Regarding Murchison: every meteorite is identified by the name of the nearest community or other identifiable geographic feature it was first found near. The 100kg Murchison identified in the Meteoritical Bulletin was found in 1969 in Australia.
Some meteorites break up shortly after hitting the Earth's atmosphere, producing a strewn field with several to thousands of pieces being found. It would be extremely unlikely that a 100kg meteorite which fell near Victoria, Australia would also produce a fragment that fell in the U.S.
That said, there are several things to do to identify or rule out meteorites:
1) Most recent falls (within the last 10,000 years or so) have black or dark brown fusion crusts. This crust in rocks will look rather glossy, similar to a nodule of weathered obsidian.
2) Most meteorites are magnetic. If a magnet is not attracted to it, it probably isn't a meteorite.
3) Most meteorites are extremely heavy for their size. How much does your specimen weigh? How many cubic centimeters of water does it displace?
4) Many (but not all) meteorites have ablation blisters caused by the friction of air against the stone at high speed. These are called regmaglympts. I don't see any in this stone.