Taunton vs Aurora

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Taunton is a town in Somerset, England, with a 2011 population of 69,570. It has over 1,000 years of religious and military history, including a 10th-century monastery. Taunton Castle has origins in the Anglo Saxon period. It was later the site of a priory. The Normans then built a stone castle that belonged to the Bishops of Winchester. Today's reconstructed buildings are the inner ward, housing the Museum of Somerset and Somerset Military Museum. Events include the Second Cornish uprising of 1497, when Perkin Warbeck marched a 6000-strong army to Taunton, most of which surrendered to Henry VII on 4 October 1497.

On 20 June 1685 the Duke of Monmouth crowned himself King of England at Taunton during a rebellion that culminated in the Battle of Sedgemoor. Judge Jeffreys then lived in the town during the Bloody Assizes held in the Great Hall of the Castle. The Grand Western Canal reached Taunton in 1839 and the railway in 1842. Today Taunton holds Musgrove Park Hospital, the Somerset County Cricket Club's County Ground and the headquarters of 40 Commando, Royal Marines. The Taunton flower show has been held in Vivary Park since 1866. The United Kingdom Hydrographic Office is located in Admiralty Way.

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