Brief description
Ellis Fjord is a small, fjord-like marine embayment in the vestfold Hills, eastern Antarctica. Modern sediment input is dominated by a biogenic diatom rain, although aeolian, fluvial, ice-rafted, slumped and tidal sediments also make a minor contribution. In areas where bioturbation is significant relict glaciogenic sediments are reworked into the fine-grained diatomaceous sediments to produce poorly sorted fine sands and silts. Where the bottom waters are anoxic, sediments remain unbioturbated and have a high biogenic silica component. Three depositional and non-depositional facies can be recognised in the fjord: an area of non-deposition around the shoreline; a relict morainal facies in areas of low sedimentation and high bioturbation; and a basinal facies in the deeper areas of the fjord.Issued: 2000-08-04
Data time period: 1991-10-01 to 1991-11-30
Data time period: 1995-11-01 to 1995-11-30
text: northlimit=-68.0; southlimit=-68.5; westlimit=78.0; eastLimit=79.0; projection=WGS84
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AU-ANL:PEAU :
http://nla.gov.au/nla.party-617536
- global : bef21805-b1c6-497f-b344-ae97d9a89ab3
- Local : ASAC_705
- URI : https://data.aad.gov.au/metadata/records/ASAC_705
- URI : https://data.aad.gov.au/metadata/records/ASAC_705