# PARCS Data File # Site Name: Sunneshine Fiord # Location: CAN - Northwest Territories # Elevation: -146 # Latitude: 66.55 # Longitude: -61.72 # Site Code: SUNNELH # Entity Name: SU5LH # Entity Type: Core # Age Model: # Depth Thickness Age Method # # Suggested Data Citation: # # PALE contribution 72 Sunneshine Fiord; SUNNELH # John Andrews, 1995. Standard sedimentology. submitted to the PALE/PARCS Data Archive. # # # References: # Andrews, J. T., Syvitski, J. P. M., Williams, K. M., Jennings, A. E., Short, S. K., Mode, W. N., and Kravitz, J., 1994. Marine Geology of Sunneshine Fiord, Baffin Island. Geological Survey of Canada Open Field Report 2987, 2 sheets. Andrews, J.T., Osterman, L.E., Jennings, A.E., Syvitski, J.P.M., Miller, G. H. and Weiner, N., 1996. Abrupt changes in marine conditions, Sunneshine Fiord, eastern Baffin Island, N.W.T. during the last deglacial transition (Younger Dryas and H-0 events), In: Andrews, J.T., Austin, W.E.N., Bergsten, H., and Jennings, A.E. (eds.), Late Quaternary Paleoceanography of North Atlantic Margins. Geological Society of London, Special Publication, no. 111, p.11-27. Depth 1 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 5 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 10 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 15 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 20 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 25 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 30 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 35 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 40 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 45 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 50 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 55 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 60 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 65 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 70 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 75 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 80 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 85 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 90 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 95 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 100 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 110 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 120 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 130 Percent carbonate: 0 Percent dolomite: 0 Mass magnetic susceptibility: 0 Dry bulk density: 0 140 150 160 170 180 190 200 210