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Jacobsville Sandstone is a red sandstone formation, marked with light-colored streaks and spots, primarily found in northern Upper Michigan, portions of Ontario, and under much of Lake Superior. Desired for its durability and aesthetics, the sandstone was used as an architectural building stone in both Canada and the United States.
The Courthouse is an asymmetrical 2 + 1 ⁄ 2-story brick-and-sandstone structure with a mansard roof, designed primarily in an interpretation of Second Empire style, but with elements of other styles included. 18: Jacobsville Finnish Lutheran Church: Jacobsville Finnish Lutheran Church
Pictured Rocks is the site of many of Michigan's waterfalls. Most of the waterfalls resulted from water running over the cliffs of the Munising Formation. This lime and sandstone formation exists between Tahquamenon Falls, some 75 miles (121 km) east, to Laughing Whitefish Falls, 30 miles (48 km) west of the Lakeshore. Pets are not allowed on ...
The Wall is a near-vertical slope of the Jacobsville Sandstone which dips as steeply 85°. [7] The steep dip of the Jacobsville Sandstone is the result of it being folded due to motion on the fault. Interstate State Park at St. Croix Falls, Wisconsin is an example of the Keweenaw Fault. On its trails visitors can find Tholeiitic basalts.
Freda Sandstone (Pcf, grey) on NPS Apostle Islands geological map. The Freda Sandstone is a geologic formation in Michigan.It dates back to the Proterozoic.Lithologically, the Freda Sandstone is a lithic, red-brown, cyclic sequence of sandstones, mudstones and shales (conglomerates are rare).
Jacobsville is an unincorporated community on the south side of the Keweenaw Peninsula near the outlet of the Keweenaw Waterway at [ 5 ] [ 9 ] It is the site of sandstone quarries that are now shut down but formerly supplied red sandstone for buildings throughout North America and Europe .
The Hancock Town Hall is a two-story building constructed of rock-faced red Jacobsville Sandstone set in even courses, exhibiting Richardsonian Romanesque, Dutch, and Flemish architectural influences. [2] It has a gable roof and a square tower with belfry at one corner; the tower originally had a steep conical roof.
[1] [3] In addition, exposures of gently dipping, friable Jacobsville Sandstone, have been reported from Caribou Island. [4] The Jacobsville Sandstone is the uppermost and youngest layer comprising about 8 kilometers (5.0 mi) of sandstone and conglomerate that underlies Lake Superior and fills the upper part of the Lake Superior segment of the ...