Approximately 6.5 km NE of Mount Blackburn at the head of Long Valley, on a high altitude, westward trending, Beacon Sandstone broad ridge, on a step on the ridge
Altitude:
2550 m
Aspect:
W
Slope:
3 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
86° 13.8' S 146° 42' W
86° 13.8' S 146° 42' W
Latitude Longitude DD
-86.2300 -146.700
-86.2300 -146.700
Latitude longitude precision DD
0.0008 0.008
0.0008 0.008
Locality
Scott Glacier region, southern Trans-antarctic Mountains on the Watson Escarpment
Survey
US Geological Survey 1:250 000 1968, Mount Blackburn
Climate
Soil climate zone:
Inland Mountain
Estimated mean annual temperature:
-40
°C
Frozen ground depth:
0 cm
Frozen type:
Dry frozen
Frozen comment:
Geology
Geological setting:
The sedimentary sequence is about 550m of Beacon Group rocks overlying the Kukri Peneplane cut in granite basement; The sediments are generally quartzitic sandstones and silty shale with occasional conglomerate; dolerite intrusive rocks cap the ridge top
Patterned ground:
Nil
Surface weathering or surface features:
Between bedrock exposures are thin patchy accumulations of disaggregated sandstone; the Beacon rocks show typical horizontal sandstone fragmentation patterns; there is little oxidation of the sandstone or little cavernous weathering; occasional dolerite clasts, probably from upslope, are strongly stained with deep 5-7cm deep pits on upper surfaces and have salt accumulations beneath
Soil
Soil parent material:
Weathered disaggregated sandstone with minor dolerite and other crystalline rock fragments
light grey to very pale brown (2.5Y 7/2 - 10YR 7/3) sandy granule and pebble gravel; loose; quartzose rock particles dominantly angular to subrounded and unstained but some dolerite fragments strongly stained and altered; a few scattered salts; distinct boundary,
241b
5
–
15
cm
light grey to very pale brown (2.5Y 7/2 - 10YR 7/3) sandy granule and pebble gravel; loose; salt accumulations round some clasts; rock particles angular to subrounded; many altered and readily disaggregated with salt in interstices; a few strongly altered dolerite fragments; sharp boundary, on sandstone,