An undulating uneven very bouldery moraine surface about 1.5km SE of Evans Cove; the surface has been reworked by patterned ground/soliflual processes with finer sized soil material appearing to have flowed around very large boulders; the site is a pocket of finer till amongst large boulders
Altitude:
100 m
Aspect:
W
Slope:
2 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
74° 54' S 163° 44' E
Latitude Longitude DD
-74.900 163.733
Latitude longitude precision DD
0.008 0.008
Locality
Inexpressible Island, Terra Nova Bay
Survey
USGS 1:250 000 1968; Mt Melbourne SS 58-60/9
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
20 cm
Frozen type:
Hard ice-cemented
Frozen comment:
20cm
Geology
Geological setting:
The surface materials are bouldery tills derived principally from rocks of the Granite Harbour Intrusives; large boulders have been split and separated indicating regolith reworking by patterned ground processes
Patterned ground:
Weakly developed small to medium (2-5m) nets with borders marked by boulder accumulations
Surface weathering or surface features:
Cobbles and boulders mainly subangular and unstained
Soil
Soil parent material:
Granitic till reworked by patterned ground processes
Oceanic subxerous; no liquid water present and little local snow cover
Biological activity:
Few small patches of yellow and black lichen
Profile Description
Horizon
Depth
Description
52a
0
–
2
cm
olive grey (5Y 5/2) sandy silty gravel; cohesive; distinct vesicular crust; rock fragments subangular and unstained; abrupt boundary,
52b
2
–
15
cm
grey (5Y 5/1) gravelly silt; firmly cohesive; breaking to well developed silt ball structure; rock fragments subangular and unstained; abrupt boundary,
52c
15
–
20
cm
grey (5Y 5/1) gravelly silt; firmly cohesive; frosted breaking to well developed silt ball structure; rock fragments subangular and unstained; sharp boundary, on frozen ground