What Lies Beneath Our Feet?
So far, humanity has only managed to explore about 12 kilometres into the Earth’s crust, and even that took us 20 years! But science never rests. Researchers continue to investigate how seismic waves travel through the Earth, and how their speed and behaviour change as they pass through different densities within the Earth’s layers.
Above this is the mantle, which starts about 30 kilometers below the Earth's surface. The mantle is composed mostly of iron, magnesium, and silicon. It contains precious gems like diamonds, as well as rock formations.
Next, we have the Earth’s crust, which can be compared to the hard shell of a boiled egg. The crust varies in thickness from 5 to 70 kilometers. This part of the Earth is cool and fragile, and can be easily broken. The crust is divided into several pieces called tectonic plates, which move slowly—about 3 to 5 centimeters (1.2 to 2 inches) per year. These movements are responsible for earthquakes and volcanic eruptions.
The Composition of the Earth:
- Iron – 32.1%
- Oxygen – 30.1%
- Silicon – 15.1%
- Magnesium – 13.9%
- Sulfur – 2.9%
- Nickel – 1.8%
- Calcium – 1.5%
- Aluminum – 1.4%
- Other elements – 1.2%
The concept of the Earth’s rotation and its spherical shape was first proposed by Greek philosophers. Later, the great Muslim scholar Al-Biruni, during the Ottoman Caliphate, accurately measured the Earth’s circumference. He claimed that the Earth is not flat, but spherical, and revolves around the sun. Using only mathematics and algebra, Al-Biruni’s measurement was so precise that it differed from today’s scientific measurement by only 2%.
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