Any gap in age of rock between rock layers is called an uncomformity. An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
A horizontal layer intruding between two sedimentary layers could be labeled as a SILL.
a SILL is an intrusion that is parallel to the strata.
Gaps in rock layers are called unconformities.
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Uncomformitty
erosion
Unconformities occur when erosion wears away rock, or when rock deposits are never formed.
A gap in the geological record in a body of rock is called an unconformity.
An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
A gap in the geologic record of rock formations is called an uncomformity.
unconformities
a gap in the geologic record that shows where rock layers have been lost do to erosion
erosion
Unconformities occur when erosion wears away rock, or when rock deposits are never formed.
A gap in the geological record in a body of rock is called an unconformity.
An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
A dis-conformity is an unconformity representing a period of erosion or lack of deposition in a sedimentary rock section.
Erosion of already deposited layers or a time span of non-deposition.
A gap in the geologic record of rock formations is called an uncomformity.
A gap in sedimentary layers is known as an unconformity, and occurs as a result of either erosion or a period of non-deposition.
unconformity (plural unconformities)(nonstandard) A lack of conformity.(geology) A gap in time in rock strata, where erosion occurs while deposition slows or stops.
An unconformity is a gap in time of the rock record. In a stratigraphic column this is evidence that erosion has removed a portion of the natural deposition of sediment in an area. In a disconformity erosion takes place between sedimentary rocks that have not been otherwise modified. In an angular unconformity, previous bedding has been tilted from its original deposition and undergone erosion, and is topped by new sediment that is deposited horizontally on top of this tipped surface. In a nonconformity, huge amounts of erosion have exposed igneous or metamorphic basement rock and there is an igneous or metamorphic rock contacting sedimentary rock.