Vermilion Granite Complex Minnesota

The 2 700 ma vermilion granitic complex of northern minnesota is a granite migmatite terrane composed of supracrustal metasedimentary rocks mafic rocks tonalitic and granodioritic plutonic rocks and granite.

Vermilion granite complex minnesota.

Not synopsized to date. It s also well stocked with muskies and hosts several tournaments each year. Includes but not restricted to the vermilion granite of grout 1923 no longer used and to other abandoned names. Burntside gneiss lac la croix granite.

The wawa subprovince i e. The vermilion granitic complex consists of granitic and migmatitic rocks of archean age 2 700 m y that are the westward extension into minnesota of the quetico gneiss belt of ontario. Alphabetical all in mn. The tower soudan underground mine is open for tours all season.

Is part of vermilion granitic complex in the northern part of the superior province of the canadian shield in northern mn in the lake superior region. The giants range batholith south of the vermilion fault. Vermillion is a city in dakota county minnesota united states. Vermilion series vermilion schist and vermilion group as used by winchell and winchell 1887 and van hise and clements 1901.

It s part of the fortune bay casino complex located on everett bay of lake vermilion. The vermilion granitic complex consists of granitic and migmatitic rocks of archean age 2 700 m y that are the westward extension into minnesota of the quetico gneiss belt of ontario fig. Vermilion granitic complex mn subunits. The population was 419 at the 2010 census.

The western half of the larger wawa abitibi subprovince and the wabigoon subprovinces are both typical archean granite greenstone terranes composed of metamorphosed volcanic rocks greenstones later intruded by granitoids e g. Is present in an area north of vermilion district in northeastern mn in lake superior region. The 2 700 ma vermilion granitic complex of northern minnesota is a granite migmatite terrane composed of supracrustal metasedimentary rocks mafic rocks tonalitic and granodioritic plutonic rocks and granite. Was passively emplaced into previously folded stratified rocks at depths somewhat greater than plutonic activity in adjoining volcanic plutonic belts.