Final answer:
The iron from the deep rock layer at the mine was likely reddish-brown due to the presence of iron oxides such as hematite or magnetite, which form due to iron's reaction with oxygen.
Step-by-step explanation:
The iron taken from the deep rock layer at the mine likely had a reddish-brown color, different from the shiny and grey appearance of pure metallic iron. This is because, on Earth, iron is typically found in oxidized forms, not as the pure metal. Iron usually exists in the form of iron oxides, such as hematite (Fe2O3) or magnetite (Fe3O4), due to its reaction with oxygen. These iron oxides have various colors; hematite often gives a red-brown coloration, while magnetite is typically black.
The presence of these iron oxides in the rock from the mine is an indication that the iron there has reacted with oxygen to form these compounds. The process can also result in minerals like hydroxyapatite, which can incorporate iron traces, causing coloration in the mineral's appearance. Iron's tendency to react with oxygen and form oxides is why ancient civilizations used meteoritic iron or learned to smelt iron ores to obtain workable metal for tools and goods.