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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Antarctica
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Antarctic Peninsula
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Graham Land (1)
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Arctic Ocean (1)
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Arctic region
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Svalbard
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Spitsbergen
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Spitsbergen Island (1)
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Asia
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Far East
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China (1)
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Atlantic Ocean
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North Atlantic
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Hudson Bay (1)
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Canada
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Eastern Canada
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James Bay Lowlands (1)
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Quebec (2)
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Hudson Bay (1)
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Central America
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Nicaragua (1)
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Europe
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Western Europe
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Iceland (1)
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Scandinavia
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Norway
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Northern Norway (1)
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Troms Norway
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Lyngen Peninsula (1)
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Mediterranean Sea
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West Mediterranean
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Alboran Sea (1)
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Mount Baker (1)
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Northern Hemisphere (1)
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Oceania
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Micronesia
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Caroline Islands
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Palau (1)
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Pacific Ocean
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Equatorial Pacific (1)
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West Pacific (1)
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polar regions (1)
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Southern Hemisphere (1)
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Southern Ocean
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Bellingshausen Sea (1)
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United States
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Alaska (1)
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Colorado (1)
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Washington
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Whatcom County Washington (1)
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elements, isotopes
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carbon
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C-13/C-12 (2)
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C-14 (6)
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hydrogen
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D/H (2)
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isotope ratios (4)
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isotopes
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radioactive isotopes
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C-14 (6)
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Cs-137 (3)
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Pb-210 (4)
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stable isotopes
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C-13/C-12 (2)
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D/H (2)
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N-15/N-14 (1)
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O-18/O-16 (1)
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metals
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alkali metals
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cesium
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Cs-137 (3)
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lead
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Pb-210 (4)
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nitrogen
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N-15/N-14 (1)
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oxygen
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O-18/O-16 (1)
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fossils
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Invertebrata
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Protista
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Foraminifera (1)
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microfossils (1)
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Plantae
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algae
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diatoms (1)
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Bryophyta (1)
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Spermatophyta
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Angiospermae (1)
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geochronology methods
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optically stimulated luminescence (1)
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paleomagnetism (1)
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tephrochronology (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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Medieval Warm Period (4)
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middle Holocene (1)
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Neoglacial
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Little Ice Age (14)
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upper Holocene
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Little Ice Age (14)
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Laurentide ice sheet (1)
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metamorphic rocks
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turbidite (1)
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Primary terms
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absolute age (7)
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Antarctica
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Antarctic Peninsula
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Graham Land (1)
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Arctic Ocean (1)
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Arctic region
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Svalbard
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Spitsbergen
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Spitsbergen Island (1)
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Asia
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Far East
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China (1)
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-
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Atlantic Ocean
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North Atlantic
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Hudson Bay (1)
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Canada
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Eastern Canada
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James Bay Lowlands (1)
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Quebec (2)
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Hudson Bay (1)
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carbon
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C-13/C-12 (2)
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C-14 (6)
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Cenozoic
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Quaternary
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Holocene
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Medieval Warm Period (4)
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middle Holocene (1)
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Neoglacial
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Little Ice Age (14)
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upper Holocene
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Little Ice Age (14)
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Central America
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Nicaragua (1)
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climate change (4)
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earthquakes (1)
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Europe
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Western Europe
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Iceland (1)
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Scandinavia
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Norway
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Northern Norway (1)
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Troms Norway
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Lyngen Peninsula (1)
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glacial geology (3)
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hydrogen
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D/H (2)
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Invertebrata
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Protista
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Foraminifera (1)
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-
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isotopes
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radioactive isotopes
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C-14 (6)
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Cs-137 (3)
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Pb-210 (4)
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stable isotopes
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C-13/C-12 (2)
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D/H (2)
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N-15/N-14 (1)
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O-18/O-16 (1)
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-
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Mediterranean Sea
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West Mediterranean
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Alboran Sea (1)
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-
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metals
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alkali metals
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cesium
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Cs-137 (3)
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-
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lead
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Pb-210 (4)
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nitrogen
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N-15/N-14 (1)
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Northern Hemisphere (1)
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ocean circulation (1)
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Oceania
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Micronesia
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Caroline Islands
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Palau (1)
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oxygen
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O-18/O-16 (1)
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Pacific Ocean
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Equatorial Pacific (1)
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West Pacific (1)
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paleoclimatology (8)
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paleomagnetism (1)
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permafrost (1)
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Plantae
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algae
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diatoms (1)
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Bryophyta (1)
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Spermatophyta
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Angiospermae (1)
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sedimentary structures
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planar bedding structures
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varves (1)
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sedimentation (2)
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sediments
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marine sediments (4)
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peat (1)
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Southern Hemisphere (1)
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Southern Ocean
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Bellingshausen Sea (1)
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United States
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Alaska (1)
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Colorado (1)
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Washington
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Whatcom County Washington (1)
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sedimentary rocks
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turbidite (1)
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sedimentary structures
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sedimentary structures
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planar bedding structures
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varves (1)
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sediments
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sediments
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marine sediments (4)
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peat (1)
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turbidite (1)
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Little Ice Age
Dramatic weakening of the East Asian summer monsoon in northern China during the transition from the Medieval Warm Period to the Little Ice Age
Precise chronology of Little Ice Age expansion and repetitive surges of Langjökull, central Iceland
High-elevation fire regimes in subalpine ribbon forests during the Little Ice Age and Medieval Period along the Continental Divide, Colorado, U.S.A.
