At the western end of Alatna Valley and approximately 2km east of Battleship Promontory; the site is in a patterned ground crack where wind-blown sand is accumulating
Altitude:
900 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 54.5' S 161° 02' E
76° 54.5' S 161° 02' E
Latitude Longitude DD
-76.908 161.033
-76.908 161.033
Latitude longitude precision DD
0.004 0.008
0.004 0.008
Locality
Convoy Range, Transantarctic Mountains; Alatna Valley
Survey
Ross Island & Vicinity, Antarctica, 1:250 000 US Geological Survey, 1986
Climate
Soil climate zone:
Coastal Mountain, xerous to subxerous
Estimated mean annual temperature:
-28
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
Alatna Valley has formed through ice recession from the Benson Glacier and ice from Staten Island Heights; the local rocks are extensive Beacon Sandstone outcrops capped with Ferrar Dolerite; the high sand content may be due to incorporation of wind-blown sand from erosion of adjacent dolerite and sandstone outcrops
Patterned ground:
Moderately developed nets; 50cm deep active cracks containing boulders and sand accumulations
Surface weathering or surface features:
Boulders up to 1m are moderately rounded and stained; some show distinct exfoliation; movement of boulders into the patterned ground cracks is active; windblown sand is also accumulating
Soil
Soil parent material:
Windblown largely pre-weathered sand derived from fretting and abrasion of local rocks
Local snow patches but no water or soil moistening observed
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
526a
-3 – 0 cm
dark brown (7.5YR 3/20 granular coarse sand; loose; quartz particles rounded and unstained, dolerite particles subrounded to rounded, strongly stained and many distinctly altered from pre-weathering