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Basalt
This dense igneous rock forms the bedrock of the ocean floors. It erupts as molten lava from oceanie volcanoes.
tGeology is the science of rocks—how they are created and destroyed, and how they have formed our planet. This lnvolves studying minerals, which are the natural \ Chemical compounds that form rocks, as well as k looking at the forces that drive geological processes.
01: Igneous rocks are madę of minerals formed by the cooling of molten rock erupting from below Earth’s crust.
02: These rocks are worn down into tiny particles (sediments), which are carried into the sea.
03: Over millions of years, the sediments are compressed to form sedimentary rocks.
04: Earth movements push these rocks up so that they become land and start wearing down.
When geologists first began studying rocks, they had no way of knowing how old they were. They figured out which rocks were the same age by comparing the minerals and fossils within them.
Groups of rocks are named after areas where they were studied or after an obvious feature. So Devonian rocks get their name from rock in Devon, England, while Carboniferous rocks include seams of coal, which is mostly carbon.
Older rock layers usually lie beneath younger ones, sińce they formed earlier. Devonian rocks are normally below carboniferous rocks, so are older. Permian rocks mainly lie above carboniferous rocks, so are younger.
These names are used to describe divisions of relative geological time. The Devonian, Carboniferous, and Permian are the three periods that led up to the age of the dinosaurs.
i Geologists can now datę rocks in millions of years, to give absolute geological time.
The number of years ago that Earth formed
The dating (in years) of the oldest-known rock on Earth’s surface—the Acasta gneiss of northwest Canada
The age (in years) of the oldest fossils of living things—algal colonies called stromatolites in the rocks of Pilbara,
Western Australia
The number of years ago that dinosaurs roamed Earth
The datę (in years) of the first evidence of our human i ancestors walking upright
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geology does literally ntean y “Earth science.
ock types
Granite
A very hard igneous rock, granite is mostly glassy quartz and feldspar, which often forms colorful crystals.
Sandstone
Many rocks are sedimentary— rock fragments bound together by other minerals. Sandstone is composed of sand grains.
Limestone
Another sedimentary rock, most limestones are madę of the skeletons of millions of microscopic sea organisms.
Schist
Earth’s oldest rocks have been squeezed and melted by massive forces to form metamorphic rocks, such as schist.
Geologists can datę rocks by measuring the amount of radioactive minerals (like uranium) that they contain. Over time, these turn into different minerals; by measuring this process, the rock can be dated.
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