Summary

1911 Encyclopædia Britannica, Volume 11… (1911)

The glaciers front, with a perpendicular ice-wall, a shore of debris on which a few low plants are found to grow—poppies, mosses and the like. The islands are volcanic, the main geological formation being Tertiary or Jurassic basalt, which occasionally protrudes through the ice-cap in high isolated blocks near the shore. A connecting island-chain between Franz Josef Land and Spitzbergen is probable.
Source: Wikisource

1911 Encyclopædia Britannica, Volume 11… (1911)

The bear and fox are the only land mammals; insects are rare; but the avifauna is of interest, and the Jackson expedition distinguished several new species.
August Petermann expressed the opinion that Baffin may have sighted the west of Franz Josef Land in 1614, but the first actual discovery is due to Julius Payer, a lieutenant in the Austrian army, who was associated with Weyprecht in the second polar expedition fitted out by Count Wilczek on the ship “Tegetthof” in 1872. On the 13th of August 1873, the “Tegetthof” being then beset, high land was seen to the north-west.
Source: Wikisource

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