A scoria patch on a moderately steep slope below a flattish surface just off the main Redcastle Ridge surface; description and sample site from the centre of a solifluction lobe
Altitude:
175 m
Aspect:
NW
Slope:
20 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
72° 26' S 169° 58' E
Latitude Longitude DD
-72.433 169.967
Latitude longitude precision DD
0.008 0.008
Locality
Northern Victoria Land near Hallett Peninsula; at Redcastle Ridge between the Arneb and Edisto Glaciers
Survey
MZMS 166; 1960 Tucker Glacier
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-16
°C
Frozen ground depth:
0 NoObs
Frozen type:
NoObs
Frozen comment:
NoObs
Geology
Geological setting:
Scoriaceous basalt, denser flow basalts and brown tuffites of the McMurdo Volcanic Group
Patterned ground:
Well developed patterned ground/solifluction lobes, coarse particles around the margins and fine material in the centres
Surface weathering or surface features:
Angular unstained surface pebbles with salt accumulations beneath some stones
Soil
Soil parent material:
Mainly coarse volcanic slope detritus reworked by patterned ground and solifluction processes