Siccar Point unconformity

E122990

The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.

All labels observed (3)

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf geological site
geological unconformity
accessibleFrom nearby village of Cockburnspath
contradicts strictly young-Earth interpretations of geology
dateOfFamousVisit 1788
demonstrates multiple cycles of deposition, deformation, erosion, and renewed deposition
exposes older tilted sedimentary rocks
younger overlying sedimentary strata
faces North Sea coast
formsPartOf Southern Uplands terrane
surface form: Southern Uplands geological region
hasApproximateDipOfOlderRocks near-vertical
hasApproximateDipOfYoungerRocks gently dipping
hasConservationStatus protected geological site
hasEducationalDesignation classic field locality for teaching unconformities
hasGeologicalAge Devonian for the younger rocks
Silurian for the older rocks
hasGeologicalSignificance classic example of angular unconformity
key evidence for deep geological time
key evidence for uniformitarianism
key site in the history of modern geology
hasGeologicalStructure angular unconformity
hasNameOrigin named after Siccar Point headland
hasRockType Old Red Sandstone
surface form: Devonian Old Red Sandstone

Silurian greywacke
hasStratigraphicRelationship younger strata overlie steeply tilted older rocks
hasTourismType geotourism destination
inspiredTheory James Hutton's concept of deep time
James Hutton's theory of the rock cycle
isPartOf the historical development of modern geology
isReferencedIn Theory of the Earth
surface form: James Hutton's writings on the Theory of the Earth

classical geology literature
isUsedFor field excursions for geology students
geological education
locatedIn Berwickshire
Scotland
Scottish Borders
Siccar Point unconformity self-linksurface differs
surface form: Siccar Point

United Kingdom
observedBy James Hall
James Hutton
John Playfair
overlainBy Old Red Sandstone
surface form: Devonian Old Red Sandstone
supports uniformitarian interpretation of Earth's history
underlainBy Silurian greywacke
visibleAt coastal cliff exposure

How these facts were elicited

Referenced by (4)

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

James Hutton studied Siccar Point unconformity
Siccar Point unconformity locatedIn Siccar Point unconformity self-linksurface differs
this entity surface form: Siccar Point
Hutton's Unconformity at Lochranza comparedWith Siccar Point unconformity
this entity surface form: Hutton's Unconformity at Siccar Point
Berwickshire Coast contains Siccar Point unconformity
this entity surface form: Siccar Point