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Singleton Swash

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TABLE 2. CALIBRATED AGES AND EFFECTS OF STORM EVENTS IN <span class="search-highlight">SINGLETON</span> <span class="search-highlight">SWASH</span> AND...
Published: 01 September 2003
TABLE 2. CALIBRATED AGES AND EFFECTS OF STORM EVENTS IN SINGLETON SWASH AND THEIR FREQUENCY
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Figure 2. Aerial photograph of <span class="search-highlight">Singleton</span> <span class="search-highlight">Swash</span> showing the positions of the...
Published: 01 September 2003
Figure 2. Aerial photograph of Singleton Swash showing the positions of the vibracore sites discussed in this paper. There are several core locations shown that are not discussed here because the cores contained only massive sand with nondefinable horizons.
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Figure 8. Enlargement of offshore region seaward of <span class="search-highlight">Singleton</span> <span class="search-highlight">Swash</span>. The ar...
Published: 01 September 2003
Figure 8. Enlargement of offshore region seaward of Singleton Swash. The area in the rectangle is Singleton Swash, where the cores were taken; the present shoreline is also emphasized. This map also shows the position of the 3 m contour and illustrates that the shoreline could not have been more
Journal Article
Journal: GSA Bulletin
Published: 01 September 2003
GSA Bulletin (2003) 115 (9): 1027–1039.
...TABLE 2. CALIBRATED AGES AND EFFECTS OF STORM EVENTS IN SINGLETON SWASH AND THEIR FREQUENCY ...
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Figure 1. Regional map with inset of South Carolina showing the positions o...
Published: 01 September 2003
Figure 1. Regional map with inset of South Carolina showing the positions of Price Inlet, Murrells Inlet (near Sandpiper Pond), and Singleton Swash.
Journal Article
Journal: GSA Bulletin
Published: 01 January 2005
GSA Bulletin (2005) 117 (1-2): 254–256.
... and sedimentological evidence, with comparison to other Atlantic coast records : Geological Society of America Bulletin , 115 . 1027 – 1039 doi: 10.1130/B25011.1. Hippensteel and Martin suggest that Singleton Swash is a tidal inlet—certainly it is—with large sand bars throughout its length, which...
Journal Article
Journal: GSA Bulletin
Published: 01 January 2005
GSA Bulletin (2005) 117 (1-2): 250–253.
.... Moreover, given the potential for physical reworking at Singleton Swash (cf. above), the calcareous foraminiferal assemblages of Scott et al. (2003) may have originated not only from deposition by tidal currents but also from death assemblages derived from populations living in the marsh. Obviously...
Journal Article
Published: 01 July 2004
Journal of Foraminiferal Research (2004) 34 (3): 243–244.
... on the South Carolina coast based on micropaleontological and sedimentological evidence, with comparison to other Atlantic Coast records.— GSA Bulletin , v. 115 , no. 9, 2003 , p. 1027 –1039, 9 figures, 2 tables.—“Singleton Swash on the South Carolina coast provides an extended record of storm events...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2008
GeoArabia (2008) 13 (3): 39–120.
.... The upper D member in Wadi Mi’Aidin shows several units of grainy swash zone or beach facies ( Figures 28c and d) that are anomalously thick (nearly 10 m thick, much thicker than a single beach sequence). The anomalous thickness implies that the shoreline must have stayed close to this location, aggrading...
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Journal Article
Published: 01 April 2005
Journal of Foraminiferal Research (2005) 35 (2): 130–147.
... fits with the overall degradation in all subsurface intervals observed in a study of hurricane records from Singleton Swash, South Carolina ( Scott and others, 2003b ), except that the older parts of those cores were in a brackish sequence (salinities probably <10‰) and also far below the impact...
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Journal Article
Published: 27 March 2020
Journal of Sedimentary Research (2020) 90 (3): 313–335.
..., possibly in response to breaking waves (cf. Clifton 1976 ). This latter interpretation of swash–backwash processes is supported by localized overprinting of planar-parallel-laminated sandstones by rootlets, which indicate subaerial exposure. The trace-fossil assemblage in Facies Association 3 constitutes...
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Series: GSA Field Guides
Published: 04 September 2019
DOI: 10.1130/2019.0055(03)
EISBN: 9780813756554
... fault system in the lower Colorado River corridor as compared to the now-active Eastern California Shear Zone (an inboard part of the plate boundary) suggests that any late Miocene shear in the lower Colorado River corridor may be subtly distributed and/or not yet recognized ( Singleton, 2015 ; Bennett...
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