Results 61 to 70 of about 816 (150)
Glaciotectonic features studied in the siliciclastic deposits of Cabeças Formation, Upper Devonian, represent the first evidence of Famennian glaciation in Southeastern Parnaíba Basin, Brazil. Outcrop-based stratigraphic and facies analyses combined with
Roberto Cesar de Mendonça Barbosa +2 more
doaj +1 more source
Our study investigates late Holocene ice-sheet activity in the northern Drygalski Basin (western Ross Sea) using a multi-proxy approach, including sediment properties, geochemical indicators, and diatom assemblages, combined with AMS 14C ages of a ...
Sangbeom Ha +6 more
doaj +1 more source
The “Lund Moraine”–the geomorphic limit of the last Young Baltic ice advance in the Öresund region
Here we present geomorphological evidence of a previously unrecognised ∼50 km long, ice-marginal moraine complex in southwestern Skåne, southernmost Sweden, which we name the “Lund Moraine”.
Alexanderson, Helena +10 more
core +1 more source
Massive ice of the Tuktoyaktuk area, western Arctic coast, Canada
The extensive coastal exposure of massive underground ice at Peninsula Point, southwest of Tuktoyaktuk, Northwest Territories, is believed to be intrasedimental ice.
Scott R. Dallimore, J. Ross Mackay
core +1 more source
Sedimentology of placer gravels near Mt. Nansen, Central Yukon Territory
Bibliography: p. 172-180.Unconsolidated sediments in the Mount Nansen area can be subdivided into eight elastic facies: I) clay-rich diamicton; 2) massive/stratified silt/clay; 3) massive/disorganized pebbly sand/sand; 4) stratified pebbly sand/sand; 5 ...
LeBarge, William Peter
core +1 more source
Evidence for a Middle Pleistocene glaciation of MIS 8 age in the southern North Sea
In the cores of borehole 89/2, situated at 54° 00 01′N and 5° 00 04′E about 70 km north of the Frisian Islands in the southern North Sea, two diamictons levels are found at ±70 and 100 m below sea floor (i.e.
Cleveringa, P. +5 more
core +2 more sources
The stratigraphic distribution, assemblage content, paleoecology and age of foraminifera recovered in fourteen of sixteen samples from the 5.63 m thick CRP-2 (Lithostratigraphic Unit 2.2) are discussed.
Webb, Peter-Noel, Strong, C Percy
core +1 more source
The upper 5-20 m of ice-rich permafrost at three sites overridden by the northwest margin of the Laurentide ice sheet in the Tuktoyaktuk Coastlands, western Arctic Canada, comprise massive ice beneath ice-rich diamicton or sandy silt.
Hart, Jane K. +17 more
core +1 more source
Pre-Late-Wisconsin Glacial History of the Naknek River Valley, Southwestern Alaska [PDF]
The lower Naknek River in southwestern Alaska dissects thick (~20m) exposures of Pleistocene glaciogenic sediments. The stratigraphy of the deposits and their physical, geochemical, mineralogical, and geochronological properties were studies to determine
Thompson, Caleb H.
core +1 more source
14C ages, grain size distribution and foraminifer abundance of sediments from the Barents Sea shelf
The origin of friable sediments blanketing the Barents Sea shelf is considered. It is shown that their characteristic seismoacoustic record patterns reflect low degree of diagenetic transformations and indicates continuous sedimentation.
R B Krapivner (7984715), Krapivner, R B
core +1 more source

