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Grape Bay

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FIGURE 6. Corrugations typical of molds of palmetto fronds at Grape Bay, Bermuda. The hammer handle in the lower left of the photo is 3.5 cm wide.
Published: 01 July 2011
FIGURE 6. Corrugations typical of molds of palmetto fronds at Grape Bay, Bermuda. The hammer handle in the lower left of the photo is 3.5 cm wide.
Journal Article
Published: 01 January 1996
Journal of Sedimentary Research (1996) 66 (1): 243–258.
... the diagenetic environments involved. Diagenetic features of multiple pore-water changes (herein termed early-diagenetic oscillation) depend on whether substrates were loosely or firmly cemented. (1) In loosely cemented beach sands (Belmont Group, Grape Bay) truncated layers of Mg-bearing low-Mg calcite covered...
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FIGURE 1. Located 1040 km ESE of Cape Hatteras, North Carolina (inset), Bermuda has a current land area of 56 km2. 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  =  Rocky Bay (type section), SH  =  Saucos Hill, SP  =  Spittal Pond, and CH  =  Charles Island.
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
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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. Georges soil; S  =  Southampton Formation; HBF  =  Hungry Bay Formation; Hp  =  Harrington protosol; Dm  =  Devonshire Member (marine); De  =  Devonshire Member (eolianite); GBm  =  Grape Bay Member (marine).
Published: 01 July 2011
. Georges soil; S  =  Southampton Formation; HBF  =  Hungry Bay Formation; Hp  =  Harrington protosol; Dm  =  Devonshire Member (marine); De  =  Devonshire Member (eolianite); GBm  =  Grape Bay Member (marine).
Journal Article
Journal: PALAIOS
Published: 01 July 2011
PALAIOS (2011) 26 (7): 394–405.
...FIGURE 6. Corrugations typical of molds of palmetto fronds at Grape Bay, Bermuda. The hammer handle in the lower left of the photo is 3.5 cm wide. ...
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Maps showing known and inferred 1855 earthquake features with respect to the position of ‘Lyell's fault' (locality F), NW corner of Palliser Bay (modified after Grapes & Downes 1997, fig. 12). (See Fig. 1 for location.) The ‘Mukamuka Fault' and another north–south-trending fault to the west were mapped as unnamed faults by Begg & Mazengarb (1996). The fine dashed line shown on the inset map is the line of the 1855 uplifted beach surveyed in 1868–69 from Waimarama (Palliser Bay) to west of Baring Head. The greatest amount of 1855 uplift of c. 6 m was localized where the axial trace of the Rimutaka anticline intersects the coast as shown (see also Fig. 6). The bold dashed line represents the probable submarine extension of the Wharekauahau Thrust (on-land bold continuous line) (after Barnes 2005; see also Fig. 1).
Published: 01 January 2010
Fig. 4. Maps showing known and inferred 1855 earthquake features with respect to the position of ‘Lyell's fault' (locality F ), NW corner of Palliser Bay (modified after Grapes & Downes 1997 , fig. 12). (See Fig. 1 for location.) The ‘Mukamuka Fault' and another north–south-trending fault
Journal Article
Published: 01 January 2010
Journal of the Geological Society (2010) 167 (1): 35–47.
...Fig. 4. Maps showing known and inferred 1855 earthquake features with respect to the position of ‘Lyell's fault' (locality F ), NW corner of Palliser Bay (modified after Grapes & Downes 1997 , fig. 12). (See Fig. 1 for location.) The ‘Mukamuka Fault' and another north–south-trending fault...
