South side of the Labyrinth, upper Wright Valley, approximately 0.5km SE of the SE corner of the Wright Upper Glacier; on a lateral moraine surface about 100m above the Labyrinth surface; a smooth but gently sloping terrace or bench-like surface about 10m from the escarpment edge
The Labyrinth has a negligible till cover with the Wright Upper Glacier carrying only occasional supraglacial boulders; in a more extended form more debris was probably carried as lateral drift; this lateral moraine gives an indication of the former extent and age of previous advances or retreat stages of the Wright Upper Glacier
Patterned ground:
Weakly developed broad nets
Surface weathering or surface features:
Scattered surface boulders from 1-4m showing some abrasion weak exfoliation and granular disintegration and weak ventiforms; boulders upstanding to 50cm; a close packed cobble and boulder pavement but weakly deflated; slight to moderate surface staining; some weathering may be inherited
Soil
Soil parent material:
Dolerite/sandstone bouldery sandy till; one schistose rock observed; the till may include much reworked material from the older adjacent landscapes
surface cobbles, boulders and granular sand; weakly to moderately stained; sandstone clasts unstained and non case hardened,
345b
0 – 5 cm
light yellowish brown (10YR 6/4) cobbly sandy gravel; weakly to moderately cohesive; moderately developed vesicular structure; rock particles subrounded and weakly to moderately stained; distinct boundary,
345c
5 – 10 cm
light yellowish brown (10YR 6/4) gravelly granular sand; slightly moist; rock particles subrounded, moderately stained and some partly altered; sharp boundary, on ice-cemented ground