Structures in the icePasterze is one of the glaciers where the earliest studies of foliation were studied and described. | |||
 The great icefall of Pasterze generates the ice structures presented on this page (overview from Franz Josefs-Höhe). |  A closer view of the glacier just below the icefalls shows faint ogives (lower left). |  Zooming in even more, ogives and folding caused by longitudinal compression of the ice become evident. |  The strongest zoom shows intensively folded ice near the true left margin of the glacier. |
 Telephoto view of strongly folded ice at the true left margin of the glacier. |  Telephoto view of ogives and folding near the centerline of the glacier. |  Fisheye photo taken when standing on the glacier, in the are below the icefall. Meltwater streams exploit structures within the ice. |  Anticlinal folding becomes evident due to uneven ablation of different types of glacier ice. |
 Anticlinal (far left) and synclinal folding (right foreground). |  Ice of a tributary glacier descending via a small icefall is strongly compressed in the longitudinal direction, also causing folding. |  Fault showing lateral displacement to the right and bending of longitudinal foliation. |  A deeply incised meltwater channel exposes foliation structures in the ice. |
| All photos where taken on 6th and 7th August 2009 by Jürg Alean. | |||