Soil weathering examination of a rock sample on a raised beach surface
Description:
Approximately 90m from the coast in Arnold Cove; east from the S end of the Marble Point Air Facility; just below the crest of the third from the topmost distinct beach ridge surface
Altitude:
15 m
Aspect:
E
Slope:
8 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 24.72' S 163° 43.68' E
77° 24.80' S 163° 0.0' E
Latitude Longitude DD
-77.41200 163.72800
-77.4133 163.000
Latitude longitude precision DD
0.00008 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:
0 cm
Frozen type:
Frozen comment:
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, granodiorite marble with kenyite in places; some boulders are oxidised and partly crumbled
Patterned ground:
Indistinct net pattern with shallow sand-filled inactive cracks
Surface weathering or surface features:
Surface boulders and cobbles rounded but subsurface clasts at lower depth are subangular; granite boulders are disintegrating and some granodiorite clasts are distinctly oxidised and partly crumbly; the oxidation intensity appears to increase with proximity to the coast and may be a result of marine influence