Magnetite
A defining entry in the Top 100 Books. Sitting at number 80, Magnetite earned its place through a combination of craft, context, and consensus among the twenty-four editors who maintain this list. The companions immediately above and below it on this ranking are worth reading in the same sitting.
Position in the list
About this entry
A defining entry in the Top 100 Books. Sitting at number 80, Magnetite earned its place through a combination of craft, context, and consensus among the twenty-four editors who maintain this list. The companions immediately above and below it on this ranking are worth reading in the same sitting. The editors’ note placed it here on the basis of three criteria: durability across re-reads (or re-watches, or re-plays), influence on the entries that came after it, and the degree to which it could only have been made by the person — or team — who made it.
In the comparative table maintained by the Books desk, Magnetite sits within a band of 77 – 83 that contains some of the most contested swaps of the year. Editors vote with arguments; a swap requires three editors and one written defense.
From Wikipedia
Magnetite is a mineral and one of the main iron ores, with the chemical formula Fe2+Fe3+2O4. It is one of the oxides of iron, and is ferrimagnetic; it is attracted to a magnet and can be magnetized to become a permanent magnet itself. With the exception of extremely rare native iron deposits, it is the most magnetic of all the naturally occurring minerals on Earth. Naturally magnetized pieces of magnetite, called lodestone, will attract small pieces of iron, which is how ancient peoples first discovered the property of magnetism.
