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  • 1
    Publikationsdatum: 2024-03-09
    Schlagwort(e): Clasts; Description; Elevation of event; Event label; Latitude of event; Lithologic unit/sequence; Lithology/composition/facies; Longitude of event; MULT; Multiple investigations; Polygon_Spur; Quartz_Hills; Transantarctic Mountains; Ventifacts
    Materialart: Dataset
    Format: text/tab-separated-values, 360 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Todd, Claire E; Stone, John O; Conway, Howard; Hall, Brenda L; Bromley, Gordon RM (2010): Late Quaternary evolution of Reedy Glacier, Antarctica. Quaternary Science Reviews, 29(11-12), 1328-1341, https://doi.org/10.1016/j.quascirev.2010.02.001
    Publikationsdatum: 2024-03-09
    Beschreibung: Fresh deposits above the margins of Reedy Glacier show that maximum ice levels during the last glaciation were several hundred meters above present near the glacier mouth and converged to less than 60 m above the present-day surface at the head of the glacier. Exposure ages of samples from five sites along its margin show that Reedy Glacier and its tributaries thickened asynchronously between 17 and 7 kyr BP At the Quartz Hills, located midway along the glacier, maximum ice levels were reached during the period 17-14 kyr BP. Farther up-glacier the ice surface reached its maximum elevation more recently: 14.7-10.2 kyr BP at the Caloplaca Hills; 9.1-7.7 kyr BP at Mims Spur; and around 7 kyr BP at Hatcher Bluffs. We attribute this time-transgressive behavior to two different processes: At the glacier mouth, growth of grounded ice and subsequent deglaciation in the Ross Sea embayment caused a wave of thickening and then thinning to propagate up-glacier. During the Lateglacial and Holocene, increased snow accumulation on the East Antarctic Ice Sheet caused transient thickening at the head of the glacier. An important result of this work is that moraines deposited along Reedy Glacier during the last ice age cannot be correlated to reconstruct a single glacial maximum longitudinal profile. The profile steepened during deglaciation of the Ross Sea, thinning at the Quartz Hills after 13 kyr BP while thickening upstream. Near its confluence with Mercer Ice Stream, rapid thinning beginning prior to 7-8 kyr BP reduced the level of Reedy Glacier to close to its present level. Thinning over the past 1000 years has lowered the glacier by less than 20 m.
    Schlagwort(e): Antarctica; ICEM; Ice measurement; International Polar Year (2007-2008); ipy; IPY; Reedy_Glacier
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Bromley, Gordon RM; Hall, Brenda L; Stone, John O; Conway, Howard; Todd, Claire E (2010): Late Cenozoic deposits at Reedy Glacier, Transantarctic Mountains: implications for former thickness of the West Antarctic Ice Sheet. Quaternary Science Reviews, 29(3-4), 384-398, https://doi.org/10.1016/j.quascirev.2009.07.001
    Publikationsdatum: 2024-03-09
    Beschreibung: Deposits corresponding to multiple periods of glaciation are preserved in ice-free areas adjacent to Reedy Glacier, southern Transantarctic Mountains. Glacial geologic mapping, supported by 10Be surface-exposure dating, shows that Reedy Glacier was significantly thicker than today multiple times during the mid-to-late Cenozoic. Longitudinal-surface profiles reconstructed from the upper limits of deposits indicate greater thickening at the glacier mouth than at the head during these episodes, indicating that Reedy Glacier responded primarily to changes in the thickness of the West Antarctic Ice Sheet. Surface-exposure ages suggest this relationship has been in place since at least 5 Ma. The last period of thickening of Reedy Glacier occurred during Marine Isotope Stage 2, at which time the glacier surface near its confluence with the West Antarctic Ice Sheet was at least 500 m higher than today.
    Schlagwort(e): International Polar Year (2007-2008); IPY
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-03-09
    Schlagwort(e): Antarctica; Area/locality; Beryllium-10; Beryllium-10, standard deviation; Correction; ELEVATION; Exposure age; Exposure age, standard deviation; ICEM; Ice measurement; LATITUDE; LONGITUDE; Reedy_Glacier; Sample comment; Sample ID
    Materialart: Dataset
    Format: text/tab-separated-values, 324 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2024-03-09
    Schlagwort(e): Antarctica; Area/locality; Beryllium-10; Beryllium-10, standard deviation; Correction; ELEVATION; Exposure age; Exposure age, standard deviation; ICEM; Ice measurement; LATITUDE; LONGITUDE; Reedy_Glacier; Sample comment; Sample ID
    Materialart: Dataset
    Format: text/tab-separated-values, 444 data points
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 6
    Publikationsdatum: 2024-03-09
    Schlagwort(e): -; Accelerator mass spectrometry (AMS); Age, 10Beryllium; Age, dated; Age, dated standard deviation; Age, error; Beryllium-10; Beryllium-10, production rate per year; Beryllium-10, standard deviation; Correction; ELEVATION; Event label; LATITUDE; Lithologic unit/sequence; LONGITUDE; MULT; Multiple investigations; Polygon_Spur; Quartz_Hills; Sample ID; Tillite_Spur; Transantarctic Mountains
    Materialart: Dataset
    Format: text/tab-separated-values, 325 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-03-09
    Schlagwort(e): Caloplaca_Hills; Comment; Depth, relative; Description; Elevation of event; Event label; Latitude of event; Layer thickness; Lithologic unit/sequence; Lithology/composition/facies; Longitude of event; MULT; Multiple investigations; Observation; Polygon_Spur; Quartz_Hills; Transantarctic Mountains
    Materialart: Dataset
    Format: text/tab-separated-values, 154 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Digitale Medien
    Digitale Medien
    [s.l.] : Nature Publishing Group
    Nature 326 (1987), S. 587-589 
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] The Caroline No. 1 well is situated 15km south-east of Mt Gambier, South Australia, along the southeasterly extension of a small chain of intraplate basaltic volcanism (Fig. 1). On geomorphic grounds, the oldest volcanoes are at the north-west end of the chain. Mt Schank has an age of 4,900 yr1 and ...
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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