The Darwin Mountains, just to the south of the Midnight Plateau; the site is near site 338 but from beneath a consolidated snowpack; the snow forms a continuous cover merging into the Midnight Plateau ice field; the soil beneath 60cm of hard snow was examined to compare soil weathering from beneath the snow cover with that at site 338 beyond the snowpack
Altitude:
1650 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
79° 56.9' S 156° 16.4' E
79° 57' S 156° 16' E
Latitude Longitude DD
-79.9483 156.2730
-79.950 156.267
Latitude longitude precision DD
0.0008 0.0008
0.008 0.008
Locality
Hatherton Glacier, Darwin Mountains, Transantarctic Mountains
Survey
United States Geological Survey 1966; 1:250,000 Carlyon Glacier, Antarctica
Climate
Soil climate zone:
Central Mountain
Estimated mean annual temperature:
-35
°C
Frozen ground depth:
0 cm
Frozen type:
Hard ice-cemented
Frozen comment:
0cm
Geology
Geological setting:
Rock outcrops on the area are Ferrar Dolerite; the ground surfaces have been exposed following retreat of ice from the Midnight Plateau; close to the ice edge, the soils appear less weathered but distinct successional surfaces marking ice retreat are not present; with increasing distance away from the ice front, soil weathering increases; the weathering is probably relict and unrelated to the present ice cover
yellowish brown (10YR 5/6 moist) sandy gravel; hard frozen; rock particles subangular to subrounded, unstained but easily disaggregated; NB: the rock particles in the sample have a very dark, almost blackish look and crush easily - the unusual dark colour is suggestive of anoxic weathering conditions