Site Information

Site number:
725
Authors:
IBC,GGC,MRB,DIC
Date recorded:
1993/12/31
Reason Sampled:
Soil moisture, permafrost monitoring and soil climate measurement
Description:
A gently sloping area forming a small bench on a moderately steep slope between Crater Hill and the east coast of Ross Island approximately 150m northwest from the Scott Base buildings; drill hole and access tube site located in the northern disturbed and downhill SE part of an experimental area
Altitude:
75 m
Aspect:
SE
Slope:
13 °
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
Site temperature profile
Depth (cm)Soil temp (°C)Notes
0 17 surface
Estimated mean annual temperature:
-18 °C
Frozen ground depth:
0 cm
Frozen type:
Hard frozen and ice cemented with segregated ice
Frozen comment:
At ground surface

Geology

Geological setting:
The deposit comprises volcanics of the McMurdo Volcanics Formation mainly as scoriaceous flows; the surface materials are a thin cover of mainly fractured bedrock with addition of glacially derived granular and pebble clasts from outside the immediate area; the volcanic bedrock has been considerably fractured by freeze thaw; the surface age is probably very late Pleistocene (Ross Sea Glaciation) having been modified by McMurdo Sound filling glacial ice
Patterned ground:
Weakly developed and without distinctive trough expression or well developed net pattern
Surface weathering or surface features:
Surface soil was removed to show a uniformly greyish brown subsurface above the frozen ground

Soil

Soil parent material:
Fragmented bouldery volcanic bedrock with some additions of glaciogenic finer materials, in part with some modification by slope drift processes; surface of the soil to approximately 30cm depth was removed by bulldozer
Previous disturbance:
No evidence of past mechanical disturbance at the immediate trial site area but moderate foot traffic disturbance is very likely; present disturbance includes the presence of numerous particles of introduced organic and inorganic materials; at this site the active layer has been removed
Soil weathering stage:
6 1 (Campbell & Claridge 1975)
Soil moisture status:
Xerous to subxerous; soil is moist below the surface; some moisture derived from small transient snow banks
Biological activity:
A few small patches of yellow lichen and some moss in the general vicinity
Profile Description
HorizonDepthDescription
725b -144 – 40 cm
725a 0 – 14 cm top of frozen ground
725c 40 – 56 cm
725d 56 – 89 cm
725e 89 – 117 cm

Sample Data

Physical Data
Sample nameDepth descriptionTop (cm)Base (cm)Bulk DensityDry Bulk DensityGravimetric MoistureVol. Moisture (BD=2)
725a 0-14 0 14 0.86 47.16
725b 144-40 -144 40 1.04 40.75
725c 40-56 40 56 1.3 27.43
725d 56-89 56 89 1.8 13.97
725e 89-117 89 117 2.38 15.2
Particle size distribution
Sample name< 2 mm2 - 0.5 mm0.5 - 0.25 mm0.25 - 0.1 mm0.1 - 0.05 mm0.05 - 0.02 mm0.02 - 0.002 mm< 0.002 mmFe2O3CaCO3Notes
725a 36.0
725b 37.0
725c 40.0
725d 24.0
725e 13.0
Clay Mineralogy
Sample nameMicaIHMHIV - IHMICHLVTHIVCHLSMCHL SMFE - CHLHTQTZFLDHBCALNotes
725a :
725b :
725c :
725d :
725e :

Photos

Photo record:
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