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Bodalsbreen

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Journal Article
Journal: Geology
Published: 01 February 2013
Geology (2013) 41 (2): 215–218.
... of sediment slurries at 2 °C under oxic conditions. A: Bodalsbreen Glacier, Norway. B: Haut Glacier d’Arolla, Switzerland. Black diamonds represent biotic; gray diamonds represent abiotic. Error bars are one standard deviation of the mean of triplicate bottles, and are generally within the size of the symbol...
FIGURES | View All (4)
Image
Difference of solute released (Δ μeq L−1) from Bodalsbreen Glacier, Norway (A), and Haut Glacier d’Arolla, Switzerland (B), slurries incubated at 2 °C under oxic conditions. Δ μeq L−1 is calculated as the difference in concentration of Ca2+ (diamonds), Mg2+ (triangles), K+ (squares), and Na+ (circles) in biotic incubations minus abiotic controls for each time point (mean of triplicate bottles).
Published: 01 February 2013
Figure 2. Difference of solute released (Δ μeq L −1 ) from Bodalsbreen Glacier, Norway (A), and Haut Glacier d’Arolla, Switzerland (B), slurries incubated at 2 °C under oxic conditions. Δ μeq L −1 is calculated as the difference in concentration of Ca 2+ (diamonds), Mg 2+ (triangles), K
Image
Calcium concentrations in aqueous extracts from dark incubations of sediment slurries at 2 °C under oxic conditions. A: Bodalsbreen Glacier, Norway. B: Haut Glacier d’Arolla, Switzerland. Black diamonds represent biotic; gray diamonds represent abiotic. Error bars are one standard deviation of the mean of triplicate bottles, and are generally within the size of the symbol.
Published: 01 February 2013
Figure 1. Calcium concentrations in aqueous extracts from dark incubations of sediment slurries at 2 °C under oxic conditions. A: Bodalsbreen Glacier, Norway. B: Haut Glacier d’Arolla, Switzerland. Black diamonds represent biotic; gray diamonds represent abiotic. Error bars are one standard
Image
Examples of the scanning electron microscope micrographs of the polished mounted grains of the size less than 1 mm. A: Agglomerates of finer grains in rock avalanche deposits. a—Round Top, New Zealand; b—Aoraki / Mount Cook, New Zealand; c—Coleridge, New Zealand; d—Coleridge with a section magnified to show that agglomerates are visible at higher resolution. B: Clean grains of glacial deposit with no rock avalanche input. e—Franz Josef Glacier terminal moraine, 2008/2009; f—Fox Glacier terminal moraine, 1999; g—Franz Josef Glacier LIA (Little Ice Age) moraine, 1750; h—Mueller Glacier lateral moraine; i—Bødalsbreen Glacier terminal position, 2010. Note the different scales for each micrograph.
Published: 01 April 2012
Glacier lateral moraine; i—Bødalsbreen Glacier terminal position, 2010. Note the different scales for each micrograph.
Journal Article
Journal: Geology
Published: 01 April 2012
Geology (2012) 40 (4): 319–322.
... Glacier lateral moraine; i—Bødalsbreen Glacier terminal position, 2010. Note the different scales for each micrograph. ...
FIGURES