Soil weathering examination and permafrost examination
Description:
Approximately 2km east of Battleship Promontory; on the lower south slope of Alatna Valley; 20m below the crest of a minor moraine ridge on the valley side; the site is 6m from site 522 at the edge of the polygon
Altitude:
925 m
Aspect:
N
Slope:
4 °
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:
-28
°C
Frozen ground depth:
20 cm
Frozen type:
Hard ice-cemented
Frozen comment:
20cm
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 tills include granites and gneissic rocks which occur nearer the coast and indicate ice movement from the east
Patterned ground:
Weakly developed broad hummocky nets
Surface weathering or surface features:
Some dolerite weakly pitted; exfoliation and spalling are active; some cavernous weathering; boulders moderately stained and slightly rounded; a bouldery surface with some clasts upstanding; a weakly developed pavement with some ventiforms; some clasts with thick salt accumulations beneath
Soil
Soil parent material:
Sandy gravel derived from sandstone, dolerite and some granite