Dom Pedro aquamarine

Nowadays, Dom Pedro aquamarine is a topic that has captured the attention of many people around the world. From its impact on society to its influence on the economy, Dom Pedro aquamarine is a topic that has become increasingly relevant in everyday conversations. With the increasing importance of Dom Pedro aquamarine, it is crucial to understand its scope and implications in different aspects of life. In this article, we will thoroughly explore Dom Pedro aquamarine and analyze its impact on our modern society. From its origins to its possible future developments, we will delve into the fascinating world of Dom Pedro aquamarine and discover its true meaning in today's world.

Dom Pedro Aquamarine
The Dom Pedro aquamarine at the Natural History Museum in Washington, D.C.
General
CategoryOxide mineral[1][2]
FormulaBe3Al2Si6O18

The Dom Pedro aquamarine is the world's largest cut aquamarine gem. It was cut from a crystal originally weighing approximately 60 pounds (27 kg) and measuring almost 2 feet (0.61 m) in length. The stone was mined in Pedra Azul, in the state of Minas Gerais in Brazil around 1980, and named after the Brazilian emperors Pedro I and Pedro II. The blue-green gemstone was cut by Bernd Munsteiner into an obelisk form weighing 10,363 carats. The finished dimensions measure 14 inches (36 cm) tall by 4 inches (10 cm) wide. The jewel was donated to the Smithsonian Institution by Jane Mitchell and Jeffery Bland. It is housed in the National Museum of Natural History's Janet Annenberg Hooker Hall of Geology.[3][4]

See also

References

  1. ^ Beryl mineral information and data, Mindat
  2. ^ Quartz page on Mineralien Atlas
  3. ^ Vastag, Brian (2 December 2012). "The Dom Pedro aquamarine's long and winding path to the Smithsonian". The Washington Post. Archived from the original on 8 December 2012. Retrieved 7 December 2012.
  4. ^ "Magnificent Dom Pedro aquamarine to go on view in the Smithsonian's Natural History Museum". Smithsonian Science. Smithsonian Institution. Archived from the original on 5 July 2014. Retrieved 7 December 2012.