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all geography including DSDP/ODP Sites and Legs
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Table Mountain
Evaluating the role of topographic inversion in the formation of the Stanislaus Table Mountains in the Sierra Nevada (California, USA)
MODELLING AND ANALYSIS OF SOUTHERN AFRICAN GEOMAGNETIC FIELD OBSERVATIONS: 1840 UNTIL 1903
Recent changes in climate and permafrost temperatures at forested and polar desert sites in northern Canada
Antarctic permafrost: An analogue for water and diagenetic minerals on Mars
Thrust faults and fold vergence in the Palaeozoic middle and upper Witteberg Group, Cape Supergroup (Cape Fold Belt), Steytlerville: an interpretation of their relationship
Geochronology of Laramide synorogenic strata in the Denver Basin, Colorado
Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians
Mesoscopic Analysis of Diamictite in Semiconsolidated, Non-Oriented Core
Authigenic chabazite and implications for weathering in Sirius Group diamictite, Table Mountain, dry valleys, Antarctica
Minimum 10 Be exposure ages of early Pliocene for the Table Mountain plateau and the Sirius Group at Mount Fleming, Dry Valleys, Antarctica
L'orcelite des peridotites de Beni Bousera (Maroc), Ronda (Espagne), Table Mountain et Blow-Me-Down Mountain (Terre-Neuve) et du Pinde Septentrional (Grece)
Palladium, platinum, rhodium, ruthenium and iridium in peridotites and chromitites from ophiolite complexes in Newfoundland
Eolian features provide a record of the interaction between winds and the Earth’s surface. Most eolian features are identifiable on aerial photographs; some are large enough to be mapped from LANDSAT imagery. Therefore, eolian features can be remotely identified and interpreted in terms of the strength and flow pattern of the winds that produced them. The techniques that are useful in interpreting wind patterns from eolian features include: (1) Interpretation of wind direction, wind energy, and wind velocity from sand dunes and dune fields; (2) interpretation of wind direction and wind velocity from playas; and (3) interpretation of wind direction and relative wind velocity from scour features, dust and smoke plumes, vegetation patterns, and snow drifts. Wind patterns can be interpreted from eolian features even if the researcher does not have a direct knowledge of the field area nor ancillary data from wind-measuring stations in the region. However, the reliability of the interpretation and the amount of information that can be derived from eolian features are greatly increased if the observer has meteorological and sedimentological information about the area.