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Location: Roughly 2300-2900 N. Main, 2300-2800 Normandy, & 100-200 blocks E. Ardennes, Palau, Bastogne, Leyte, Saint Lo & Guam, Mishawaka, Indiana Coordinates: Area
Andrew Thomas House, in Carroll County First Christian Church, designed by Eliel Saarinen, in Bartholomew County Jeffries Ford Covered Bridge, destroyed by fire in 2002 but still NRHP-listed, in Parke County State Bank of Indiana, Branch of (Memorial Hall), in Vigo County USS LST 325 (tank landing ship), Vanderburgh County St. Augustine's Episcopal Church, designed by Edward D. Dart, in Lake ...
The NHLs in Indiana comprise approximately 2% of the 1,656 properties and districts listed on the National Register of Historic Places in Indiana as of December 2009. The landmarks are among the most important nationally recognized historic sites in the state; the George Rogers Clark National Historical Park is one other site that has high ...
Google Maps' location tracking is regarded by some as a threat to users' privacy, with Dylan Tweney of VentureBeat writing in August 2014 that "Google is probably logging your location, step by step, via Google Maps", and linked users to Google's location history map, which "lets you see the path you've traced for any given day that your ...
Montgomery County was established by an act of the Indiana state legislature passed on December 21, 1822, which defined the county's boundaries and provided for the organization of its government. It was formed from parts of Wabash New Purchase attached to Parke and Putnam Counties. [ 6 ]
U.S. Route 27 (US 27) is a part of the United States Numbered Highway System that runs from Miami, Florida, to Fort Wayne in the U.S. state of Indiana. In Indiana, it is a state road that enters the state in College Corner, Ohio, and West College Corner. The 117.765 miles (189.524 km) of US 27 that lie within Indiana serve as a major conduit.
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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.