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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 (1)
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South Shetland Islands
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King George Island (1)
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Arctic region
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Greenland
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Greenland ice sheet (1)
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Atlantic Ocean (1)
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Glacier Bay (1)
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North America
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Saint Elias Mountains (1)
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Pacific Ocean
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East Pacific
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Gulf of Alaska (2)
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North Pacific
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Northeast Pacific
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Gulf of Alaska (2)
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Scotia Sea Islands
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South Shetland Islands
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King George Island (1)
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United States
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Alaska
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Glacier Bay National Park (2)
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Maine
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elements, isotopes
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O-18/O-16 (1)
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Yakataga Formation (1)
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Laurentide ice sheet (2)
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Primary terms
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absolute age (3)
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Antarctica
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Antarctic Peninsula (1)
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South Shetland Islands
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King George Island (1)
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Arctic region
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Greenland
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Greenland ice sheet (1)
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Atlantic Ocean (1)
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carbon
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C-14 (4)
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Cenozoic
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Quaternary
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Holocene
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Middle Ages (1)
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Neoglacial
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Little Ice Age (1)
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upper Holocene
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Little Ice Age (1)
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Pleistocene
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upper Pleistocene (1)
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Tertiary
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Neogene
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upper Miocene (1)
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Pliocene (1)
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Yakataga Formation (1)
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climate change (1)
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conservation (1)
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earthquakes (1)
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faults (1)
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geochronology (1)
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glacial geology (6)
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government agencies (1)
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hydrology (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Ostracoda (1)
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Mollusca (1)
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Protista
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Foraminifera
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Rotaliina
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Cassidulinacea
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Globocassidulina (1)
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isostasy (1)
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isotopes
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radioactive isotopes
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C-14 (4)
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stable isotopes
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O-18/O-16 (1)
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North America
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Saint Elias Mountains (1)
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oceanography (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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East Pacific
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Northeast Pacific
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Gulf of Alaska (2)
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North Pacific
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Northeast Pacific
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Gulf of Alaska (2)
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paleoclimatology (3)
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paleoecology (2)
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paleomagnetism (1)
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Plantae
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algae
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diatoms (1)
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remote sensing (1)
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sedimentation (2)
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sediments
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clastic sediments
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outwash (1)
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till (1)
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United States
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Alaska
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Glacier Bay National Park (2)
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Seldovia Quadrangle (1)
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Yakutat Bay (1)
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Maine
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Washington County Maine (1)
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sediments
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sediments
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clastic sediments
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outwash (1)
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till (1)
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tidewater glaciers
Greenland tidewater glacier advanced rapidly during era of Norse settlement
Ocean‐Bottom Seismology of Glacial Earthquakes: The Concept, Lessons Learned, and Mind the Sediments
KEEPING THE BAY IN GLACIER BAY NATIONAL PARK: INTRODUCING GLACIER SCIENCE TO THE UNITED STATES SUPREME COURT
FORAMINIFERA IN TWO INLETS FED BY A TIDEWATER GLACIER, KING GEORGE ISLAND, ANTARCTIC PENINSULA
Influence of rapid glacial retreat on the rate of erosion by tidewater glaciers
Holocene history of Hubbard Glacier in Yakutat Bay and Russell Fiord, southern Alaska
Retreat of a tidewater margin of the Laurentide ice sheet in eastern coastal Maine between ca. 14 000 and 13 000 14 C yr B.P.
Late Holocene, high-resolution glacial chronologies and climate, Kenai Mountains, Alaska
Timing of late Cenozoic tidewater glaciation in the far North Pacific
Structural control of deposition by Pleistocene tidewater glaciers, Gulf of Maine
The temperate Laurentide Ice Sheet exhibited a grounded calving front as it retreated across coastal Maine about 14,000 to 12,500 B.P. The terminus resembled a modern tidewater glacier as the ice retreated through 0 to 80-m-deep water in the isostatically depressed region. Many areas of coastal Maine exhibit structural features that affect Holocene coastal landforms. In southwestern Maine, these northeast-southwest–trending strike valleys and ridges formerly exerted strong control on glacial retreat rates and deposition along the ice margin. Deposition of small DeGeer-type moraines and larger, stratified, subaqueous moraines/fans occurred where structural ridges slowed ice retreat. As ice retreat continued landward into even shallower water, the retreat rate was slowed by structural ridges, and deposition prograded to sea level, producing ice-contact beheaded deltas. In some areas, bedrock ridges underlie Gilbert-type deltas, while in other situations, ridges protruded above sea level as hills or islands. Eskers connected to the proximal sides of the deltas indicate that ridges deflected subglacial water to the surface in these locations.