Approximately 1.5km ENE on the upper convex surface of a broad moraine ridge
Altitude:
2000 m
Aspect:
N
Slope:
7 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 22' S 176° 14' W
Latitude Longitude DD
-85.367 -176.233
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
Estimated mean annual temperature:
-40
°C
Frozen ground depth:
45 cm
Frozen type:
Dry frozen over hard ice cemented
Frozen comment:
45cm
Geology
Geological setting:
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 possibly reworking older surface deposits; weathered soil overlies unweathered soil but it is not clear if the soil stratigraphy is due to weathering or reworking
Patterned ground:
Nil
Surface weathering or surface features:
Surface dolerite cobbles and boulders are moderately and weakly stained, subrounded to subangular, non-pitted but have moderate exfoliation
Soil
Soil parent material:
Doleritic fine textured slightly compact till
Previous disturbance:
Nil
Soil weathering stage:
6
Soil moisture status:
Ultraxerous, intermittent snow cover and adjacent snow patch but no thawing observed
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
79a
0
–
2
cm
yellowish red (5Y 5/6) fine gravelly silt forming a discrete mass almost entirely surrounded by pale yellow soil; cohesive; small salt flecks diffused throughout; finer rock particles subrounded and moderately altered; abrupt boundary,
79b
2
–
20
cm
pale yellow (5Y 7/3) fine gravelly sandy silt enclosing the yellowish red soil material; cohesive; small salt flecks diffused throughout; sharp boundary,
79c
20
–
45
cm
olive grey (5Y 5/2) fine gravelly sandy silt; moderately cohesive; larger rock particles fresh but smaller particles strongly altered; sharp boundary, on frozen ground