On the S side of Wright Valley, approximately 4.5km from the Wright Upper Glacier; on a moraine surface to the south of the Labyrinth; a bouldery moraine knoll on the upper sloping surface of the knoll, 20m from the crest
Till deposits of the upper Wright Valley mark former extensions of the Wright Upper Glacier; the history of movement of this glacier is unclear; the deposit is probably Upper Wright Glacier till
Patterned ground:
Weakly developed broad nets
Surface weathering or surface features:
Boulders up to 2m and moderately rounded; upstanding to 75cm; distinct staining and dark varnished or polished surfaces; some crumbling and slight pitting; weak ventiforms; clasts fracturing rather than crumbling; a few salts under some stones; a weakly pavementic surface
Soil
Soil parent material:
Bouldery sandy till from predominantly dolerite and sandstone; probably includes some previously weathered materials
surface boulders, cobbles, pebbles and granular sand; rock particles moderately to strongly stained and rounded to subangular; some smaller particles moderately altered,
342b
0
–
10
cm
reddish yellow (7.5YR 6/6) pebbly to cobbly sandy gravel; weakly cohesive; moderately developed vesicular structure; rock particles subangular, moderately stained and some moderately altered; distinct boundary,
342c
10
–
24
cm
brownish yellow (10YR 6/6) sandy bouldery to pebbly gravel; few fine scattered salt flecks; weakly to moderately cohesive; some rock particles subrounded, weakly stained and weakly altered; indistinct boundary,
342d
50
–
60
cm
brownish yellow to very pale brown (10YR 6/6 - 7/4) bouldery sandy gravel; loose; rock particles subangular to subrounded and some weakly altered; sharp boundary,