Permafrost and soil moisture examinations; investigation of differences at a patterned ground crack
Description:
Approximately 4.5km NW of Marble Point peninsula and W of the Marble Point Air Facility; about 100m from the Wilson Piedmont Glacier; on a surface near a small thawing snow patch; 50cm from a shallow patterned ground crack; a gently sloping surface, half way between a knoll crest and a pond at the foot of the slope; the site is between site 616 and 517
Altitude:
70 m
Aspect:
N
Slope:
2 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 24.94' S 163° 39.78' E
77° 25.1' S 163° 0.0' E
Latitude Longitude DD
-77.41570 163.66300
-77.4183 163.000
Latitude longitude precision DD
0.00008 0.00008
0.0008 0.008
Locality
Marble Point, western McMurdo Sound
Survey
USGS Antarctica Topographic Series 1:50,000; Marble Point, Antarctica
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
45 cm
Frozen type:
Hard ice-cemented
Frozen comment:
45cm
Geology
Geological setting:
The surface is a gently undulating till plain formed by retreat of the Wilson Piedmont Glacier; the Marble Point region is an old landscape, with deposits of phillipsite, buried soils and oxidised gneiss, which have been covered by advances of the grounded Ross Ice Shelf; later ice retreat and glaciological features have been controlled by changes in the stranded Wilson Piedmont Glacier; the till mantle is patchy and dominated largely by locally occurring rocks; granodiorite, granite, marble, gneiss, and dolerite
Patterned ground:
Weakly developed 20m nets; 5cm troughs with active open cracks
Surface weathering or surface features:
Most boulders angular and unstained; a few with distinct oxide staining; a moderately developed pebble and cobble pavement; calcium carbonate coatings beneath many surface clasts; some surface salt efflorescences adjacent to thawing snow patches
Soil
Soil parent material:
Bouldery sandy gravel till
Previous disturbance:
Extensive mechanical and human activity in the region since the mid-1950's
Nil at site; moss patches and cyanobacteria are common locally
Profile Description
Horizon
Depth
Description
618a
-2 – 0 cm
surface sandy gravel; rock particles angular and unstained,
618b
0 – 3 cm
light yellowish brown (2.5Y 6/4) sandy gravel; loose; some cemented silt coatings; rock particles angular and unstained with a few slightly oxidised; distinct boundary,
618c
3 – 8 cm
light yellowish brown (2.5Y 6/4) sandy gravel; weakly cohesive; slightly moist; rock particles angular and unstained; sharp boundary,
618d
8 – 24 cm
light yellowish brown (2.5Y 6/4) sandy gravel; very firm; frosted; rock particles subangular and unstained; some distinct silt coatings; sharp boundary,
618e
30 – 43 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618f
43 – 48 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618g
48 – 61 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618h
61 – 69 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618i
69 – 83 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618j
83 – 107 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618k
107 – 114 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,
618l
114 – 124 cm
drill core; light grey (5Y 7/2) sandy to silty gravel; rock particles subangular to subrounded,