oxygen and aluminum
Quartz and feldspars are the most common silicate minerals of the crust.
Silicate minerals form through the cooling and solidification of magma or lava, in a process called crystallization. As the molten rock cools, elements and compounds within the magma combine to form various silicate minerals based on their chemical composition and crystal structure. The process can occur both deep within the Earth's crust and on the surface during volcanic activity.
Quartz, feldspar or mica
Only 10% of the Earth's crust is composed of non-silicate minerals. Examples of non-silicate minerals are barringerite, nickel phosphide, taenite and suessite.
minerals
Many minerals occur naturally on the earths surface in rock form
Oxygen is the largest component of crustal rock.
The Earth's mantle is primarily composed of silicate minerals, which give it a greenish-gray color. However, the mantle is located beneath the Earth's crust, so its color is not visible on the surface.
silicon & oxygen.
The most common minerals found in Earth's crust are quartz, feldspar, and mica. These minerals make up a significant portion of the Earth's continental crust and are essential components of many rock types.
Less than. The moon rock density is greater in ferromagnesion and nickel content, with greater density, whereas silicate rocks contain largely quartz and feldspar minerals.
it is called a dick