Ochil Fault

E486175

Ochil Fault is a major geological fault line in central Scotland that marks the southern boundary of the Ochil Hills and has significantly influenced the region’s landscape and settlement patterns.

All labels observed (2)

Label Occurrences
Ochil Fault canonical 1
Ochil Fault escarpment 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geological fault
normal fault
associatedWith Ochil Volcanic Formation
category Geology of Scotland
Seismic faults of Scotland
controls local drainage patterns
location of some transport routes
country Scotland
formsBoundaryOf Ochil Hills
geologicalPeriod Devonian
hasFeature steep scarp along parts of its length
hasThrownDownTo south
influenced regional landscape of central Scotland
settlement patterns in central Scotland
locatedIn central Scotland
mappedBy British Geological Survey
marksSouthernBoundaryOf Ochil Hills
movementType extensional
near Alloa
Alva
Dollar
Kinross
Perth
Stirling
Tillicoultry
partOf Midland Valley of Scotland
separates Devonian volcanic rocks from younger sedimentary rocks
Ochil Hills from the lowlands to the south
linked to: Ochil Hills
trend southwest–northeast
visibleAs topographic break between hills and lowlands

How these facts were elicited

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Alva hasNearbyFeature Ochil Fault
Abbey Craig partOf Ochil Fault escarpment
linked to: Ochil Fault