Between Scott base and Crater Hill just north of west, a small nivation cirque above and southwest of a bend in the track to a US radio antennae facility; this site is the first of 5 sites sampled in sequence from beneath a snow bank to about 15m beyond to examine soil moisture relationships adjacent to a snow source; this site is underneath a patch of 'permanent' (but retreating) snow
Altitude:
70 m
Aspect:
SE
Slope:
6 °
Location Data
Observer
GGC
IBC
GPS
Yes
Latitude Longitude DMS
77° 50.67' S 166° 44.28' E
77° 51' 7" S 166° 44' 28" E
Latitude Longitude DD
-77.84450 166.73800
-77.8519 166.7410
Latitude longitude precision DD
0.00008 0.00008
0.00015 0.00015
Locality
Pram Point, Scott Base, Ross Island
Survey
Dept of Interior US Geological Survey 1986
Climate
Soil climate zone:
Coastal Antarctic
Site temperature profile
Depth (cm)
Soil temp (°C)
Notes
31
-4.9
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
0 cm
Frozen type:
Hard ice-cemented
Frozen comment:
0cm
Geology
Geological setting:
Rocks are predominantly scoria flows of the McMurdo Volcanics; Last Glaciation Ross 1 ice covered the site and traces of rocks (sandstone and granite granules and small pebbles) probably from the Royal Society Range can be found; the drift mantle is thin and patchy with bedrock a little below the surface; the ground surface is covered with permanent snow
Patterned ground:
Nil
Surface weathering or surface features:
Soil
Soil parent material:
Bouldery till and slope debris predominantly from scoria with minor accessions of sedimentary and granitic rocks