Fife vs Aurora

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Fife (, Scottish English: [fɐi̯f]; Scottish Gaelic: Fìobha, IPA: [fiːvə]; Scots: Fife) is a council area, historic county, registration county and lieutenancy area of Scotland. It is situated between the Firth of Tay and the Firth of Forth, with inland boundaries to Perth and Kinross (i.e. the historic counties of Perthshire and Kinross-shire) and Clackmannanshire. By custom it is widely held to have been one of the major Pictish kingdoms, known as Fib, and is still commonly known as the Kingdom of Fife within Scotland. A person from Fife is known as a Fifer. Fife was a county of Scotland until 1975, having been the parliamentary constituency of Fife in the House of Commons of the United Kingdom until 1885 and the Fife constituency in the Parliament of Scotland until the Acts of Union 1707. In older documents it was very occasionally known by the anglicisation Fifeshire. From 1975 to 1996 Fife was a local government region, divided into three districts: Dunfermline, Kirkcaldy and North-East Fife.

In 1996 the district councils were abolished and Fife regional council became a unitary authority known as Fife Council. Fife is one of the six local authorities in the city region of Edinburgh and South East Scotland. Fife is Scotland's third largest local authority area by population. It has a resident population of just under 367,000, over a third of whom live in the three principal towns, Dunfermline, Kirkcaldy and Glenrothes. The historic town of St Andrews is located on the northeast coast of Fife. It is well known for the University of St Andrews, the most ancient university of Scotland and one of the oldest universities in the world. From the 15th century it was the metropolis of the former Archdiocese of St Andrews, St Andrews Cathedral having been the seat of the most senior bishop of Scotland since the 10th century. St Andrews is also renowned as the home of golf.

Source: Wikipedia

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An aurora (plural: auroras or aurorae), sometimes referred to as polar lights (aurora polaris), northern lights (aurora borealis), or southern lights (aurora australis), is a natural light display in the Earth's sky, predominantly seen in high-latitude regions (around the Arctic and Antarctic). Auroras are the result of disturbances in the magnetosphere caused by solar wind. These disturbances are sometimes strong enough to alter the trajectories of charged particles in both solar wind and magnetospheric plasma. These particles, mainly electrons and protons, precipitate into the upper atmosphere (thermosphere/exosphere).

The resulting ionization and excitation of atmospheric constituents emit light of varying color and complexity. The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere. Proton auroras are usually observed at lower latitudes.

Source: Wikipedia