Lacustrine stable isotope record of precipitation changes in Nicaragua during the Little Ice Age and Medieval Climate Anomaly
Mild Little Ice Age and unprecedented recent warmth in an 1800 year lake sediment record from Svalbard
Varve formation during the past three centuries in three large proglacial lakes in south-central Alaska
Precipitation changes in the western tropical Pacific over the past millennium
Visitors to ‘the northern playgrounds’: tourists and exploratory science in north Norway
Abstract This paper outlines some significant visits made to north Norway by geologists and mountaineers from Britain and Ireland from the early to late nineteenth century. These visitors wrote up their travels and climbing experiences in a region in north Norway that was difficult to get to other than by sea: Øksfjordjøkelen and Lyngen. Early travellers revealed the sights of the fjord areas and thereby promoted the region for subsequent travellers. Leopold von Buch’s Travels though Norway and Lapland during the Years 1806, 1807, and 1808 probably prompted J. D. Forbes to visit and produce Norway and Its Glaciers and Archibald Geikie’s Geological Sketches at Home and Abroad as part of the contemporary discussions about the ‘glacial theory’. In the latter years of the nineteenth century the British climbers William Cecil Slingsby and George Hastings, with local climber Josef Caspari, explored the Lyngen Peninsula. Elizabeth Main (Mrs Aubrey Le Blond) also climbed in Lyngen. As well as providing written summaries of their exploits, the early explorers included photographs in their books. Some of these images are helpful in the reconstruction of the glacierized landscapes at the end of the Little Ice Age. It is suggested that present-day travellers might leave their observations available, in digital media, for future investigators.
Climate change and recent sedimentation in Nastapoka Sound, eastern coast of Hudson Bay
Late Holocene glacial advance and ice shelf growth in Barilari Bay, Graham Land, west Antarctic Peninsula
Palaeoclimate and palaeoceanographic conditions in the westernmost Mediterranean over the last millennium: an integrated organic and inorganic approach
Long-term dynamics of a palsa in the sporadic permafrost zone of northwestern Quebec (Canada)
Abstract The Middle Fork Nooksack River drains the southwestern slopes of the active Mount Baker stratovolcano in northwest Washington State. The river enters Bellingham Bay at a growing delta 98 km to the west. Various types of debris flows have descended the river, generated by volcano collapse or eruption (lahars), glacial outburst floods, and moraine landslides. Initial deposition of sediment during debris flows occurs on the order of minutes to a few hours. Long-lasting, down-valley transport of sediment, all the way to the delta, occurs over a period of decades, and affects fish habitat, flood risk, gravel mining, and drinking water. Holocene lahars and large debris flows (>10 6 m 3 ) have left recognizable deposits in the Middle Fork Nooksack valley. A debris flow in 2013 resulting from a landslide in a Little Ice Age moraine had an estimated volume of 100,000 m 3 , yet affected turbidity for the entire length of the river, and produced a slug of sediment that is currently being reworked and remobilized in the river system. Deposits of smaller-volume debris flows, deposited as terraces in the upper valley, may be entirely eroded within a few years. Consequently, the geologic record of small debris flows such as those that occurred in 2013 is probably very fragmentary. Small debris flows may still have significant impacts on hydrology, biology, and human uses of rivers downstream. Impacts include the addition of waves of fine sediment to stream loads, scouring or burying salmon-spawning gravels, forcing unplanned and sudden closure of municipal water intakes, damaging or destroying trail crossings, extending river deltas into estuaries, and adding to silting of harbors near river mouths.