unconformity
Sign in to savethumb|''Hutton's Unconformity'' at [[Jedburgh, Scotland, illustrated by John Clerk in 1787 and photographed in 2003.]] An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval of time before deposition of the younger layer, but the term is used to describe any break in the sedimentary geologic record. The significance of angular unconformity (see below) was shown by James Hutton, who found examples of Hutton'
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11 sectionsContents
- Types
- Disconformity
- Nonconformity
- Angular unconformity
- Paraconformity
- Buttress unconformity
- Blended unconformity
- Gallery
- See also
- References
- Further reading
thumb|''Hutton's Unconformity'' at [[Jedburgh, Scotland, illustrated by John Clerk in 1787 and photographed in 2003.]] An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval of time before deposition of the younger layer, but the term is used to describe any break in the sedimentary geologic record. The significance of angular unconformity (see below) was shown by James Hutton, who found examples of Hutton's Unconformity at Jedburgh in 1787 and at Siccar Point in Berwickshire in 1788, both in Scotland.
The rocks above an unconformity are younger than the rocks beneath (unless the sequence has been overturned). An unconformity represents time during which no sediments were preserved in a region or were subsequently eroded before the next deposition. The local record for that time interval is missing and geologists must use other clues to discover that part of the geologic history of that area. The interval of geologic time not represented is called a hiatus. It is a kind of relative dating.