Nf. Glasser et al., LITHOLOGICAL AND STRUCTURAL CONTROLS ON THE SURFACE WEAR CHARACTERISTICS OF GLACIATED METAMORPHIC BEDROCK SURFACES - OSSIAN SARSFJELLET, SVALBARD, The Journal of geology, 106(3), 1998, pp. 319-329
Although there is an established relationship between geological struc
ture and the morphology of certain glacial erosional landforms, the ro
le of lithology is less clear. This is particularly true of the surfac
e wear characteristics of glaciated bedrock. In order to examine this
relationship, the surface wear characteristics of eight recently degla
ciated metamorphic bedrock slabs in the Kongsfjorden area of Svalbard
were mapped and recorded using detailed ''micromaps.'' Features record
ed included lee-side fracture surfaces, lee-side cavities, and the loc
ation and depth of open joints and quartz veins. On schist, glacial er
osion is favored by situations where ice movement is parallel to the t
rend of the bedrock foliation. In these situations, cavities may be el
ongated in the direction of ice flow. On more homogeneous lithologies
such as marble, cavity formation is suppressed and more uniform glacia
lly abraded rock surfaces develop. On all the metamorphic rocks examin
ed, glacial abrasion is favored in situations where bedrock foliation
is normal to ice flow. The structure of the parent bedrock, especially
the orientation of foliation, exerts a strong influence on the surfac
e wear characteristics of glaciated bedrock slabs and on the location
of subglacial cavities. Geological structure therefore has the potenti
al to influence rates of ice flow across bedrock surfaces.