ROCK OUTCROP

Halang Formation — Fault and Deformation

Deformed Halang sandstone–claystone interbeds, structural discontinuities, fault-proximal fracture damage and the geomorphic expression of the mapped Sukarapi structure.

16photographs

Fractured Halang interbeds in the outer fault-damage zone

Fault-proximal disruption of Halang interbeds

Narrow structural strand cutting Halang interbeds

$Folded and fractured thin beds$

$Steeply deformed and fractured Halang interbeds$

Fracture zone cutting deformed interbeds

Outcrop-scale folded and disrupted bedding

Steep weathered discontinuity within thin-bedded host rock

Central fault zone with disrupted and rotated bedding

$Pervasively fractured Halang damage zone$

$Steep fracture cutting thin-bedded Halang rocks$

Steeply inclined Halang sandstone–claystone interbeds

Waterfall developed along a mapped structural discontinuity