For determination of sources and levels of soil contaminants around Scott Base
Description:
SS11 T2; 31 m north-northwest of the water storage tanks alongside the track to the storage area; a smooth surfaced area that has had some disturbance from land shaping operations and which receives some runoff
Altitude:
23 m
Aspect:
NE
Slope:
9 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 51' S 166° 46' E
77° 51' S 166° 48' E
Latitude Longitude DD
-77.850 166.767
-77.850 166.800
Latitude longitude precision DD
0.008 0.008
0.008 0.008
Locality
Pram Point, Scott Base
Survey
not recorded
Climate
Soil climate zone:
Coastal mountain
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
32 cm
Frozen type:
Hard ice-cemented
Frozen comment:
32
Geology
Geological setting:
The materials comprise volcanics of the McMurdo Volcanics Formation mainly as scoriaceous lava flows; the surface materials are a thin cover of mainly fractured bedrock with addition of some glacially derived granular and pebble clasts from outside the immediate area; the volcanic bedrock has been considerably fractured by patterned ground freeze thaw; the surface age is probably very late Pleistocene (Ross Sea Glaciation) having been modified by McMurdo Sound filling glacial ice
Patterned ground:
Nil
Surface weathering or surface features:
There are surface salt efflorescences around the site; the surface has fewer stones than elsewhere
Soil
Soil parent material:
Disturbed scrape and fill material formed through land reshaping activities
Previous disturbance:
The ground surface has been disturbed by scraping activities for the construction of storage areas and access ways; foreign materials are mainly wood fragments