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・ Sauk City, Wisconsin
・ Sauk County, Wisconsin
・ Sauk Lake
・ Sauk language
・ Sauk people
・ Sauk Prairie High School
・ Sauk Prairie, Wisconsin
・ Sauk Rapids Bridge
・ Sauk Rapids Regional Bridge
・ Sauk Rapids Township, Benton County, Minnesota
・ Sauk Rapids, Minnesota
・ Sauk Rapids-Rice High School
・ Sauk River
・ Sauk River (Minnesota)
・ Sauk River (Washington)
Sauk sequence
・ Sauk Trail
・ Sauk Trail Beach, Wisconsin
・ Sauk Trail Woods
・ Sauk Valley Community College
・ Sauk Valley Predators
・ Sauk Village, Illinois
・ Sauk, Albania
・ Sauk-Suiattle Indian Tribe of Washington
・ Sauka
・ Sauka parish
・ Saukam Khoy
・ Saukampen
・ Saukampen (Lom)
・ Saukampen (Nord-Fron)


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Sauk sequence : ウィキペディア英語版
Sauk sequence
The Sauk sequence was the earliest of the six cratonic sequences that have occurred during the Phanerozoic in North America. It was followed by the Tippecanoe, Kaskaskia, Absaroka, Zuñi, and Tejas sequences.
It dates from the late Proterozoic through the early Ordovician periods, though the marine transgression did not begin in earnest until the middle Cambrian.〔Monroe, JS, and R Wicander (1997) ''The Changing Earth: Exploring Geology and Evolution,'' 2nd ed. Belmont: West Publishing Company, 1997. ISBN 0-314-09577-2 p. 533-534〕
At its peak, most of North America was covered by the shallow Sauk Sea, save for parts of the Canadian Shield and the islands of the Transcontinental Arch. The stratigraphy of the Sauk sequence indicates shallow-water deposition, primarily consisting of well-sorted sandstones and clastic carbonates. A marine regression ended the Sauk sequence early in the Ordovician, to be followed by the Tippecanoe sequence later in the period.〔
==References==




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