The Asgard Range is comprised of Beacon Sandstone and Ferrar Dolerite; the landscape is ancient with the high altitude valley cirques cut in pre Miocene time; subsequent glaciation has been restricted mainly to valley head cirque type activity; the glacial deposits represent accumulations of local head wall materials which have probably been weathered in place before incorporation into local glaciers; the moraine sequence is complex
Patterned ground:
Weakly developed nets
Surface weathering or surface features:
Surface boulders moderately rounded many clasts strongly oxidised; well developed pitting on some clasts on both upper and lower surfaces
Recent 3 cm snowfall with some thawing and water films on rock surfaces and some moistening of the soil surface
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
385a
-2 – 0 cm
surface boulders, cobbles and sandy gravel; moist; rounded to subrounded, many strongly stained and moderately to strongly altered with yellowish red (5Y 5/8) internal oxide coatings,
385b
0 – 8 cm
strong brown (7.5YR 5/6) sandy gravel; moderately to firmly cohesive; strongly developed vesicular structure; rock particles mainly subrounded and weakly stained with slight to moderate alteration; sharp boundary,
385c
8 – 10 cm
strong brown (7.5YR 5/6) sandy gravel; ice cemented; rock particles subrounded and moderately stained