pilocene

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Triceratops disappeared thousands of years ago Royalty Free Stock Photo
Queleues fruilles of the pliocene forest of the cantal, vintage engraving Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
View from the Big Andreneasa mold cave
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
The organs of Ille-sur-Têt in the Pyrénées Orientales department in the Occitanie region - France Royalty Free Stock Photo
Location Transvania. The mold caves of Călimani Gurghiu volcano from the pilocene are 5,3 million years old. Peştera Mare din Andreneasa Cave has a unique gallery, the walls are formed by volcanic agglomerate and rarely sandstone. Fatörzsbarlang. Peşteră de mulaj.


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