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  2. Indiana Limestone - Wikipedia

    en.wikipedia.org/wiki/Indiana_Limestone

    Indiana limestone (also known as Bedford limestone) is a form of limestone used as a building material, particularly for monumental public structures. Some 35 of the 50 state capitol buildings in the United States are made of Indiana limestone, [ 1 ] as are the Empire State Building , Biltmore Estate , the Pentagon and National Cathedral in ...

  3. Muscatatuck Group - Wikipedia

    en.wikipedia.org/wiki/Muscatatuck_Group

    The North Vernon Limestone is a geologic formation in Indiana. Also called the Sellersburg Limestone, this term however is no longer in use. [ 2 ] Originally called "Corniferous Limestone" it was defined as the unit between the New Albany Shale and the Jeffersonville Lime.

  4. Harrodsburg Limestone - Wikipedia

    en.wikipedia.org/wiki/Harrodsburg_Limestone

    Fossiliferous Harrodsburg Limestone from Indiana. The Harrodsburg Limestone is a geologic formation, a member of the Sanders Group of Indiana Limestone, of Mississippian age. It was named for Harrodsburg in southern Monroe County, Indiana by T. C. Hopkins and C. E. Siebenthal ("The Bedford Oolitic Limestone of Indiana" - 1897). It is made up ...

  5. Limestone - Wikipedia

    en.wikipedia.org/wiki/Limestone

    Limestone (calcium carbonate CaCO 3) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of CaCO 3. Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place ...

  6. From caves to cemeteries, here are 15 'undiscovered ... - AOL

    www.aol.com/caves-cemeteries-15-undiscovered...

    Orange County: Indiana's Lost River bubbles up at Orangeville Rise Visiting Orangeville Rise is another way to get a view into the Lost River as it surfaces from the caves and passages underground.

  7. Wyandotte Caves - Wikipedia

    en.wikipedia.org/wiki/Wyandotte_Caves

    The Monument Mountain in Wyandotte Caves, Indiana, is a cluster of large stalagmites on a breakdown pile. The ceiling is a classic tension dome. Wyandotte Caves began to form in the Pliocene Era, about 2 million years ago. [3] Like most of Southern Indiana's caves, the caves were formed when water dissolved limestone, causing hollow caves to form.

  8. Indiana Caverns - Wikipedia

    en.wikipedia.org/wiki/Indiana_Caverns

    The Indiana Caverns portion of Binkley Cave is almost entirely located in St. Louis Limestone, which is a thinly bedded limestone of Mississippian origin. St. Louis Limestone includes beds of chert and shale (the chert is showcased on the tour). Brachiopods and coral are apparent in the rock on the show tour. [4]

  9. AOL Mail

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    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!