After the oceans formed; you could imagine that the water was full of all sorts of materials, which were dissolved from the rocks as the waters slowly filled up the oceans, when the earth cooled sufficiently for large volumes of water to accumulate.
The dissolved materials included a lot of iron salts (probably iron chloride and iron sulphate); as well as the soduim chloride still present today.
The first forms of life that developed are thought to be bacteria (similar to today's blue-green algae). They didn't require oxygen, but converted carbon dioxide and water to sugars using sunlight; much like todays plants. Oxygen was actually a waste product, so they excreted it (blue green algae still do this today). Conditions were ideal for them, so they multiplied rapidly, and had the oceans mostly to themselves for hundreds of millions of years.
The oxygen they gave off reacted with the dissolved iron salts in the water to form iron hydroxides and iron oxides. These materials are insoluble; so they settled to the bottom. It took millions of years for the oxygen to react with all the dissolved iron, and very thick deposits formed. These can still be seen today, and are called
'banded iron formation'.
Finally, when most of the iron had been precipitated out of the water, there was an excess of oxygen, which was partly dissolved in the water, and then also passed into the atmosphere, enabling marine and terrestrial oxygen requiring life forms to develop. This where the oxygen in the atmosphere came from; and if it weren't for the early cyanobacteria, life on earth would not exist.
Over time, the large deposits of iron rich sediments were moved and changed because of the movements of the crustal plates, and they eventually formed large deposits of magnetite and haematite, which make up most of the world's iron ore deposits.
That is why most iron ore deposits are found in ancient rock formations.
"Ore" is the singular form and refers to a naturally occurring material from which minerals can be extracted, typically metal ores. "Ores" is the plural form of "ore," indicating multiple sources of mineral deposits.
No, Bauxite is not a type of iron ore. it is an ore of aluminum.
Lead is a nonsilicate mineral. It belongs to the sulfide mineral group and is commonly found in ore minerals such as galena.
Limestone is not an ore. It is a sedimentary rock composed primarily of calcium carbonate. Ores are rocks or minerals that contain valuable elements or minerals that can be extracted for profit, such as iron ore or gold ore.
Its considered an ore when it contains enough of a useful substance that it can be sold for a profit.
"Ore" is the singular form and refers to a naturally occurring material from which minerals can be extracted, typically metal ores. "Ores" is the plural form of "ore," indicating multiple sources of mineral deposits.
veins
No. By definition a rock is made of minerals. An ore is a mineral resource that can be extracted, refined, and sold at a profit.
Minerals are minerals. An ore is a rock matrix that has a rather large amount of a certain mineral in it, hence "Iron ore", Silver ore", etc.
Major rock forming minerals include quartz, feldspar, and mica. Ore minerals include galena (lead ore), chalcopyrite (copper ore), and hematite (iron ore). These minerals play a crucial role in the formation of rocks and are economically important for their mineral content.
Ore deposits typically form from the concentration of ore minerals within Earth's crust through various geological processes such as hydrothermal fluids, magmatic segregation, or sedimentary accumulation. These processes involve the mobilization and concentration of valuable elements or minerals in specific areas, leading to the formation of economically viable deposits.
A mixture of minerals is called an ore
A mixture of minerals is called an ore
Ore deposit.
Ore is made up of minerals.
No, Bauxite is not a type of iron ore. it is an ore of aluminum.
Ore.