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  2. Late Cretaceous - Wikipedia

    en.wikipedia.org/wiki/Late_Cretaceous

    The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after creta, the Latin word for the white limestone known as chalk.

  3. Judith River Formation - Wikipedia

    en.wikipedia.org/wiki/Judith_River_Formation

    The Judith River Formation is a fossil-bearing geologic formation in Montana, and is part of the Judith River Group.It dates to the Late Cretaceous, between 79 and 75.3 million years ago, [4] corresponding to the "Judithian" land vertebrate age.

  4. Dinosaur Park Formation - Wikipedia

    en.wikipedia.org/wiki/Dinosaur_Park_Formation

    The Dinosaur Park Formation is the uppermost member of the Belly River Group (also known as the Judith River Group), a major geologic unit in southern Alberta.It was deposited during the Campanian stage of the Late Cretaceous, between about 76.5 and 74.4 million years ago. [3]

  5. Mancos Shale - Wikipedia

    en.wikipedia.org/wiki/Mancos_Shale

    The Mancos Shale or Mancos Group is a Late Cretaceous (Upper Cretaceous) geologic formation of the Western United States. The Mancos Shale was first described by Cross and Purington in 1899 [ 1 ] and was named for exposures near the town of Mancos, Colorado .

  6. Maastrichtian - Wikipedia

    en.wikipedia.org/wiki/Maastrichtian

    The Maastrichtian (/ m ɑː ˈ s t r ɪ k t i ə n / mahss-TRIK-tee-ən) is, in the International Commission on Stratigraphy (ICS) geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from .

  7. Horseshoe Canyon Formation - Wikipedia

    en.wikipedia.org/wiki/Horseshoe_Canyon_Formation

    It is of Late Cretaceous age, Campanian to early Maastrichtian stage (Edmontonian Land-Mammal Age), and is composed of mudstone, sandstone, carbonaceous shales, and coal seams. A variety of depositional environments are represented in the succession, including floodplains , estuarine channels, and coal swamps, which have yielded a diversity of ...

  8. Appalachia (landmass) - Wikipedia

    en.wikipedia.org/wiki/Appalachia_(landmass)

    During most of the Late Cretaceous (100.5 to 66 million years ago) the eastern half of North America formed Appalachia (named for the Appalachian Mountains), an island land mass separated from Laramidia to the west by the Western Interior Seaway. This seaway had split North America into two massive landmasses due to a multitude of factors such ...

  9. Cretaceous - Wikipedia

    en.wikipedia.org/wiki/Cretaceous

    The Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series. In older literature, the Cretaceous is sometimes divided into three series: Neocomian (lower/early), Gallic (middle) and Senonian (upper/late). A subdivision into 12 stages, all originating from European stratigraphy, is now used worldwide. In ...