Central Alatna Valley, approximately 9km NNE of Battleship Promontory; 500m from the southern edge of the stagnant Staten Island Heights glacier; on an undulating moraine surface; the site is a sand accumulation patch behind a boulder and in a patterned ground crack
Altitude:
950 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 52' S 161° 13' E
76° 52' S 161° 15' E
Latitude Longitude DD
-76.867 161.217
-76.867 161.25
Latitude longitude precision DD
0.008 0.008
0.008 0.04
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; granite outliers are also present; the presence of pink Irizar Granite indicates earlier up-valley ice movement; many of 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 processes
Patterned ground:
Extensive and well developed broad nets with active movement
Surface weathering or surface features:
Loose sandy surface; clasts in the patterned ground crack are subangular and weakly stained
Periodic summer snow falls; snow in patterned ground cracks but little visible soil moistening
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
531a
0
–
5
cm
yellowish brown (10YR 5/8) sand; loose; particles subangular to subrounded, moderately stained with some moderately altered,
531b
0
–
5
cm
yellowish brown (10YR 5/8) coarse sand from patterned ground crack; loose; particles subangular to subrounded moderately stained with some moderately to strongly altered