Tameside vs Aurora

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The Metropolitan Borough of Tameside is a metropolitan borough of Greater Manchester in North West England. It is named after the River Tame, which flows through the borough and spans the towns of Ashton-under-Lyne, Audenshaw, Denton, Droylsden, Dukinfield, Hyde, Mossley and Stalybridge plus Longdendale. Its western border is approximately 4 miles (6.4 km) east of Manchester city centre. It borders High Peak in Derbyshire to the east, the Metropolitan Borough of Oldham to the north, the Metropolitan Borough of Stockport to the south, and the City of Manchester to the west.

As of 2011 the overall population was 219,324.The history of the area extends back to the Stone Age. There are over 300 listed buildings in Tameside and three Scheduled Ancient Monuments, which includes a castle of national importance. The settlements in Tameside were small townships centred on agriculture until the advent of the Industrial Revolution. The towns of the borough grew and became involved in the cotton industry, which dominated the local economy. The current borough was created in 1974 as part of the provisions of the Local Government Act 1972.

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