Soil moisture and permafrost investigation; examination on beach ridge surfaces of differing ages
Description:
Approximately 150m from the coast in Arnold Cove; east from the S end of the Marble Point Air Facility; on the second clearly defined raised beach surface; a narrow ridge surface with a 10m 1o backslope and a 10o foreslope; on the crest of the ridge
Altitude:
20 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 24.70' S 163° 43.74' E
77° 24.80' S 163° 0.0' E
Latitude Longitude DD
-77.4117 163.72900
-77.4133 163.000
Latitude longitude precision DD
0.0008 0.00008
0.0008 0.008
Locality
Marble Point, western McMurdo Sound
Survey
USGS Antarctica Topographic Series 1:50,000; Marble Point, Antarctica
Climate
Soil climate zone:
Coastal Antarctic
Site temperature profile
Depth (cm)
Soil temp (°C)
Notes
155
-12
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
38 cm
Frozen type:
Hard ice-cemented
Frozen comment:
38cm
Geology
Geological setting:
The Marble Point beach ridges are a well defined set of raised beaches; they are though to have formed due to isostatic uplift; the age may range from 10,000 years; the lithology is mixed granite, gneiss, marble with kenyite in places; surface boulders are well rounded but clasts below the surface are subangular; sorting due to beach processes may only have been superficial
Patterned ground:
Weakly developed rectangular nets with 20cm deep troughs; some troughs closed with sand fillings
Surface weathering or surface features:
Bouldery gravel; many granodiorites have distinct oxidation
Soil
Soil parent material:
Weakly sorted sandy bouldery gravel of mixed lithology; some shell fragments present