All these statements describe King Louis XIV of France.
- <em>He called himself the Sun King because he considered himself as important as the sun itself.</em> Louis XIV is known to have had a very high opinion of himself. This is why he chose the sun as his symbol. Le Roi Soleil (the Sun King) was a way to present himself as a ruler who knew and saw everything (like the sun) and could not fail. He also felt a strong connection to the Greek Sun God, Apollo.
- <em>During his seventy-two year reign he claimed the divine rights of kings.</em> 72 years is the longest time any monarch has ruled over a European kingdom in history. Louis XIV believed he was the representative of God on earth, and therefore decided that the absolute powers of kingship were a sacred, god-given right.
- <em>He moved his court from Paris to Versailles, where he and his courtiers lived in splendor and excess.</em> Louis XIV frequently changed residences, but in 1682 he settled with his court in the Palace of Versailles, making it a symbol of French riches and prestige.
- <em>He did little or nothing to help the working people with everyday struggles. </em>Many of his subjects thought that Louis XIV put his personal interests before the country's. During the War of Spanish Succession for example (1701-14), he kept France at war to make sure his grandson, Philip V, would gain control over the Spanish Empire, while the cost of war caused famine among the people.
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I think it would be Aztec
"Why should we follow British rule?"
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Mohs hardness, rough measure of the resistance of a smooth surface to scratching or abrasion, expressed in terms of a scale devised (1812) by the German mineralogist Friedrich Mohs. The Mohs hardness of a mineral is determined by observing whether its surface is scratched by a substance of known or defined hardness.
Related Topics: hardness
To give numerical values to this physical property, minerals are ranked along the Mohs scale, which is composed of 10 minerals that have been given arbitrary hardness values. The minerals contained in the scale are shown in the Table; also shown are other materials that approximate the hardness of some of the minerals. As is indicated by the ranking in the scale, if a mineral is scratched by orthoclase but not by apatite, its Mohs hardness is between 5 and 6. In the determination procedure it is necessary to be certain that a scratch is actually made and not just a “chalk” mark that will rub off. If the species being tested is fine-grained, friable, or pulverulent, the test may only loosen grains without testing individual mineral surfaces; thus, certain textures or aggregate forms may hinder or prevent a true hardness determination. For this reason the Mohs test, while greatly facilitating the identification of minerals in the field, is not suitable for accurately gauging the hardness of industrial materials such as steel or ceramics. (For these materials a more precise measure is to be found in the Vickers hardness or Knoop hardness) Another disadvantage of the Mohs scale is that it is not linear; that is, each increment of one in the scale does not indicate a proportional increase in hardness. For instance, the progression from calcite to fluorite (from 3 to 4 on the Mohs scale) reflects an increase in hardness of approximately 25 percent; the progression from corundum to diamond, on the other hand (9 to 10 on the Mohs scale), reflects a hardness increase of more than 300 percent.
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