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Map of the central part of New Zealand (Cook Strait area) showing place names mentioned by Lyell (1868), the surface trace of the 1855 fault rupture and localities (1–6) where measurements of uplift and subsidence relative to sea level were reported by Edward Roberts; 1, Mukamuka Rocks; 2, Pencarrow Head; 3, Balley Rock; 4, Porirua Harbour; 5, Wainui; 6, Lower Wairau Valley. Fault displacement localities described in the text are shown as BM (Begg & Mazengarb 1996); C (Crawford 1865): J (Jackson; Grapes & Downes 1999); PB (Pigeon Bush; Fig. 7); F, Palliser Bay. B, Charles Borlase's house. The best defined extent of the 1855 earthquake rupture occurs in central Wairarapa Valley (central segment) with short lines representing subvertical fault traces south of Lake Wairarapa (southern segment) to the coast, and possible 1855-activated faults NE of Mauriceville (northern segment) (modified after Grapes & Downes 1997, fig. 37). The SW continuation of the central Wairarapa Valley segment of the fault into the Rimutaka Range shows evidence of recent displacement that in part may represent 1855 movement. Probable submarine extensions of the faulting are from Barnes (2005). Only the central Wairarapa Valley segment and coastal exposure of the southern segment of the 1855 rupture were described by Lyell. Upper inset shows plot of uplift or subsidence (m) v. distance (km) during the 1855 earthquake where measurement localities 1–6 are projected onto a 300°-trending line approximately normal to the trace of the 1855 fault rupture.
Published: 01 January 2010
; 2, Pencarrow Head; 3, Balley Rock; 4, Porirua Harbour; 5, Wainui; 6, Lower Wairau Valley. Fault displacement localities described in the text are shown as BM ( Begg & Mazengarb 1996 ); C ( Crawford 1865 ): J (Jackson; Grapes & Downes 1999 ); PB (Pigeon Bush; Fig. 7 ); F , Palliser
Journal Article
Journal: Elements
Published: 01 June 2018
Elements (2018) 14 (3): 179–184.
...Jonathan P. Swinchatt; David G. Howell; Sarah L. MacDonald The physical parameters of terroir are scale dependent. At the regional scale, climate is paramount and relates to the grape varietals most suited to the setting. Intermediate factors include geologic setting, sun exposure, and topography...
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Stick plot showing the magnitude–time relationships for the historical earthquakes Mw≥6.5 presented in Figure 3. Black sticks indicate events on identified active‐fault earthquake sources, and gray sticks indicate unidentified active‐fault earthquake sources. Short, intermediate, and long recurrence interval (RI) active faults have been distinguished (see the legend) from the literature, inferred from data on nearby faults and/or from unpublished data (Berryman, 1980; Beanland et al., 1989; Grapes et al., 1998; Pettinga et al., 2001; Schermer et al., 2004; Hornblow et al., 2014; Nicol et al., 2016). In cases where it was not possible to discriminate between intermediate or long‐fault recurrence intervals, the filled circles are half white and gray. Earthquakes possibly associated with subduction (horizontal arrow) and with surface rupture (vertical downward arrow) are indicated, as is the western Hawkes Bay event (“x” filled circle).
Published: 19 October 2016
, and long recurrence interval ( RI ) active faults have been distinguished (see the legend) from the literature, inferred from data on nearby faults and/or from unpublished data ( Berryman, 1980 ; Beanland et al. , 1989 ; Grapes et al. , 1998 ; Pettinga et al. , 2001 ; Schermer et al. , 2004
Journal Article
Published: 01 April 2020
Geochemical Perspectives (2020) 9 (1): 99–112.
..., vineyard “X” with a particular slope, elevation, sun angle, and soil type may produce better wine than vineyard “Y”, whereas the reverse may be true in years that are cooler and wetter. Finally, there are human controlled variables such as grape variety, rootstock, canopy management, fertilisation...
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Journal Article
Journal: Elements
Published: 01 June 2018
Elements (2018) 14 (3): 153–158.
...Lawrence D. Meinert Terroir involves the complex interplay of climate, soil, geology, and viticulture, all of which influence the character and quality of a wine from a given grape variety, rootstock, and viticultural practice. Contrary to the assertions of some wine writers, the minerals...
FIGURES
Journal Article
Journal: Elements
Published: 01 June 2018
Elements (2018) 14 (3): 159–165.
...Cornelis van Leeuwen; Laure de Rességuier A “terroir” is a cultivated ecosystem in which the vine interacts with the soil and the climate. The soil influences vine phenology and grape ripening through soil temperature, water supply and mineral supply. Limited water supply to the vines is critical...
