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UNIT 12 The history of the Earth TYPES OF STRATIGRAPHIC DISCONTINUITIES Biology and Geology 4. Secondary Education UNIT UNIT 12 3 Types of stratigraphic discontinuities Stratigraphic discontinuity is the absence of the stratigraphic record for a specific period. There is a geologic time interval in the Earth's history, between two sequences separated by a discontinuity, that is not represented by sediments. There are many types of discontinuities: Biology and Geology 4. Secondary Education UNIT UNIT 12 3 Types of stratigraphic discontinuities ANGULAR UNCONFORMITY Young horizontal series Old folded series Discontinuity between an older stratigraphic series which folded and eroded when the strata were exposed to the weather and a more recent stratigraphic series. Biology and Geology 4. Secondary Education UNIT UNIT 12 3 Types of stratigraphic discontinuities DISCONFORMITY Series deposited after the erosion of the previous series Discontinuity between an old stratigraphic series which underwent a period of erosion and the more recent stratigraphic series which was deposited after that process. Biology and Geology 4. Secondary Education UNIT UNIT 12 3 Types of stratigraphic discontinuities NONCONFORMITY Young sedimented series Old eroded granite Discontinuity between an old series consisting of eroded rocks (e.g., granite) and the more recent sedimentary strata. Biology and Geology 4. Secondary Education UNIT UNIT 12 3 Types of stratigraphic discontinuities PARACONFORMITY Recently deposited young series Interruption in sedimentation over several million years Old series deposited millions of years ago. Discontinuity between an old series deposited many millions of years ago, after which there was an interruption in sedimentation over millions of years, and the more recent stratigraphic series. Biology and Geology 4. Secondary Education