The weight of the rocks in the crust and upper mantle results in the pressure that allows diamonds to form.
The weight of the rocks above the mantle results in high pressure.Diamonds need high temperatures and pressure to form from carbon. Diamonds form in the mantle in certain zones where conditions are right for them to do so.There just happens to be the right critical temperature-pressure-mineral environment in the mantle in certain zones for their formation.
Yes, chocolate diamonds are formed under high pressure deep within the earth's mantle. The high pressure and temperature cause carbon atoms to crystallize into diamonds, which can vary in color, including chocolate tones.
Diamonds are formed deep within the Earth's mantle -- under extreme pressure and intense high heat. They are erupted to the Earth's surface through volcanic pipes. As well, there are man-made diamonds formed in laboratories.
When a tectonic plate reaches a certain depth in the mantle, the heat and pressure from being so close to the Earth's core causes certain parts of the plate to melt. The section of the plate that has melted becomes lighter in weight than the rocks surrounding it. This causes it to rise and move upwards in the mantle.
Diamonds are formed deep within the earth's mantle, typically between 140-190 kilometers (87-118 miles) below the surface. The intense heat and pressure at this depth cause carbon atoms to form the structure of a diamond over millions of years.
They cause plate movement. The plate movement then causes an earthquake.
No. As the pressure at the relatively shallow depths where volcanoes occur is not high enough to form diamonds. However it is true that volcanic eruptions can cause diamonds to be erupted onto the surface but these diamonds were already formed at much greater depth.
The most common cause of magma formation in the mantle is the increase in temperature due to the heat generated from the Earth's core, which causes the mantle rock to melt. This process is known as mantle convection, where hotter mantle material rises and cooler material sinks, creating a cycle that leads to the melting of rock and the formation of magma.
Pressure and heat in the mantle cause the rocks to become ductile and start deforming. As pressure decreases and heat increases due to the rising of magma, the rocks reach their melting point, allowing them to melt. This melted rock can then rise to the surface as magma and form igneous rocks.
When the pressure causes the rock to snap, it results in an earthquake. This sudden release of energy sends seismic waves that can cause the ground to shake and potentially damage buildings and infrastructure.
it will steady as liquid form and hot
The Earth's mantle is not entirely liquid because the temperature and pressure conditions vary throughout the mantle. While the high temperatures in the lower mantle can cause some rock to partially melt and flow, the majority of the mantle remains solid due to the higher pressure that prevents complete melting.