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Journal Article
Published: 01 February 2020
Earthquake Spectra (2020) 36 (1): 138–163.
... fatality burden caused by earthquakes when compared with other areas of similar seismicity ( Nichols et al., 2000 ). The two most deadly New Zealand earthquakes, being the Hawke’s Bay earthquake ( M w 7.4) and the 2011 Christchurch earthquake ( M w 6.2), resulted in 256 and 185 fatalities, respectively...
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Journal Article
Journal: Elements
Published: 01 June 2018
Elements (2018) 14 (3): 167–172.
... to both environmental and cultural factors that together influence the grape growing to wine production continuum. While the landscape, geology, and soil strongly interact to influence a vine's balance of nutrients and water, it is the climate that is critical because it is this that limits where...
FIGURES
Journal Article
Published: 01 October 2024
American Mineralogist (2024) 109 (10): 1760–1784.
... in this contribution. Pyrometamorphism of xenoliths (XEN; p09 ): Thermally altered xenoliths are derived from both crustal and mantle sources subjected to high-temperature, low-pressure hornfels and sanidinite facies metamorphism by igneous melts ( Grapes 2006 ). Typically formed at temperatures above 900 °C...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2009
Lithosphere (2009) 1 (1): 4–28.
..., the Ms ~8.2 Wairarapa fault event in 1855, resulted in uplift of the hanging wall of that dextral-reverse fault near the southern coast of the North Island ( Fig. 1A ) and in the generation of a set of tsunami waves up to ~9 m high ( Grapes and Downes, 1997 ). The coseismic uplift reached a maximum near...
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Journal Article
Published: 15 August 2007
Canadian Journal of Earth Sciences (2007) 44 (7): 1005–1013.
.... At outcrop 416, a pronounced paleosurface with a relief of up to several metres is developed on limestones of the Upper Ordovician to Lower Silurian Allen Bay Formation. The weathering surface is encrusted by a centimetre- to decimetre-thick zone of brownish to yellowish iron hydroxides. A possible...
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A 300°-trending profile approximately normal to the submarine extension of the Wharekauhau Thrust in Palliser Bay showing the change in elevation of the 1855 uplift beach ridge crest shown in Figure 10a and b along the Cook Strait coast from Turakirae Head to west of the entrance to Port Nicholson (locations shown in Figs 1 and 4). Uplift amounts represent the height difference between the 1855 beach ridge crest and the modern beach ridge crest. The uplift height of the rock platform at Pencarrow Head determined by Roberts (1855) is also indicated. Also shown is the height of the beach ridge uplifted by the penultimate earthquake (fine dashed line; beach line immediately inland from the 1855 uplifted beach shown in Fig. 10a). Data for the Turakirae Head to Pencarrow Head section are from Begg & McSaveney (2005) and McSaveney et al. (2006). Data for 1855 uplift west of the entrance to Port Nicholson are from Pillans & Huber (1995) and R. H. Grapes (unpubl. data). The position of an unnamed fault (Begg & Mazengarb 1996) that may have been activated in 1855 and penultimate earthquake causing the reversal in beach ridge heights just north of Baring Head is indicated. The location of this fault and inferred sense of vertical displacement are shown on the inset map in Figure 4.
Published: 01 January 2010
Fig. 11. A 300°-trending profile approximately normal to the submarine extension of the Wharekauhau Thrust in Palliser Bay showing the change in elevation of the 1855 uplift beach ridge crest shown in Figure 10 a and b along the Cook Strait coast from Turakirae Head to west of the entrance
Journal Article
Published: 01 April 2017
Journal of Foraminiferal Research (2017) 47 (2): 208–218.
...João Moreno; Francisco Fatela; Eduardo Leorri; Filipa Moreno Abstract A hydro-climatic reconstruction is proposed for the Minho region (NW Portugal), integrating two different proxies: grape harvest dates (GHD) as a proxy of temperature variations, and benthic marsh foraminifera as a proxy...
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