Érdekességek az Ipolytarnóci Ősmaradványok történetéből II.
1874. március 28-án hunyt el az ipolytarnóci megkövült fa első tudományos leírója, Kubinyi Ferenc.
Route: Fiľakovo - The Rocks of Belina – outlook – Monica – Monica-sag - Owl Castle, Šurice – Hajnáčka, train stop
The Rocks of Belina – outlook N48°13.594' E19°51.913'
The Rocks of Belina (Belinské skaly) formed on rocky border of the basalt ridge of the Belina peakare presenting the lava flow structure streamed from the Monosa volcano (584 m). To its most characteristic formations belong the Dragon´s teeth, the Mathyas Tower and the Bastion. The cliff ends at the Čamovce mine, the geological excavation of which extends up to the bottom of marine sediment.
The outlook offers panoramic views of the Karanč hill and villages Čakanovce and Radzovce.On the Rocks of Belina there is an impressive weathering of basalt with pillar and plate separability and with sloping movements.
Owl Castle N48°13.572' E19°54.781'
The noticeable rocky hill near Šurice, the “Owl Castle” (Soví hrad) (284 m) is the remainder of a 4-million-year-old volcanic diatreme. On its upper part the tuff layers remained in the former maar crater's lake. In the 13. century the fortress was built on the top of the cliff, owned by Beckov Dominion. The fortress had withstood even the Tartars invasion, but nowadays its remnants are hardly to be seen. There are remnants of water reservoir on top of the peak.