Ben Crom

Ben Crom
Binn Chrom
Ben Crom mountain
Highest point
PeakBen Crom summit, Mourne Mountains, County Down
Elevation526 m (1,726 ft)
Prominence81 m (266 ft)
Parent peakSlieve Binnian
ListingMyrddyn Dewey
Coordinates54°09′58″N 5°59′26″W / 54.166233°N 5.990448°W / 54.166233; -5.990448
Naming
EtymologyFrom Irish Binn Chrom, meaning "curved" or "stooped peak"
Native nameBinn Chrom (Irish)
English translationCurved/stooped peak
Geography
Ben Crom
County Down, Northern Ireland
CountryUnited Kingdom
StateNorthern Ireland
CountyCounty Down
Parent rangeMourne Mountains
OSI/OSNI gridJ31300 26000
Topo mapOrdnance Survey of Northern Ireland OSNI Discoverer 29
BiomeUpland heath and grassland
Geology
Formed byIntrusive igneous activity
OrogenyCaledonian
Rock age~60 million years (Paleogene)
Mountain typeGranite mountain
Rock type(s)Aplitic granite with dolerite and feldspar porphyry dykes
Last eruptionNot applicable
Climbing
First ascentUnknown
Easiest routeHike from Silent Valley or Ott Car Park
Normal routeSouthern approach via Ben Crom Reservoir
AccessPublic access via Mourne Wall paths and upland trails

Ben Crom (from Irish Binn Chrom, meaning 'curved/stooped peak') is a 526 metres (1,726 ft) mountain in the Mourne Mountains in County Down, Northern Ireland. It is situated beside Ben Crom Reservoir, which is upstream from Silent Valley Reservoir. The mountain is composed of granite. An exposed area on the south west of the mountain shows where the Eocene aplitic granite meets the laccolith top of the older Mesozoic granite ring dike. The summit of the mountain features granite crags which are crossed by basic and feldspar porphyry dikes. The mountain is used for sheep grazing and hill walking.

The eastern slopes of Ben Crom are steep and covered in scree, a result of glacial activity that affected north- and east-facing slopes more intensely. The Ben Crom Reservoir, located nearby, was constructed in 1957 to supplement the Silent Valley Reservoir. Together, these reservoirs supply water to the Greater Belfast area and have a combined capacity of nearly 21 billion litres. The granite used in the construction of the reservoirs was sourced locally. From the Ben Crom dam wall, the valley between Ben Crom and Slievelamagan is visible, with notable contrasts between the steep, craggy eastern slopes and the smoother western slopes.