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Sacred Mountain

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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), Montgr&oacute;s (1,120 m) and Miranda de les Agulles (903 m).

It is well known as the site of the Benedictine abbey, Santa Maria de Montserrat, which hosts the Virgin of Montserrat sanctuary.

&quot;Montserrat&quot; literally means &quot;serrated (like the common handsaw) mountain&quot; 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 (&quot;the little tan/dark one&quot; in Catalan).

Access 
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&#39;s Pla&ccedil;a d&#39;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. Montserrat is part of the GR footpath 172. The Cavall Bernat 1,111 meters (3,645 feet) is an important rock feature popular with climbers. 
The well-known via ferrata Canal de las Damas (difficulty level D) leads from Collbat&oacute; through a canal.

Panorama of the view from the Sant Jeroni summit of Montserrat

Mountain seen from Puig Lluent with a sea of clouds. 
Geology

Large-scale layering in the conglomerate sequence

Conglomerate with a rare sandstone layer on the path to Sant Jeroni on the flank of La Gorra Frigia. The conglomerate is polymict, clast-supported and poorly sorted with clasts ranging from pebble to boulder size 
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&ndash;150 square kilometres.&nbsp;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.

Namesakes 
In 1493, Christopher Columbus named the Caribbean island of Montserrat Santa Maria de Montserrate, after the Virgin of Montserrat.&nbsp;Again, in 1606, the Spanish expedition of Luis Va&eacute;z de Torres charted Mount Ernest island in the Torres Strait as Santa Maria de Montserrate, due to its relatively high peak.: 83 &nbsp;Also Monserrate is a 3,152 m high mountain that dominates Bogot&aacute;&#39;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.

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