Walcott Bay, to the east of Walcott Glacier; approximately 2km east of Walcott Glacier; on the floor of an inactive stream channel with scattered moss patches; the site is beneath a moss patch
Altitude:
300 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
78° 14' S 163° 26' E
78° 13' S 163° 26' E
Latitude Longitude DD
-78.233 163.433
-78.217 163.433
Latitude longitude precision DD
0.008 0.008
0.008 0.008
Locality
Royal Society Range; Transantarctic Mountains
Survey
Ross Island & Vicinity, Antarctica, 1:250 000 US Geological Survey, 1986
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-21
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
The Walcott Bay area has a complex geology with basement rocks, small volcanic cones and an extensive drift mantle which include a wide range of rocks; the lower altitude surfaces represent the most recently exposed surfaces following retreat of ice from Walcott Bay and the nearby alpine glaciers; the lower slopes are extensively ice-cored and the landscape is being actively modified in places by thermokarst processes
Patterned ground:
Nil
Surface weathering or surface features:
The moss has some sand on the surface and is probably windblown; the adjacent surface without a moss cover is unweathered loose sandy pebble gravel