Alatna Valley, approximately 2.5km E of Battleship Promontory; an gently undulating moraine surface in a slight depression; a sand accumulation patch behind a boulder
Altitude:
950 m
Aspect:
N
Slope:
2 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 54.5' S 161° 03' E
76° 54.5' S 161° 03' E
Latitude Longitude DD
-76.908 161.050
-76.908 161.050
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:
-25
°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 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
Patterned ground:
Weakly developed broad nets
Surface weathering or surface features:
Strong landsurface stability indicated by wind-fluted and polished and oxidised boulder upper surfaces; abrasion on surfaces exposed to up-valley wind; a well developed pebble pavement between larger boulders; some salts precipitated on the edges of some boulders
dark yellowish brown (10YR 3/4) granular coarse sand; loose; weakly stratified; rock particles subangular to subrounded, strongly stained and weakly altered