A low till covered surface close to a small stream and a nearby meltwater lake alongside the Mincey Glacier
Altitude:
1300 m
Aspect:
E
Slope:
4 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
84° 58' S 177° 35' W
Latitude Longitude DD
-84.967 -177.58
Latitude longitude precision DD
0.008 0.04
Locality
West side of Shackleton Glacier at Cascade Bluff, Queen Maud Mountains
Survey
USGS 1:250 000 1968; Liv Glacier SV 1-10/5
Climate
Soil climate zone:
Coastal mountain
Estimated mean annual temperature:
-30
°C
Frozen ground depth:
30 cm
Frozen type:
Hard ice-cemented
Frozen comment:
30cm
Geology
Geological setting:
In the lower half of the Shackleton Valley, granites of the Granite Harbour Intrusives occur and tills are more varied in composition with Beacon Group sediments, dolerite and granite being the main components; the tills are young; because the climate is warmer, small streams and meltwater pools are present
Patterned ground:
Nil
Surface weathering or surface features:
Bouldery surface with little staining or weathering; no surface crust
Soil
Soil parent material:
Young till from sedimentary rocks, granite and dolerite
Xerous to subxerous; some water flowing in a nearby small stream
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
96a
0
–
10
cm
pale brown (10YR 6/3) cobbly silty gravel; loose; few fine salt flecks; many rock particles covered with silt coating; rock particles angular to subrounded and mainly unstained; indistinct boundary,
96b
10
–
30
cm
pale brown (10YR 6/3) cobbly silty gravel; loose; weakly developed vesicular structure; thin silt coatings on many rock particles; rock particles mostly angular to subrounded and unstained but some granite and dolerite particles moderately stained and partly altered; distinct boundary, on bouldery till