The Earth's crust contains eight elements. The most common element among the eight is Oxygen (47 percent) and second is Silicon (28 percent).
depends if you're talking about in the earths crust, in water or in the human boby. In us, carbon comes second. In the water, hydrogen. In the atmosphere ther is actually way more nitrogen than there is oxygen.
yes this is true.
Earths outermost layer is the crust.Actually, the crust is divided into two parts,Sial and Sima.In that way, actually Sial is the outermost layer of the crust,as it lies above the Sima.
Just to say: This question refers to rock groups. Not what type of rock.Igneous rocks make up most of the earth's crust.
The eight most common elements in the Earth's crust are oxygen, silicon, aluminum, iron, calcium, sodium, potassium, and magnesium. These elements make up approximately 99% of the Earth's crust by weight. Oxygen is the most abundant element in the Earth's crust, comprising about 46.6% of its mass, followed by silicon at around 27.7%.
Quartz and feldspars are the most common silicate minerals of the crust.
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.
Silicate is the mineral group in the Earth's crust. This contains quartz, feldspars, and micas.
Silicate is the mineral group in the Earth's crust. This contains quartz, feldspars, and micas.
Silicate is the mineral group in the Earth's crust. This contains quartz, feldspars, and micas.
one of the common minerals that make up most of the rocks of the earths crust
earths crust , oceans and atmosphere
one of the common minerals that make up most of the rocks of the earths crust
one of the common minerals that make up most of the rocks of the earths crust
silicates
The eight most common elements in the earths continental crust are; 1. Oxygen. 2. Silicon. 3. Aluminium. 4. Iron. 5. Calsium. 6. Sodium. 7. Potassium. 8. Magnesium.
Quartz and feldspars are the most common silicate minerals of the crust.