For determination of sources and levels of soil contaminants around Scott Base
Description:
SS6 T1; this site is situated 3.8 m southeast of the southern corner of the field store building at the foot of a small slope; just of the edge of a traffic way
Altitude:
7 m
Aspect:
SW
Slope:
8 °
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:
40 cm
Frozen type:
Ice-cemented
Frozen comment:
40
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:
Some small patches of salt are present within a metre of the site; the surface is just outside of vehicle access areas; foreign materials include copper cable
Soil
Soil parent material:
Old fill materials formed for construction of the field store building; probably included accumulations of younger materials derived from activities outside the field store
Previous disturbance:
The land surface was shaped at the time of construction of the field store building; probably minimal disturbance since apart from activities around the field store