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Home > Art, Film & Photography > Regions of Minnesota: Animikie Group, Driftless Area, North Shore, Iron Range, Northwest Angle, Minnesota River, Siouxland, Central Minnesota
Regions of Minnesota: Animikie Group, Driftless Area, North Shore, Iron Range, Northwest Angle, Minnesota River, Siouxland, Central Minnesota

Regions of Minnesota: Animikie Group, Driftless Area, North Shore, Iron Range, Northwest Angle, Minnesota River, Siouxland, Central Minnesota


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About the Book

Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Pages: 25. Chapters: Animikie Group, Driftless Area, North Shore, Iron Range, Northwest Angle, Minnesota River, Siouxland, Central Minnesota, Red River Valley, Arrowhead Region, Boundary Waters, Southeast Minnesota, Pipestone Region. Excerpt: The Animikie Group is a geologic group composed of sediments that were deposited between 2,500 and 1,800 million years ago within the Animikie Basin. This group of formations are geographically divided into the Gunflint Range, the Mesabi and Vermilion ranges, and the Cuyuna Range. On the map the Animikie Group is the dark grey northeast-trending belt which ranges from south-central Minnesota, U.S., up to Thunder Bay, Ontario, Canada. The Gunflint Iron Range is the linear black formation labeled G, the Mesabi Iron Range is the jagged black linear formation labeled F and Cuyuna Iron Range is the two black spots labeled E. The gabbro of the Duluth Complex, intruded during the formation of the Midcontinent Rift, separates the Mesabi and Gunflint iron ranges; it is shown by the speckled area wrapping around the western end of Lake Superior. Banded-iron formations are iron formations which formed about 2,000 million years ago and were first described in the Lake Superior region. Sediments associated with the last stage of the Great Lakes tectonic zone contain banded-iron formations. These sediments were deposited for two hundred million years and extend intermittently along roughly the same trend as the Great Lakes tectonic zone, from Minnesota into eastern Ontario, Canada, and through upper Wisconsin and Michigan. They are characterized by bands of iron compounds and chert. Enough oxygen had accumulated in seawater so that dissolved iron was oxidized; iron reacts with oxygen to form compounds that precipitate out - including hematite, limonite and siderite. These iron compounds precipitated from the sea...


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Product Details
  • ISBN-13: 9781156582114
  • Publisher: Books LLC, Wiki Series
  • Publisher Imprint: Books LLC, Wiki Series
  • Height: 246 mm
  • No of Pages: 72
  • Spine Width: 4 mm
  • Weight: 145 gr
  • ISBN-10: 1156582113
  • Publisher Date: 09 Jul 2011
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Animikie Group, Driftless Area, North Shore, Iron Range, Northwest Angle, Minnesota River, Siouxland, Central Minnesota
  • Width: 189 mm


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