silicon 78%
oxygen 21%
oxygen and silicon
Oxygen, though usually a gas, is still in a molecule form and can be bonded to with any other molecule that is able to do so. Oxygen is a very common element in the crust because many rocks and more importantly minerals that make up those rocks use it in there atomic bonds. A simple example is Quartz, SiO2 So each single structure has one silicon atom and two oxygen atoms.
Oxygen, though usually a gas, is still in a molecule form and can be bonded to with any other molecule that is able to do so. Oxygen is a very common element in the crust because many rocks and more importantly minerals that make up those rocks use it in there atomic bonds. A simple example is Quartz, SiO2 So each single structure has one silicon atom and two oxygen atoms.
the elements of a mineral bond together in very ... of silicon and oxygen account for more than 75 percent of the earth's crust. ...
The crust, more specifically the lithosphere.
oxygen and silicon are the two elements that make up more than 80 percent of the atoms found in the Earths crust...(there is a constructed response for you guys)
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.
oxygen and silicon
Earth crust is composed of much more than two elements.The two most common elements in the crust are oxygen and silicon.
There are various parts that consist the earth's crust. It is mainly made up of two parts namely the lighter granite-based continental crust and the heavy basaltic oceanic crust. Some of the elements in the earth's crust include oxygen, silicon, magnesium, iron and so many more.
Oxygen, though usually a gas, is still in a molecule form and can be bonded to with any other molecule that is able to do so. Oxygen is a very common element in the crust because many rocks and more importantly minerals that make up those rocks use it in there atomic bonds. A simple example is Quartz, SiO2 So each single structure has one silicon atom and two oxygen atoms.
Oxygen, though usually a gas, is still in a molecule form and can be bonded to with any other molecule that is able to do so. Oxygen is a very common element in the crust because many rocks and more importantly minerals that make up those rocks use it in there atomic bonds. A simple example is Quartz, SiO2 So each single structure has one silicon atom and two oxygen atoms.
the elements of a mineral bond together in very ... of silicon and oxygen account for more than 75 percent of the earth's crust. ...
Silicon
Oceanic crust is more dense.
The crust, more specifically the lithosphere.
This is the SiO4 anionic group. Thus, the answer you need would be that there are more oxygen atoms.