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  2. Examples of unconformities in geology include1234:
    • Angular unconformity: Represents a time gap between tilted or folded rock layers and overlying horizontal layers.
    • Nonconformity: Separates younger sedimentary rock from older igneous or metamorphic rock.
    • Disconformity: Erosional contact parallel to bedding planes.
    • Paraconformity: Subtle, difficult-to-identify unconformity.
    • Onlap or buttress unconformity: Overlapping younger layers on older rocks.
    • Blended unconformity: Combination of different types of unconformities.
    Learn more:
    For example, the contact between a 400‐million‐year‐old sandstone that was deposited by a rising sea on a weathered bedrock surface that is 600 million years old is an unconformity that represents a time hiatus of 200 million years.
    www.cliffsnotes.com/study-guides/geology/geologi…
    James Hutton found examples of unconformity in Scotland, at Jedburgh in 1787 and at Siccar Point in 1788. 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 the region.
    kids.kiddle.co/Unconformity

    Types of unconformities

    • 1. Angular unconformity
    • 2. Nonconformity
    • 3. Disconformity
    • 4. Paraconformity
    • 5. On lap or buttress unconformity
    geologybase.com/unconformity/

    Unconformities

    • Disconformity Disconformities are usually erosional contacts that are parallel to the bedding planes of the upper and lower rock units.
    geologyscience.com/geology/unconformities/
     
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    WEBJun 3, 2019 · An unconformity is a buried erosional or non-depositional surface that separates two different-age rock masses or strata, indicating that the deposition of sediments was not continuous.

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    WEBFeb 2, 2019 · When the rock record shows something unexpected it's called an unconformity. Unconformities come in four types and may be important or insignificant.

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    WEBFeb 2, 2022 · An unconformity denotes a long period throughout which deposition ceased, erosion removed previously formed rocks, and then new deposition resumed. It happens by upliftment of old strata and …

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