Banded iron formations (also known as banded ironstone formations or BIFs) are a distinctive type of rock often found in primordial
sedimentary rocks. The structures consist of repeated thin layers of
iron oxides, either
magnetite or
hematite, alternating with bands of iron-poor
shale and
chert. Some of the oldest known rock formations, formed around three thousand million years before present (3
Ga), include banded iron layers, and the banded layers are a common feature in
sediments for much of the
Earth's early history. Banded iron beds are less common after 1.8 Ga, although some are known that are much younger.
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A rock that is made up of alternating light silica-rich layers and dark-colored layers of iron-rich minerals, which were deposited in marine basins on every continent about 2 billion years ago.