Alatna Valley, approximately 5km E of Battleship Promontory; an undulating moraine surface near a knoll; a sand accumulation patch behind a boulder
Altitude:
925 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 53' S 161° 08' E
76° 53' S 161° 08' E
Latitude Longitude DD
-76.883 161.133
-76.883 161.133
Latitude longitude precision DD
0.008 0.008
0.008 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:
-25
°C
Frozen ground depth:
23 cm
Frozen type:
Hard ice-cemented
Frozen comment:
23cm
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 soils are very sandy below the bouldery surface; the sand may in part originate from local erosion and become incorporated into the soil through cryic process; multi-layering in the sand indicates variation in environmental conditions
Patterned ground:
Extensive and well developed broad nets with active movement
Surface weathering or surface features:
Dolerite boulders are oxidised and partly disaggregating; finer grained dolerite is strongly stained;