Authigenic deposits consist of such materials as manganese nodules.

The deposits, which are highly faulted, consist of three strata, the lowest averaging nine inches in thickness and the others being approximately two feet thick.

The shells are formed of aragonite, although the cameral deposits may consist of primary calcite.

The cone shaped deposits are fairly uniform and consist primarily of tuff in lapilli-size particles.

The deposit consists of two fields, the North and South Field, that latter having no connexion to the surface of the terrain.

The deposit consists of five chambers 5 x 4 x 4m.

Unconsolidated deposits in Nordaustlandet consist of scree slopes, block fields and raised shore deposits.

The deposits consist of soda, potash, borax and common salt.

The remaining deposits consisted of the alluvial materials mentioned above.

These deposits probably consist of both sedimentary rock and poorly indurated or unconsolidated sediments.