Soil moisture and permafrost investigation; examination on beach ridge surfaces of differing ages
Description:
Approximately 155m from the coast in Arnold Cove; east from the S end of the Marble Point Air Facility; on a backslope hollow of the second clearly defined raised beach surface
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
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
10 cm
Frozen type:
Hard ice-cemented
Frozen comment:
10cm
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; the backslope sediments are sandy but may be wind accumulated
Patterned ground:
Nil
Surface weathering or surface features:
Marble clasts are distinctly crumbled; distinct surface oxidation and crumbling of some gneiss and granodiorite clasts