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Hungry Bay

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FIGURE 5. Montage of trackway views in <b>Hungry</b> <b>Bay</b> Formation at Charles Isla...
in > PALAIOS
Published: 01 July 2011
FIGURE 5. Montage of trackway views in Hungry Bay Formation at Charles Island, Bermuda, St. Georges Parish, south side (mouth) of Castle Harbour located at 32° 20.312′ N; 64° 40.306′ W. A) exposure on north side of Charles Island showing eolianite slab with the bird trackways. Oval indicates
Image
FIGURE 8. Preservation of a forest of trees at <b>Hungry</b> <b>Bay</b>. A) photograph sh...
in > PALAIOS
Published: 01 July 2011
FIGURE 8. Preservation of a forest of trees at Hungry Bay. A) photograph showing several hollow and refilled casts of suspected buried Sabal bermudana forest. B) Sketch interpreting the above photograph showing standing and fallen trunks and a large number of frond molds and rhizomorphs.
Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0024(15)
EISBN: 9780813756240
... (Fig. 1 .3). “The presence of glacial lake sediments above the subcontinental drainage divide (between Superior and Agassiz basins) northwest of Thunder Bay, Ontario records a paleo lake at elevations higher than previously mapped” (Fisher et al., 2005 , p. 542). Fisher et al. ( 2005 , p. 542) go...
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Journal Article
Journal: Economic Geology
Published: 01 June 2012
Economic Geology (2012) 107 (4): 599–644.
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Journal Article
Published: 18 November 2011
Canadian Journal of Earth Sciences (2012) 49 (1): 111–127.
... ; Dilek 2003 ). The Moreton’s Harbour Group is located in Notre Dame Bay and extends along strike for 40 km from Fortune Harbour Peninsula to New World Island ( Fig. 2 ). The geology of the Moreton’s Harbour Group thus far has been based primarily on mapping that has been focussed on Fortune Harbour...
FIGURES
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FIGURE 3. Stratigraphic correlation of study sites along the south shore of...
in > PALAIOS
Published: 01 July 2011
FIGURE 3. Stratigraphic correlation of study sites along the south shore of Bermuda. The Hungry Bay Formation (HBF; former Pembroke Member) is identified across the South Shore sections with thick dashed lines. Site abbreviations are defined in Figure 1 . Stratigraphic abbreviations: SG.s  =  St
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FIGURE 7. Plant impressions and modern counterparts in rocks correlated wit...
in > PALAIOS
Published: 01 July 2011
FIGURE 7. Plant impressions and modern counterparts in rocks correlated with the Hungry Bay Formation of mid last interglacial age (MIS 5c). A) corrugated impression of a frond with arching petiole at Southcourt Avenue (Feb 2005 photo; hand for scale); B and D) The modern endemic palm Sabal
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FIGURE 1. Located 1040 km ESE of Cape Hatteras, North Carolina (inset), Ber...
in > PALAIOS
Published: 01 July 2011
FIGURE 1. Located 1040 km ESE of Cape Hatteras, North Carolina (inset), Bermuda has a current land area of 56 km 2 . Study sites along the South Shore of Bermuda (individual sections in Fig. 3 ) are as follows: GB  =  Grape Bay; SC  =  Southcourt Ave., HB  =  Hungry Bay, AS  =  Ariel Sands; RB
Journal Article
Journal: Palynology
Published: 22 December 2017
Palynology (2017) 41 (0): 158–177.
...Reed Wicander; Geoffrey Playford ABSTRACT An abundant, diverse, and moderately well-preserved assemblage of organic-walled microphytoplankton is reported from two exposures of the Middle Devonian (Givetian) Gravel Point Formation at Little Traverse Bay, Michigan. The palynoflora consists of 13...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2009
GSA Bulletin (2009) 121 (7-8): 1089–1107.
... estimates of extension rates and new information on Holocene faulting, and places Tahoe Basin deformation into the larger context of Walker Lane and Basin and Range tectonics. Measured offset marker surfaces include submerged wave-cut paleo terraces of Tioga age (19.2 ± 1.8 ka), McKinney Bay slide deposits...
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Journal Article
Published: 21 December 2011
Canadian Journal of Earth Sciences (2012) 49 (1): 147–165.
