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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Kenya
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Mount Kenya (1)
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Somali Republic (1)
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Madagascar (1)
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Morocco
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West Africa
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Ghana
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Alpine Fault (3)
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Europe
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Western Europe
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Scandinavia
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Sweden
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United Kingdom
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Great Britain
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England (3)
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Hope Fault (4)
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Indian Ocean
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Mediterranean region (1)
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Mediterranean Sea
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East Mediterranean
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Mexico (1)
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North America
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Appalachians
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Oceania
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Pacific Coast (1)
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Pacific Ocean
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East Pacific
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Northeast Pacific
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North Pacific
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Bering Sea
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Northeast Pacific
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South Pacific
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West Pacific
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Brazil
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Southern Ocean
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Ross Sea
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Eddy County New Mexico
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New York
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North Carolina
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Wellington Fault (2)
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commodities
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mineral deposits, genesis (6)
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elements, isotopes
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isotope ratios (17)
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isotopes
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C-14 (10)
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Pb-206/Pb-204 (2)
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Rb-87/Sr-86 (1)
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Sm-147/Nd-144 (2)
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Hf-177/Hf-176 (5)
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Nd-144/Nd-143 (7)
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O-18/O-16 (7)
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Pb-206/Pb-204 (2)
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Pb-207/Pb-204 (2)
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Pb-208/Pb-204 (2)
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Rb-87/Sr-86 (1)
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S-34/S-32 (1)
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Sm-147/Nd-144 (2)
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Sr-87/Sr-86 (9)
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large-ion lithophile elements (1)
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Lu/Hf (4)
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metals
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alkali metals
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rubidium
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sodium (1)
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Sr-87/Sr-86 (9)
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aluminum (3)
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chromium (2)
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Hf-177/Hf-176 (5)
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iron
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lead
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rare earths
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neodymium
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Nd-144/Nd-143 (7)
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Sm-147/Nd-144 (2)
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samarium
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Sm-147/Nd-144 (2)
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nitrogen (1)
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oxygen
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O-18/O-16 (7)
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silicon (2)
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sulfur
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S-34/S-32 (1)
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fossils
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bacteria (1)
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Vertebrata
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Aves
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Invertebrata
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Protista
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Rotaliina
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microfossils
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Conodonta (1)
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palynomorphs
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miospores
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pollen (6)
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Plantae
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algae
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nannofossils (2)
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Spermatophyta
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problematic fossils (1)
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geochronology methods
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upper Quaternary
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Tertiary
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Oligocene (4)
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Clayton Formation (1)
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upper Paleocene
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Shahejie Formation (1)
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Paleoproterozoic (4)
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igneous rocks
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igneous rocks
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carbonatites (3)
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kimberlite (1)
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gabbros (3)
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granodiorites (3)
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harzburgite (1)
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pyroxenite (1)
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porphyry (2)
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basalts
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dacites (1)
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keratophyre
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phonolites (1)
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rhyolites
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trachytes (1)
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ophiolite (4)
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metamorphic rocks
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gneisses (3)
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impactites
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marbles (4)
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mylonites
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ophiolite (4)
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jade (1)
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framework silicates
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feldspar group
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plagioclase (1)
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nepheline group
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zeolite group
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orthosilicates
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zircon group
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zircon (19)
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sorosilicates
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epidote group
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melilite group
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ring silicates
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sheet silicates
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chlorite group
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mica group
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serpentine group
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sulfates
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Primary terms
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absolute age (40)
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Africa
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carbon
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C-13/C-12 (4)
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Caribbean region
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catalogs (1)
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Cenozoic
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Quaternary
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Pleistocene
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upper Weichselian
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upper Quaternary
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Brunhes Chron (1)
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Tertiary
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Neogene
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Columbia River Basalt Group (1)
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Pliocene
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Paleogene
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upper Paleocene
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Shahejie Formation (1)
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Central America
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ceramic materials (1)
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Chordata
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Vertebrata
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Tetrapoda
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Aves
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Charadriiformes (1)
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clay mineralogy (1)
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climate change (4)
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Romania
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France
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Scandinavia
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United Kingdom
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A-type granites (1)
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granodiorites (3)
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pyroxenite (1)
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porphyry (2)
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dacites (1)
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phonolites (1)
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impact statements (1)
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Indian Ocean
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Red Sea (1)
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Indian Ocean Islands
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intrusions (19)
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Invertebrata
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Insecta (1)
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Gastropoda (1)
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Protista
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Foraminifera
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Rotaliina
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Globigerinacea
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isotopes
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C-14 (10)
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stable isotopes
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Nd-144/Nd-143 (7)
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O-18/O-16 (7)
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Pb-206/Pb-204 (2)
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Pb-207/Pb-204 (2)
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Pb-208/Pb-204 (2)
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Rb-87/Sr-86 (1)
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S-34/S-32 (1)
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land use (6)
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mantle (8)
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Mesozoic
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Cretaceous
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Lower Cretaceous (3)
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Franciscan Complex (1)
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Jurassic
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Triassic
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Permian-Triassic boundary (1)
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Hf-177/Hf-176 (5)
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iron
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lead
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neodymium
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Nd-144/Nd-143 (7)
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Sm-147/Nd-144 (2)
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samarium
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Sm-147/Nd-144 (2)
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ytterbium (2)
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zirconium (1)
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metamorphic rocks
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gneisses (3)
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granulites
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kinzigite (1)
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-
impactites
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impact breccia
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suevite (1)
-
-
-
marbles (4)
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metaigneous rocks
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metagranite (1)
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metaperidotite (1)
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serpentinite (1)
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-
metasedimentary rocks
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metapelite (1)
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metasiltstone (1)
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metasomatic rocks
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rodingite (1)
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serpentinite (1)
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skarn (2)
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-
mylonites
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pseudotachylite (1)
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schists
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blueschist (1)
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metamorphism (16)
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Mexico (1)
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Grape Bay
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Image
FIGURE 6. Corrugations typical of molds of palmetto fronds at Grape Bay, Be...
