Geological time is on a different time to human time
Geological time is on a different scale from human time. The earth is estimated to be 4.6 billion years old, and life is thought to have become dominant on Earth 542 million years ago.
The first humans existed around 2 million years ago. This is only a short period of time when we consider the following:
First flowering plants 130m
Chalk 65m-145m
First birds 150m
First mammals 220m
First dinosaurs 225m
Granite 280m
First reptiles 325m
Carboniferous Limestone 340m First amphibians 360m
First plants and animals on land 420m
First multi-cellular organisms 1200m First bacteria 3500m
Age of the Earth 4.500,000,000
While time is often measured in hours and minutes, to geologists, time relating to rocks is measured in 100s and 1000s of years. This time is divided into eras and periods, which is the formation of the geological timescale (see diagram below), which relates to events, such as mountain building, atmospheric changes or widespread sea level change, that have happened in the Earth’s history. For example, tropical weather in the UK formed coal and limestone, which is known as the Carboniferous Period. The most recent period is known as the Quaternary period, which is when the Ice Age occurred.
Granite is from the Permian Period. It is a hard, igneous rock made up of quartz, feldspar and mica.
Carboniferous Limestone is from the Carboniferous period. It is a sedimentary rock made of calcium carbonate. It reacts with the acids in rainwater and dissolves to form distinctive scenery such as limestone pavement, caves and gorges.
Chalk is from the Cretaceous period. It is also a sedimentary rock made of calcium carbonate. It is porous, so water can penetrate it. It is eroded by solution.
Clay is from the Jurassic, Cretaceous and Tertiary periods. It is a sedimentary rock made of tiny particles of weathered rocks and minerals.
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