It depends on the type of feldspar. Potassium Feldspar (also called K-Spar), contains potassium, aluminum, silicate: KAlSi3O8. Plagioclase Feldspar, on the other hand, contains calcium or sodium, aluminum, and silicate: NaAlSi3O8 or CaAl2Si2O8.
Nitrogen makes up about 78% of the Earth's atmosphere.
Nitrogen makes up 78% of Earth's atmosphere.
Nitrogen
Iron makes up most of the Earth's core.
Nitrogen makes up 78% of the Earth's atmosphere.
No
How much feldspar weighs varies greatly depending on the size of the stone or collection. Feldspar is a rock-forming mineral that makes up a huge portion of the world's crust.
Countries producing feldspar include Brazil, Colombia, France, Germany, India, Mexico, Norway and Spain. Feldspar definitely makes up the Earth's crust.
Feldspar is a mineral compound, not an element. It is a group of rock-forming tectosilicate minerals that make up about 60% of the Earth's crust. It is composed of aluminum, silica, and other elements like potassium, sodium, or calcium.
The most common element found in orthoclase feldspar but not in plagioclase feldspar is potassium (K). Orthoclase is a potassium-rich feldspar, typically represented by the chemical formula KAlSi3O8. In contrast, plagioclase feldspar is a solid-solution series that primarily consists of sodium (Na) and calcium (Ca) in its composition, lacking potassium.
The element that makes up most of the earths CORE is iron.
The element that makes up the majority of the human body is oxygen.
No, feldspar is not a native element. It is a mineral composed of aluminum silicates, often found in igneous rocks like granite. Native elements are minerals composed of a single element, like gold or silver.
The main mineral that makes up the Earth's crust is called feldspar. Feldspar is a group of rock-forming minerals that make up about 60% of the Earth's crust by weight.
Hydrogen is an element, there will be atom that makes up an element and not element that will turn into another.
Orthoclase feldspar
The mineral group of feldspar minerals comprise roughly 50% of the lithosphere (the crust plus the brittle uppermost mantle), 60% of the continental crust.