named after Siccar Point headland

E454396

The Siccar Point unconformity is a famous geological feature in Scotland that exemplifies James Hutton’s discovery of deep geological time and the principle of uniformitarianism.

All labels observed (1)

Label Occurrences
named after Siccar Point headland canonical 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geological feature ⓘ
geological unconformity ⓘ
associatedWith James Hall ⓘ
James Hutton ⓘ
John Playfair ⓘ
country United Kingdom ⓘ
demonstrates long intervals of erosion between rock-forming episodes ⓘ
multiple cycles of deposition, uplift, and erosion ⓘ
exposes older Silurian greywacke rocks ⓘ
younger Devonian Old Red Sandstone ⓘ
fieldTripDestinationFor geology students ⓘ
geologicalAge Paleozoic ⓘ
hasRockType greywacke ⓘ
sandstone ⓘ
influenced acceptance of deep time in Earth sciences ⓘ
development of modern geology ⓘ
locatedIn Berwickshire ⓘ
Scotland ⓘ
Siccar Point headland ⓘ
namedAfter Siccar Point headland ⓘ
observedBy James Hutton in the 18th century ⓘ
partOf Scottish geological heritage ⓘ
significance exemplifies James Hutton’s concept of deep geological time ⓘ
illustrates the principle of uniformitarianism ⓘ
supportsTheory deep geological time ⓘ
uniformitarianism ⓘ
touristAttraction true ⓘ
typeOf angular unconformity ⓘ
usedAs classic field example in geology education ⓘ
visibleFrom coastline at Siccar Point ⓘ

How these facts were elicited

Referenced by (1)

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

Siccar Point unconformity → hasNameOrigin → named after Siccar Point headland ⓘ