is a buried erosion
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, but the term is used to describe any break in the sedimentary
geologic record. The phenomenon of angular unconformities was discovered by James Hutton
, who found examples at Jedburgh
in 1787 and at Siccar Point
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. 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.
Types of unconformities
An unconformity between parallel layers
of sedimentary rocks
which represents a period of erosion or non-deposition. A paraconformity
is a type of disconformity in which the separation is a simple bedding plane; i.e., there is no obvious buried erosional surface.(AGI, 366) A blended unconformity
is a type of disconformity or nonconformity with no distinct separation plane or contact, sometimes consisting of soils, paleosols, or beds of pebbles derived from the underlying rock.
A nonconformity exists between sedimentary rocks and metamorphic
or igneous rocks
when the sedimentary rock lies above and was deposited on the pre-existing and eroded metamorphic or igneous rock.
An unconformity where horizontally parallel strata of sedimentary rock are deposited on tilted and eroded layers that may be either vertical or at an angle to the overlying horizontal layers. The whole sequence may later be deformed and tilted by further orogenic activity.
- American Geological Institute. Dictionary of Geological Terms. New York: Dolphin Books, 1962.
- U.S. Bureau of Mines Dictionary of Mining, Mineral, and Related Terms published on CD-ROM in 1996.
- Keith Montgomery Siccar Point and Teaching the History of Geology. University of Wisconsin. Retrieved on 2008-03-26..