historyWikipedia1840–1883
Railways forced time zones into existence, and Congress only made them law in 1918
Local solar time changes with longitude, about four minutes per degree, so before railways every town kept its own clock. In 1840 Britain's Great Western Railway began using Greenwich Mean Time, and in 1883 North American railroads adopted a system of standard time zones that Congress made law in 1918. Italian mathematician Quirico Filopanti proposed 24 worldwide zones in 1858, and Sandford Fleming pushed a worldwide system in 1876. Within a few decades almost every inhabited place had a standard time, though many used local observatory time rather than an offset from Greenwich. Today the world uses whole and fractional offsets from UTC, and some large countries still stretch across more longitude than one zone ideally covers.
Solar noon arrives about four minutes later for each degree of longitude travelled east. A shared clock time therefore has to be a fixed offset from a reference meridian, and each ideal zone spans about 15 degrees of longitude to match one hour.
Time zones are the hidden coordination layer behind trains, flights, the internet and global trade, and their borders are often political compromises. Their shape still affects daily life, from working hours to sunrise times.
Nepal adopted the offset UTC+05:45 in 1986, a quarter-hour difference from its neighbours.
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