... Williams et al. 1988 ; van Staal et al. 1998 ). Location of Fig. 2 is indicated. RIL, Red Indian Line; HMT, Hungry Mountain Thrust. In Notre Dame Bay ( Fig. 2 ), the Red Indian Line separates the peri-Laurentian Middle Ordovician Robert’s Arm Group ( Bostock 1988 ) from the peri-Gondwanan Early...
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The progression of facies development in the (1) ravinement infill facies a...
Published: 01 November 2015
assemblages may be preserved together at Hungry Bay west and Devonshire Bay, although there is insufficient exposure to demonstrate this. The ravinement infill facies assemblage is thought to have developed concomitant with early flooding of the Bermuda Platform at the beginning of an interglacial period
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FIGURE 9. Successive stages of evolution of mold and cast tree forms. A) St...
in > PALAIOS
Published: 01 July 2011
FIGURE 9. Successive stages of evolution of mold and cast tree forms. A) Stage I: unfilled mold of palmetto in 100 ka eolianite at Hungry Bay, Bermuda. B) Stage II: mostly filled cast of a large tree mold and cast in Nassau, Bahamas, 125 ka dune (note large void and rhizomorphs at top of cast). C
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Belmont Formation facies assemblage as seen in a shore-normal exposure at D...
Published: 01 November 2015
lag. Exposure of nearshore deposits as sea level fell provided a source of sand for an advancing dune (T), which overstepped the foredune. Note the absence of subtidal shoreface deposits above present sea level at this locality, unlike at Hungry Bay ( Fig. 4 ). Also, the truncation/deflation surface
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Belmont Formation facies assemblage as seen in a shore-normal exposure at H...
Published: 01 November 2015
Figure 4. Belmont Formation facies assemblage as seen in a shore-normal exposure at Hungry Bay west. A weakly cemented dune from an earlier depositional cycle (T) is transgressed by a readvancing sea. Prograded foreshore and shoreface deposits (P) are fronted on the seaward side
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Examples of Bermuda’s coastal facies and their associations. (A) A ravineme...
Published: 01 November 2015
) The Belmont Formation at Devonshire Bay featuring Lapl and Lal facies with an intervening bounding surface. Interpretation: Truncated reflective beach-face deposits superposed by a foredune. (C) The Belmont Formation at Hungry Bay east, featuring Lapl, Trm, and Flp facies with intervening bounding surfaces
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Simplified geology of the Baie Verte Peninsula with major tectonostratigrap...
Published: 01 September 2017
accretionary tract, BPS = Burlington plutonic suite, BVBL = Baie Verte-Brompton line, BVL = Baie Verte line, CB = Cape Brulé, DBL = Dog Bay line, DF = Dover fault, DG = Dunamagon Granite, GRUB = Gander River ultramafic belt, HMT = Hungry Mountain thrust, RIL = Red Indian line, TPP = Trap Pond pluton.
Journal Article
Journal: PALAIOS
Published: 01 July 2011
PALAIOS (2011) 26 (7): 394–405.
...FIGURE 5. Montage of trackway views in Hungry Bay Formation at Charles Island, Bermuda, St. Georges Parish, south side (mouth) of Castle Harbour located at 32° 20.312′ N; 64° 40.306′ W. A) exposure on north side of Charles Island showing eolianite slab with the bird trackways. Oval indicates...
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Geology of Newfoundland Appalachians, modified from  van Staal  et al.  (20...
Published: 21 March 2017
Fault; DBL, Dog Bay Line; DC, Duder Complex; DF, Dover Fault; GBF, Green Bay Fault; GHF, Gunflap Hills Fault; GRUB, Gander River Ultrabasic Belt; HBF, Hermitage Bay Fault, HMT, Hungry Mountain thrust; HR, Harry's River; IIG, Indian Islands Group; LB, Loon Bay pluton; LCF, Lobster Cove Fault; LPG, La
Journal Article
Journal: GSA Bulletin
Published: 01 November 2015
GSA Bulletin (2015) 127 (11-12): 1645–1665.
... assemblages may be preserved together at Hungry Bay west and Devonshire Bay, although there is insufficient exposure to demonstrate this. The ravinement infill facies assemblage is thought to have developed concomitant with early flooding of the Bermuda Platform at the beginning of an interglacial period...
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