Hungary

Bathory Cave

Geothermally formed limestone cave with passages.

Location

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Historical Context

About

The Bathory Cave, located in the Danube-Ipoly National Park within Budapest's 2nd district, is an archaeologically significant site carved by geothermal springs from Dachstein limestone during the Pliocene era. The cave features horizontal passages and steep shafts, with speleothem formations and a small number of stalactites lining its interiors. Notably, it has been used by humans since the Neolithic period, with prehistoric remains such as bones of the woolly rhinoceros and red deer discovered within. The cave's historical significance is further enhanced by its use as a hermitage by Pauline monk László Báthory from 1437 to 1457 CE. The cave is recognized for its unique geological formations and its role in human history, from ancient habitation to medieval religious retreat.

Paleolithic
Mesolithic
Neolithic
Chalcolithic
Bronze Age
Iron Age
Classical Period
Post-Classical Period
Early Modern Period
Industrial Period
Contemporary Period
Temporal Epochs

Historical Timeline

Journey through time and discover key events in this site's history

Neolithic human use

8,000 BCE – 3,000 BCE

1437-1457 CE hermitage

1437 CE – 1457 CE

Classification

Archaeological Features

Unique architectural and cultural elements found at this historical site

category

Domestic and Habitation Structures

Caves
category

Environmental and Natural Features

Modified Caves
Knowledge Base

Frequently Asked Questions

Reference

Details

Country

Hungary

Coordinates

47.53° N, 18.96° E