Mallet was born in Dublin, on 3 June 1810, the son of factory owner John Mallet. He was educated at Trinity College, Dublin,[2] entering it at the age of 16 and graduating in science and mathematics in 1830 at the age of 20.[3]
Career
After his graduation, he joined his father's iron foundry business and helped build the business into one of the most important engineering works in Ireland, supplying ironwork for railway companies, the Fastnet Rock lighthouse, and a swing bridge over the River Shannon at Athlone. He also helped manufacture the characteristic iron railings that surround Trinity College and which bear his family name at the base.[3]
On 9 February 1846 he presented to the Royal Irish Academy his paper, "On the Dynamics Of Earthquakes",[4] which is considered to be one of the origins of modern seismology. He is also credited with inventing the word "seismology" and some related words, e.g. the isoseismal map, which he used for his research. He also invented the term epicentre.[5]
From 1852 to 1858, he was prepared (with his son, John William Mallet) his work, The Earthquake Catalogue of the British Association (1858),[6] and performed blasting experiments to determine the speed of seismic propagation in sand and solid rock.[3]
On 16 December 1857, the area around Padula, Italy, was devastated by the Great Neapolitan earthquake which caused 11,000 deaths. At the time it was the third largest known earthquake in world history and has been estimated to have been of magnitude 7.0 on the Moment magnitude scale.[7] Mallet, with letters of endorsement from Charles Lyell and Charles Darwin, petitioned the Royal Society of London and received a grant of £150 to go to Padula and record the devastation personally. The resulting report was presented to the Royal Society as the Report on the Great Neapolitan Earthquake of 1857. It was a major scientific work and made great use of the then new process of photography to record the devastation caused by the earthquake. In 1862, he published the "Great Neapolitan Earthquake of 1857: The First Principles of Observational Seismology"[8] in two volumes; he brought forward evidence to show that the depth below the Earth's surface, from where the impulse of the Neapolitan earthquake originated, was about 8–9 geographical miles.
One of Mallet's papers was Volcanic Energy: an Attempt to develop its True Origin and Cosmical Relations,[9] in which he sought to show that volcanic heat may be attributed to the effects of crushing, contortion and other disturbances in the crust of the earth; the disturbances resulting in the formation of lines of fracture, more or less vertical, down which water would find its way, and if the temperature generated be sufficient volcanic eruptions of steam or lava would follow.[citation needed]
Other work
Mallet's Mortar with 36-inch shells which would have contained 480 lb (217 kg) of gunpowder.
During the Crimean War he designed a 42-long-ton (43 t) mortar of 36 inches (910 mm) calibre capable of throwing a 2,400 pounds (1,100 kg) shell a distance of 1.5 miles (2.4 km). The huge mortar was built in sections to allow transport, but was too late to be used in action. An example has been preserved at the Royal Artillery base in Woolwich and one is displayed before the Royal ArmouriesFort Nelson near Portsmouth.[citation needed]
