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  • A regional stratigraphic isochron (ca. 8000 C 14 yr B.P.) from final deglaciation of Hudson Strait
  • 1996
  • Implications of stratigraphic and paleoclimatic records of the last interglaciation from the Nordic seas
  • 1996
  • Most published interpretations of the stratigraphic data that form the basis for most of the world's Holocene sea-level curves do not consider palaeotsunamis as agents of coastal sedimentation. Biostratigraphic investigations of modern tsunami
  • 1996
  • The Vedde Ash Bed (mid-Younger Dryas) and the Saksunarvatn Ash (early Holocene) are important regional stratigraphic event markers in the North Atlantic, the Norwegian Sea, and the adjacent land area.It is thus essential to date them as precisely
  • 1996
  • . The sediments are significantly older than Two Creeks, both palynologically and stratigraphically and in radiocarbon age.
  • 1996
  • Two long sedimentary records from Jersey, Channel Islands: stratigraphic and pedological evidence for environmental change during the last 200 kyr
  • 1996
  • C 14 dating ; Climatic variation ; Geochronology ; Grain size distribution ; Illinois ; Interglacial ; Isotope analysis ; Lithostratigraphy ; Palaeosol ; Quaternary ; Stratigraphic correlation ; United States of America
  • 1996
  • Fairbanks that imply a deposition age of about 190,000 yr for SCt. This new reliable age assignment confirms independent stratigraphic evidence of a pre-last interglaciation age, and also has implications for regional correlations of glacial and nonglacial
  • 1996
  • in northwestern Alaska. The new geochronological data further confirm stratigraphic and paleogeographic evidence for contemporaneous advance of pre-late-Wisconsin glaciers from indeppendent northwestern and southeastern source areas into Bristol Bay.
  • 1996
  • British Columbia ; C 14 dating ; Canada ; Dating ; Earthquake ; Humid environment ; Methodology ; Sand ; Stratigraphic correlation ; Stratigraphy ; Tsunami ; United States of America ; Washington State
  • 1996
  • and orientation analyses show that pinnacle development is largely controlled by lithological and stratigraphic conditions. Further analysis indicates that Tibetan limestone pinnacles were formed by strong physical weathering under periglacial conditions. Four
  • 1996
  • , and the collapse (or truncation) of soils and other units beneath and along mound edges. The hypothesis, however, must not be applied to all other Mima or mlma-like mounds, unless votex motion can be determined and if stratigraphic similarities can be demonstrated.
  • 1996
  • the lateritisation was not continuous but occurred in phases. Geoarcheological investigations and Quaternary stratigraphical studies date the lateritic crust surface to the early late Neogene. Neotectonics have played a vital role in shaping the present landscape.
  • 1996
  • Stabilized eolian deposits, mostly parabolic dunes and sand sheets, cover much of the landscape of northeastern Colorado and adjacent parts of southwestern Nebraska in four geographically distinct dune fields. Stratigraphic and soil geomorphic
  • 1996