et al., 1993 ); the Humboldt slide, northern California ( Field and Barber, 1993 ); the Storegga slide, Norway ( Bouriak et al., 2000 ); and more recently...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2014
AAPG Bulletin (2014) 98 (4): 858–879.
....2011.12.005 . Popenoe P. Schmuck E. A. Dillon W. P. , 1993 , The cape fear landslide: Slope failure associated with salt diapirism and gas hydrate decomposition , in Schwab W. C. Lee H. J. Twichell D. C. , eds. , Submarine landslides: Selected studies in the U.S...
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Journal Article
Published: 01 December 1922
Bulletin of the Seismological Society of America (1922) 12 (4): 199–219.
... through southern Cuba, the Cayman Islands and ~isteriosa Bank. But the topography of the region is much more complex than this description would indicate. While as yet little detailed field work has been done, the principal topographic features may be readily recognized. Charlevoix, P. Pierre-Frangois...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1979
AAPG Bulletin (1979) 63 (7): 1016–1058.
... on the stable flanks of some convergent margin basins (e.g., Thornton arch of Sacramento Valley forearc basin), stable flanks of transform margin basins (e.g., Bakersfield arch of San Joaquin Valley, Fig. 16 ) and in divergent margin basins (e.g., Cape Fear arch of Atlantic seaboard). The Williston basin...
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Journal Article
Published: 01 June 1915
Bulletin of the Seismological Society of America (1915) 5 (2): 71–95.
... is known as Yuno-saki, literally "hot- water cape," it being likely that in old times there existed some hot springs, whose remnant may be the mineral spring referred to in section 2. One of the wells in the village had its water level, usually at a depth of eight or nine feet, raised to within five feet...
Journal Article
Published: 01 October 2002
Journal of Foraminiferal Research (2002) 32 (4): 384–399.
...%) 27.3 cm 2 Hatton-Rockall Basin BENBO Site B (1100 m) Samples from Aug 1997 16 (3.6%) 10 (12.3%) N. Carolina slope (850 m) Off Cape Fear 6 (2.6%) 3 (4.9%) 20 (4.5%) 13 (16.2%) 0–15 cm >300 μm 4–5 ml.l −1 Gooday and others (2001b) Off Cape Lookout...
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Journal Article
Journal: Interpretation
Published: 13 October 2015
Interpretation (2016) 4 (1): SA55–SA71.
... Schmuck , E. A. , and C. K. Paull , 1993 , Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear slide : Geo-Marine Letters , 13 , 145 – 152 , doi: 10.1007/BF01593187 . GMLEDI 1432-1157 Singha , D. K. , and R. Chatterjee...
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Series: Engineering Geology Special Publications
Published: 09 June 2020
DOI: 10.1144/EGSP29.4
EISBN: 9781786204653
... Giles). Composite and complex movements occur where two or more types of displacement occur within the same landslide area ( Fig. 4.16 ). Fig. 4.16. The landslide complex at St Catherine's, Isle of Wight with rockfalls, mud slides (rotational and translational) and mud flows all...
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