Montserrat (mountain)
Template:Short description Template:About Template:Infobox mountain Montserrat (Template:IPA) 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 Les Agulles (903 m).<ref>Mapa Topogràfic de Catalunya - Institut Cartogràfic de Catalunya</ref>
It is the site of the Benedictine abbey, Santa Maria de Montserrat, which hosts the Virgin of Montserrat sanctuary.
"Montserrat" literally means "serrated (like the common handsaw) mountain" in Catalan. It describes its peculiar aspect with a multitude of rock formations that 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 Monastery of Montserrat which houses the virgin that gives its name to the monastery is also on the mountain, although it is also known as La Moreneta ("the little tan/dark one" in Catalan).<ref>Template:Cite web</ref>
Hiking and climbing
[edit]- The highest summit of Montserrat is called Sant Jeroni (Saint Jerome) and stands at Template:Convert 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. Montserrat is part of the GR footpath 172. The Cavall Bernat Template:Convert is an important rock feature popular with climbers.
- The well-known via ferrata Canal de las Damas (difficulty level D) leads from Collbató through a canal.<ref name="vehslage">Template:Cite book</ref>
Geology
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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 and 150 square kilometres.<ref name="Lopez_Blanco_etal_2000">Template:Cite journal</ref> The resistance of the Montserrat conglomerate to erosion compared to the rest of the fill of the Ebro Basin explains its current mountainous nature.<ref name="Guerreroetal_2014">Template:Cite book</ref>
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.<ref name="Guerreroetal_2014"/>
Namesakes
[edit]In 1493, Christopher Columbus named the Caribbean island of Montserrat Santa Maria de Montserrate, after the Virgin of Montserrat.<ref>The Complete Guide to National Symbols and Emblems: Volume 2, page 724</ref> 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.<ref name="Hilder">Template:Cite book</ref>Template:Rp
In Bogotá, the Monserrate mountain (3,152 m high) has a funicular and aerial lift similar to those at Montserrat.