Item: i96516

Authentic Medal of:

Great Britain under Victoria – Queen: 20 June 1837 – 22 January 1901
1875 Brass Medal 40mm x 35mm (17.52 grams)
Reference: BHM# 3015, Eimer# 1644
HOUSE OF COMMONS 22 JULY 1875 LONDON * S. PLIMSOLL *, Plimsoll facing left.
COFFIN SHIP, Ship sinking.

Medal Notes:
Plimsoll was a member of Parliament for Derby. He fought for an internationally agreed line to mark the safe loading limit for ships. The “Plimsoll Line” still exists on ships today.

You are bidding on the exact item pictured, provided with a Certificate of Authenticity and Lifetime Guarantee of Authenticity.

The waterline is the line where the hull of a ship meets the surface of the water. Specifically, it is also the name of a special marking, also known as an international load line, Plimsoll line and water line (positioned amidships), that indicates the draft of the ship and the legal limit to which a ship may be loaded for specific water types and temperatures in order to safely maintain buoyancy,[1] particularly with regard to the hazard of waves that may arise. Varying water temperatures will affect a ship’s draft, because warm water is less dense than cold water, providing less buoyancy. In the same way, fresh water is less dense than salinated or seawater with the same lessening effect upon buoyancy.

For vessels with displacement hulls, the hull speed is determined by, among other things, the waterline length.[citation needed] In a sailing boat, the waterline length can change significantly as the boat heels, and can dynamically affect the speed of the boat.

The waterline can also refer to any line on a ship’s hull that is parallel to the water’s surface when the ship is afloat in a normal position. Hence, all waterlines are one class of “ships lines” used to denote the shape of a hull in naval architecture plans.

In aircraft design, the term “waterline” refers to the vertical location of items on the aircraft. This is (normally) the Z axis of an X × Y × Z coordinate system, the other two axes being the fuselage station (X) and buttock line (Y).

Victoria (Alexandrina Victoria; 24 May 1819 – 22 January 1901) was Queen of the United Kingdom of Great Britain and Ireland from 20 June 1837 until her death. From 1 May 1876, she had the additional title of Empress of India.

Victoria was the daughter of Prince Edward, Duke of Kent and Strathearn, the fourth son of King George III. Both the Duke of Kent and King George III died in 1820, and Victoria was raised under close supervision by her German-born mother Princess Victoria of Saxe-Coburg-Saalfeld. She inherited the throne aged 18, after her father’s three elder brothers had all died, leaving no surviving legitimate children. The United Kingdom was already an established constitutional monarchy, in which the sovereign held relatively little direct political power. Privately, Victoria attempted to influence government policy and ministerial appointments; publicly, she became a national icon who was identified with strict standards of personal morality.

Victoria married her first cousin, Prince Albert of Saxe-Coburg and Gotha, in 1840. Their nine children married into royal and noble families across the continent, tying them together and earning her the sobriquet “the grandmother of Europe”. After Albert’s death in 1861, Victoria plunged into deep mourning and avoided public appearances. As a result of her seclusion, republicanism temporarily gained strength, but in the latter half of her reign her popularity recovered. Her Golden and Diamond Jubilees were times of public celebration.

Her reign of 63 years and seven months is known as the Victorian era. It was a period of industrial, cultural, political, scientific, and military change within the United Kingdom, and was marked by a great expansion of the British Empire. She was the last British monarch of the House of Hanover. Her son and successor, Edward VII, belonged to the House of Saxe-Coburg and Gotha, the line of his father.

Great Britain, also known as Britain, is an island in the North Atlantic off the north-west coast of continental Europe. With an area of 209,331 km² (80,823 sq mi), it is the largest island in Europe and the ninth-largest in the world. In 2011 the island had a population of about 61 million people, making it the third-most populous island in the world, after Java in Indonesia and Honshu in Japan. The island is the largest in the British Isles archipelago, which also includes the island of Ireland to its west and over 1,000 smaller surrounding islands.

The island is dominated by an oceanic climate with quite narrow temperature differences between seasons. Politically, the island is part of the United Kingdom of Great Britain and Northern Ireland, constituting most of its territory: most of England, Scotland, and Wales are on the island, with their respective capital cities, London, Edinburgh, and Cardiff. The term Great Britain often extends to include surrounding islands that form part of England, Scotland, and Wales.

A single Kingdom of Great Britain resulted from the Union of Scotland and England (which already comprised the present-day countries of England and Wales) in 1707. More than a hundred years before, in 1603, King James VI, King of Scots, had inherited the throne of England, but it was not until 1707 that the Parliaments of the two countries agreed to form a unified state. In 1801, Great Britain united with the neighboring Kingdom of Ireland, forming the United Kingdom of Great Britain and Ireland, which was renamed the United Kingdom of Great Britain and Northern Ireland after the Irish Free State seceded in 1922.