Native elements are those which occur in nature in their pure form (not as compounds). Examples include gold and silver as well as carbon (in the form of graphite or diamond).
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Some native elements found in the Earth's crust are gold, silver, copper, and sulfur. These elements occur naturally in their pure form without being chemically bonded to other elements.
From most abundant to least: oxygen, silicon, aluminum, iron, calcium, sodium, magnesium, potassium, titanium, hydrogen.
The major heat source of Earth's crust is residual heat from the planet's formation and radioactive decay of elements like uranium, thorium, and potassium within the Earth's interior. This heat is responsible for driving processes like mantle convection, plate tectonics, and volcanic activity on the Earth's surface.
True, both the crust and mantle are composed of solid rock. The innermost part of the crust is also believed to be solid, although it may experience some plastic deformation under extreme pressures and temperatures.
The crust is thickest on oceanic plates where the crust is typically around 5-10 km thick under the oceans. In contrast, continental crust is generally thicker, around 30-50 km thick, with some mountain ranges having crust that can be even thicker.
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Some examples of elements that are also minerals include gold, silver, copper, sulfur, and diamond. These elements naturally occur in the Earth's crust in solid form and meet the criteria to be classified as minerals.