The crest of a hill at Wiest Bluff, a rounded convex surface with no cover material; sample collected from crevasses in dolerite rock
Altitude:
2160 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 22' S 176° 24' W
Latitude Longitude DD
-85.367 -176.400
Latitude longitude precision DD
0.008 0.008
Locality
Shackleton Glacier, Queen Maud Mountains, at the southern end of the Cumulus Hills, just north of Zaneveld Glacier junction with Shackleton Glacier
Survey
USGS 1:250 000 1968; Liv Glacier SV 1-10/5
Climate
Soil climate zone:
Inland mountain
Site temperature profile
Depth (cm)
Soil temp (°C)
Notes
0
6
(sunny day) soil surface
2
1
15
-11
Estimated mean annual temperature:
-40
°C
Frozen ground depth:
10 cm
Frozen type:
Frozen comment:
10cm
Geology
Geological setting:
Dolerite outcrops widely in an undulating ice overridden landscape; cover deposits are patchy varying from bouldery felsenmeer regolith to intermittent till patches; surface age is variable owing to remnant snow fields which behave as local nevee glaciers