Monte Cairo
 | This article needs additional citations for verification. (November 2024) |
Monte Cairo (1,669 m) is a mountain in Lazio[1] (in the province of Frosinone), overshadowing both the Abbey and the town of Monte Cassino, 5 kilometres to the south.[2] The ancient 'Mons Clarius' was so called because originally a temple dedicated to Apollo (Clarius) stood where the Abbey of Monte Cassino now stands. The Monte Cairo is the main peak of an isolated mountain range that extends eastwards for about 16–18 km from the Alta Valle del Melfa, the road from Rome to Naples.[citation needed]
Geology
[edit]Monte Cairo is situated in Italy's central peninsula which is dominated by active extensional tectonics.[3] The geological structure is of limestone[4] dating from the Cretaceous period[5] and due to its position in the region the formation is known to experience earthquakes and subsidence.[6]
The tops of the mountains are barren, in contrast to the partially wooded sides.[clarification needed]
Climbing
[edit] |
The top of the mountain is a 4-hour hike along a path through beech groves and across a plateau of snow. The vista from the top includes Appennino Marsicano (Monti Marsicani), the Mainarde, the Monti della Meta, the Matese, the sea up to Gaeta, the Pontine Islands, Mount Vesuvius and the Abbey of Montecassino.
At an altitude of 1300 m and west of Monte Cairo lies the Monte Pozzacone Refuge, a property owned by the town of Colle San Magno and a suitable base for climbing to the top of Monte Cairo. Other peaks of the group include the Monte Obachelle (1476 metres) where there is a significant Karstic sinkhole, the Pizzo di Prato Caselle (1372 metres), and the Cimmaron Villaneto (1315 m).
References
[edit]- ^ Cacciafoco, Francesco Perono; Cavallaro, Francesco (2023-03-09). Place Names. Cambridge University Press. p. 108. ISBN 978-1-108-49016-0.
- ^ Ring, Trudy; Watson, Noelle; Schellinger, Paul (2013-11-05). Southern Europe: International Dictionary of Historic Places. Routledge. p. 132. ISBN 978-1-134-25958-8.
- ^ Schlagenhauf, A.; Manighetti, I.; Benedetti, L.; Gaudemer, Y.; Finkel, R.; Malavieille, J.; Pou, K. (2011-07-15). "Earthquake supercycles in Central Italy, inferred from 36Cl exposure dating". Earth and Planetary Science Letters. 307 (3): 487–500. doi:10.1016/j.epsl.2011.05.022. ISSN 0012-821X.
- ^ Brandano, Marco; Loche, Marco (April 2014). "The Coniacian–Campanian Latium–Abruzzi carbonate platform, an example of a facies mosaic". Facies. 60 (2): 489–500. doi:10.1007/s10347-013-0393-x. ISSN 0172-9179.
- ^ CHIOCCHINI, MAURIZIO; PICHEZZI, RITA MARIA (2016-05-24). "CAIROELLA TRICAMERATA N. GEN., N. SP. (FORAMINIFERIDA, MILIOLOIDEA) FROM THE LOWER CENOMANIAN OF MONTE CAIRO (SOUTHERN LATIUM, CENTRAL ITALY)". Rivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy). 122: No 2 (2016). doi:10.13130/2039-4942/7248.
- ^ Vezzani, Livio; Festa, Andrea; Ghisetti, Francesca C. (2010-01-01). Geology and Tectonic Evolution of the Central-southern Apennines, Italy. Geological Society of America. p. 36. ISBN 978-0-8137-2469-0.
