Towards the eastern end of Alatna Valley, approximately 10km NNE of Battleship Promontory; near a granite knoll; in a patterned ground crack where wind-blown sand is accumulating
Altitude:
1000 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 52' S 161° 15' E
76° 52' S 161° 15' E
Latitude Longitude DD
-76.867 161.25
-76.867 161.25
Latitude longitude precision DD
0.008 0.04
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 high sand content of the soils may be due to the incorporation of wind-blown sand from erosion of local rocks
Patterned ground:
Moderately developed, partly infilled cracks; 50cm deep; some cracks active with sand infilling
Surface weathering or surface features:
The surface is moderately weathered with rounded to subrounded boulders, some strongly stained with polish; thin patchy surface salt accumulations
Soil
Soil parent material:
Wind-blown coarse sand from exfoliation of local granite, dolerite and sandstone
Dry at the site but snow probably lies in the patterned ground cracks
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
529a
0
–
5
cm
yellowish brown to dark yellowish brown (10YR 5/4 - 4/4) granular coarse sand; loose but with a weakly cohesive surface crust; rock particles mainly subangular and weakly stained