Montserrat seen from Manresa
|Elevation||1,236 m (4,055 ft)|
|Parent range||Catalan Pre-Coastal Range|
|Easiest route||Via road BP-1121 from Monistrol de Montserrat|
Montserrat (Catalan pronunciation: [munsəˈrat]) is a multi-peaked mountain range near Barcelona, in Catalonia, Spain. It is part of the Catalan Pre-Coastal Range. The main peaks are Sant Jeroni (1,236 m), Montgrós (1,120 m) and Miranda de les Agulles (903 m).
"Montserrat" literally means "saw (serrated, like the common handsaw) mountain" in Catalan. It describes its peculiar aspect with multitude of rock formations which are visible from a great distance. The mountain is composed of strikingly pink conglomerate, a form of sedimentary rock. Montserrat was designated as a National Park in 1987.
The Benedictine Abbey can be reached by road, by the Aeri de Montserrat cable car, or by the Montserrat Rack Railway. The lower stations of both the rack railway and the cable car can be reached by Ferrocarrils de la Generalitat de Catalunya train from Barcelona's Plaça d'Espanya station. From the abbey, the Funicular de Sant Joan funicular railway goes up to the top of the mountain, where there are various abandoned hovels in the cliff faces that were previously the abodes of reclusive monks, while the Funicular de la Santa Cova descends to a shrine.
Hiking and climbing
The highest summit of Montserrat is called Sant Jeroni (Saint Jerome) and stands at 1,236 meters (4,055 feet) above sea-level. It is accessible by hiking trails which connect from the top entrance to the Sant Joan funicular, the monastery, or the base of the mountain.
The Cavall Bernat 1,111 meters (3,645 feet) is an important rock feature popular with climbers.
Montserrat is formed of conglomerate that was originally deposited in a fan delta at the margin of the Ebro Basin, part of the foreland basin to the Pyrenees, during the middle Eocene. The conglomerate was derived from the uplifting Catalan Coastal Ranges to the southeast of the basin and the clast type is dominated by Triassic sedimentary rocks. The fan had an original size of between 100–150 square kilometres. The resistance of the Montserrat conglomerate to erosion compared to the rest of the fill of the Ebro Basin explains its current mountainous nature.
The dominant clast lithology in the conglomerate is limestone and the sequence is cemented by calcite. The presence of so much carbonate in the rock has led to the formation of typical karst landforms, such as cave systems and karst towers.
In 1493, Christopher Columbus named the Caribbean island of Montserrat Santa Maria de Montserrate, after the Virgin of Montserrat. Again, in 1606, the Spanish expedition of Luis Vaéz de Torres charted Mount Ernest island in the Torres Strait as Santa Maria de Montserrate, due to its relatively high peak.:83 Also Monserrate is a 3.152 m high mountain that dominates Bogotá's downtown which has a church built in 1650 over the ancient Muisca sacred mountain and that includes a funicular and an aerial lift similar to the ones at Montserrat.
- Mapa Topogràfic de Catalunya - Institut Cartogràfic de Catalunya
- López-Blanco M.; Marzo M.; Burbank D.W.; Vergés J.; Roca E.; Anadón P.; Piña J. (2000). "Tectonic and climatic controls on the development of foreland fan deltas: Montserrat and Sant Llorenç del Munt systems (Middle Eocene, Ebro Basin, NE Spain)" (PDF). Sedimentary Geology. 138 (1–4): 17–39. Bibcode:2000SedG..138...17L. doi:10.1016/S0037-0738(00)00142-1.
- Guerrero J.; Gutiérrez F.; Gutiérrez M. (2014). Gutiérrez F.; Gutiérrez M. (eds.). Conglomerate Monoliths and Karst in the Ebro Cenozoic Basin, NE Spain. Landscapes and Landforms of Spain. Springer. ISBN 978-94-017-8627-0.
- The Complete Guide to National Symbols and Emblems: Volume 2, page 724
- Hilder, Brett (1980). The voyage of Torres : the discovery of the southern coastline of New Guinea and Torres Strait by Captain Luis Baéz de Torres in 1606. Hong Kong: University of Queensland Press.
|Wikivoyage has a travel guide for Montserrat (Spain).|
|Wikimedia Commons has media related to Montserrat.|