in PRESERVATION OF TRACE FOSSILS AND MOLDS OF TERRESTRIAL BIOTA BY INTENSE STORMS IN MID–LAST INTERGLACIAL (MIS 5c) DUNES ON BERMUDA, WITH A MODEL FOR DEVELOPMENT OF HYDROLOGICAL CONDUITS
> PALAIOS
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
Diagenesis in coastal carbonates related to Pleistocene sea level, Bermuda Platform
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
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...
Image
FIGURE 1. Located 1040 km ESE of Cape Hatteras, North Carolina (inset), Ber...
in PRESERVATION OF TRACE FOSSILS AND MOLDS OF TERRESTRIAL BIOTA BY INTENSE STORMS IN MID–LAST INTERGLACIAL (MIS 5c) DUNES ON BERMUDA, WITH A MODEL FOR DEVELOPMENT OF HYDROLOGICAL CONDUITS
> 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
Image
FIGURE 3. Stratigraphic correlation of study sites along the south shore of...
in PRESERVATION OF TRACE FOSSILS AND MOLDS OF TERRESTRIAL BIOTA BY INTENSE STORMS IN MID–LAST INTERGLACIAL (MIS 5c) DUNES ON BERMUDA, WITH A MODEL FOR DEVELOPMENT OF HYDROLOGICAL CONDUITS
> PALAIOS
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
PRESERVATION OF TRACE FOSSILS AND MOLDS OF TERRESTRIAL BIOTA BY INTENSE STORMS IN MID–LAST INTERGLACIAL (MIS 5c) DUNES ON BERMUDA, WITH A MODEL FOR DEVELOPMENT OF HYDROLOGICAL CONDUITS
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
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. ...
Image
Maps showing known and inferred 1855 earthquake features with respect to th...
in Charles Lyell and the great 1855 earthquake in New Zealand: first recognition of active fault tectonics
> Journal of the Geological Society
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
Charles Lyell and the great 1855 earthquake in New Zealand: first recognition of active fault tectonics
Journal: Journal of the Geological Society
Publisher: Geological Society of London
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...
Image
Map of the central part of New Zealand (Cook Strait area) showing place nam...
in Charles Lyell and the great 1855 earthquake in New Zealand: first recognition of active fault tectonics
> Journal of the Geological Society
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
The Scale Dependence of Wine and Terroir: Examples from Coastal California and the Napa Valley (USA)
Journal: Elements
Publisher: Mineralogical Society of America
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...
Image
Stick plot showing the magnitude–time relationships for the historical eart...
in Completeness of the Paleoseismic Active‐Fault Record in New Zealand
> Seismological Research Letters
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
8. WINE AND TERROIR
Journal: Geochemical Perspectives
Publisher: European Association for Geochemistry
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...
Journal Article
The Science of Terroir
Journal: Elements
Publisher: Mineralogical Society of America
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...
Journal Article
Major Soil-Related Factors in Terroir Expression and Vineyard Siting
Journal: Elements
Publisher: Mineralogical Society of America
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...
Journal Article
Patterns of earthquake-related mortality at a whole-country level: New Zealand, 1840–2017
Shannon Abeling, M.EERI, Nick Horspool, David Johnston, M.EERI, Dmytro Dizhur, M.EERI, Nick Wilson, Christine Clement, Jason Ingham, M.EERI
Journal: Earthquake Spectra
Publisher: Earthquake Engineering Research Institute
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...
Journal Article
The Climate Component of Terroir
Journal: Elements
Publisher: Mineralogical Society of America
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...
Journal Article
An evolutionary system of mineralogy, Part VIII: The evolution of metamorphic minerals
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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...
Includes: Supplemental Content
Journal Article
Late Holocene surface ruptures on the southern Wairarapa fault, New Zealand: Link between earthquakes and the uplifting of beach ridges on a rocky coast
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...
Journal Article
Origin of iron-oxide and silicate melt rocks in Paleogene sediments of southern Ellesmere Island, Canadian Arctic Archipelago, Nunavut
Journal: Canadian Journal of Earth Sciences
Publisher: Canadian Science Publishing
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...
Image
A 300°-trending profile approximately normal to the submarine extension of ...
in Charles Lyell and the great 1855 earthquake in New Zealand: first recognition of active fault tectonics
> Journal of the Geological Society
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
Records from Marsh Foraminifera and Grapevine Growing Season Temperatures Reveal the Hydro-climatic Evolution of the Minho Region (nw Portugal) from 1856–2009
Journal: Journal of Foraminiferal Research
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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