3.5km N of Taylor Glacier and 0.5km from the Rhone Glacier; on a granite knoll which has strongly developed cavernous weathering in the bedrock; the sample site is a granite outcrop with strong oxide staining
Altitude:
1425 m
Aspect:
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 41.3' S 162° 8.5' E
77° 42.5' S 162° 12' E
Latitude Longitude DD
-77.6883 162.142
-77.708 162.200
Latitude longitude precision DD
0.0008 0.004
0.004 0.008
Locality
Taylor Dry Valley, McMurdo Dry Valley region, Rhone Glacier
Survey
USGS 1:50,000 Antarctic Topo. Ser. Lake Bonney Quadrangle
Climate
Soil climate zone:
Inland Mountain
Estimated mean annual temperature:
-25
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
Granite outcrops on a knoll W of and 200m above the Rhone Glacier; bedrock granite exposures have been deeply eroded by cavernous weathering and deflation; the upper rock surfaces however are oxide stained and are hardened and resist erosion; most of the erosion takes place on the rock underside leaving thin oxide stained shells; the question is what is the nature of the case hardening and the surface rock shell
Patterned ground:
Nil
Surface weathering or surface features:
Oxidation and hardening of upper surfaces of granite
Soil
Soil parent material:
Rock sample of oxide stained, case hardened rock shell