How is gold created




















Also, gold has unique properties that other metals lack. You can pound a single ounce of gold into a square foot sheet. Kings and queens across the globe have used the precious metal to display their divine superiority. The United States still has around Other than being used to display wealth or as a fashion statement, gold has some fantastic practical uses.

Probably its most important use is as a conductor for electricity. Its anti-corrosion properties make it a great resource to power our computers and mobile devices. As mentioned above, gold is a highly-malleable element. Here are some ways we use gold in modern society. Because of its rarity, people consider gold a valuable asset. In the United States, people could trade in paper money in exchange for an amount of gold equal in value.

Most developed countries once used the gold standard. However, many individuals purchase and hold them as financial investments. The most practical use of gold is in the manufacturing of electronic devices. Electronic devices containing gold are highly-dependable, which is why it is common in wiring, switches, connectors, and soldered joints. Almost all electronic devices today contain gold. Most companies also use gold to make televisions and kitchen appliances. Since few people recycle their electronics, a lot of gold gets lost.

As a result, thousands of dollars of gold goes unrecycled every year. In fact, we are the first laboratory world-wide that has successfully made such high-quality measurements. The impacting meteorites were stirred into Earth's mantle by gigantic convection processes. A tantalising target for future work is to study how long this process took.

Subsequently, geological processes formed the continents and concentrated the precious metals and tungsten in ore deposits which are mined today. Dr Willbold continued: "Our work shows that most of the precious metals on which our economies and many key industrial processes are based have been added to our planet by lucky coincidence when the Earth was hit by about 20 billion billion tonnes of asteroidal material.

Materials provided by University of Bristol. Note: Content may be edited for style and length. Science News. The research is published in Nature. Story Source: Materials provided by University of Bristol. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser or turn off compatibility mode in Internet Explorer. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

But a study published today in Nature Geoscience 1 has found that the process can occur almost instantaneously — possibly within a few tenths of a second. The process takes place along 'fault jogs' — sideways zigzag cracks that connect the main fault lines in rock, says first author Dion Weatherley, a seismologist at the University of Queensland in Brisbane, Australia.

When an earthquake hits, the sides of the main fault lines slip along the direction of the fault, rubbing against each other. But the fault jogs simply open up. Weatherley and his co-author, geochemist Richard Henley at the Australian National University in Canberra, wondered what happens to fluids circulating through these fault jogs at the time of the earthquake.

What their calculations revealed was stunning: a rapid depressurization that sees the normal high-pressure conditions deep within Earth drop to pressures close to those we experience at the surface. For example, a magnitude-4 earthquake at a depth of 11 kilometres would cause the pressure in a suddenly opening fault jog to drop from megapascals MPa to 0.

By comparison, air pressure at sea level is 0. Eventually, more fluid percolates out of the surrounding rocks into the gap, restoring the initial pressure. During the formation of Earth, molten iron sank to its centre to make the core. In fact, there are enough precious metals in the core to cover the entire surface of Earth with a four-metre thick layer.

Following the collapse of a massive star — at least eight times more massive than the Sun — what remains is a extremely dense core. They have masses comparable to a star, but that mass is compressed into an object roughly 10 kilometers in diameter, or the size of a city on Earth. Another way to look at this would be to imagine cramming Mount Everest into your morning cup of coffee to achieve the same density as a neutron star.

At these huge densities, the fabric and space and time is stretched by exotic physics. Two neutron stars in mutual orbit can collide when gravitational waves carry enough energy away from the system to destabilize the orbit. When this happens, a type of gamma-ray burst can occur — these are the most powerful explosions in the universe.

The intense energy would be enough to create gold and other heavy elements, according to a paper published in the Astrophysical Journal Letters. Tibi is a science journalist and co-founder of ZME Science. He writes mainly about emerging tech, physics, climate, and space.

In his spare time, Tibi likes to make weird music on his computer and groom felines. Home Other Did you know?



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