Approx 4km S of Mt Rich on an extensive undulating landsurface formed by over-riding and retreat of ice from Diamond Glacier; the surface has extensive patterned ground developed on rolling slopes with best development on lower gully slopes; on sloping ground, the polygon troughs have a high scarp face on the down-slope side and a short scarp face on the up- slope side; in many of the polygons, the surface of the soil has a distinct crust; in the patterned ground cracks, there is a greater amount of sandy material; the sample was collected from a crusty patch near the centre of a polygon
Altitude:
800 m
Aspect:
SE
Slope:
5 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
79° 49' S 158° 54' E
Latitude Longitude DD
-79.817 158.900
Latitude longitude precision DD
0.008 0.008
Locality
Victoria Land, Trans-antarctic Mountains; at the southern end of the Cook Mountains in the Brown Hills region of the Darwin Glacier
Survey
USGS 1:250,000 1963; Carlyon Glacier ST 57-60/13*
Climate
Soil climate zone:
Coastal mountain
Estimated mean annual temperature:
-24
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
Bouldery till from Granite Harbour Intrusives is widespread on a surface that is partly modified by patterned ground movement
Patterned ground:
Extensive moderately developed patterned ground with active troughs containing sand accumulations
Surface weathering or surface features:
Surface boulders are subangular and weakly stained without cavernous weathering; some scattered salts especially in polygon edges
Soil
Soil parent material:
Bouldery till with a sandy gravel matrix from granodiorite and granite
Xerous to subxerous; the surface is predominantly snow free; some patches of ice in patterned ground cracks; there are moist patches in the soils in some hollows
Biological activity:
Yellow and black lichens occur commonly
Profile Description
Horizon
Depth
Description
107a
0 – 10 cm
brown (10YR 5/3) sandy pebble gravel; cohesive; moderately developed vesicular structure; rock particles subangular to subrounded, weakly to moderately stained and partly coated with fines