Stratigraphy and geologic history of the Montana group and equivalent rocks, Montana, Wyoming, and North and South Dakota
James Ritchie Gill, William Aubrey Cobban
Abstract
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James Ritchie Gill, William Aubrey Cobban
Abstract
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During Late Cretaceous time a broad north-trending epicon tinental sea covered much of the western interior of North America and extended from the Gulf of Mexico to the Arctic Ocean. The sea was bounded on the west by a narrow, unstable, and constantly rising cordillera which extended from Central America to Alaska and which separated the sea from Pacific oceanic waters. The east margin of the sea was bounded by the low-lying stable platform of the central part of the United States.
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During Late Cretaceous time a broad north-trending epicon tinental sea covered much of the western interior of North America and extended from the Gulf of Mexico to the Arctic Ocean. The sea was bounded on the west by a narrow, unstable, and constantly rising cordillera which extended from Central America to Alaska and which separated the sea from Pacific oceanic waters. The east margin of the sea was bounded by the low-lying stable platform of the central part of the United States.
Key concepts: Geology, Cretaceous, Paleontology, Group (periodic table), Ammonite, Subsidence, Oceanography, Structural basin